Wildfires leave behind loss and ruin - charred homes, scorched forests, communities upended. Yet even in those blackened remnants, Professor Pei Chiu sees an overlooked resource with climate potential.&nbsp;



In his lab at the<a href="https://www.udel.edu/" target="_blank" rel="noreferrer noopener"> University of Delaware</a>, Professor Chiu studies “char,” the carbon-rich residue produced when biomass burns without much oxygen. His team has probed both naturally produced <a href="https://www.earth.com/news/wildfire-risk-is-rapidly-rising-across-the-southern-u-s/">wildfire</a> char and its artificial cousin, biochar.



The researchers uncovered a surprising role of chars: they can help starve methane-producing microbes and tilt microbial communities toward pathways that generate far less climate damage.



<h2 class="wp-block-heading" id="h-why-wildfire-char-is-everywhere">Why wildfire char is everywhere</h2>



Char forms whenever organic matter is heated at high temperatures with limited <a href="https://www.earth.com/news/dark-oxygen-discovery-deep-ocean-rocks-upends-centuries-of-scientific-beliefs/">oxygen</a>. In nature, that’s wildfires; in industry, it’s pyrolysis, the controlled heating of leftover biomass such as wood chips, corn stalks, rice husks, and other agricultural residues.&nbsp;



Commercial “biochar” is already used to improve soils, blend into compost, and filter stormwater. 



Wildfire char, by contrast, is scattered by the ton across burned landscapes and gradually worked into soils by wind, rain, and <a href="https://www.earth.com/news/plant-roots-could-be-key-to-fighting-climate-change/">roots</a>.



<h2 class="wp-block-heading" id="h-chars-that-behave-like-batteries">Chars that behave like batteries</h2>



Several years ago, Chiu’s group noticed something striking: chars made by pyrolysis behaved like tiny rechargeable batteries. They could store and release electrons - a property the team calls electron storage capacity (ESC).&nbsp;



That matters because <a href="https://www.earth.com/news/microbes-aquificales-discovered-in-hot-springs-breathe-oxygen-and-sulfur-at-same-time/">microbes</a> make a living moving electrons around. In oxygen-rich settings, they “breathe” oxygen to accept electrons as they break down sugars. In oxygen-poor places - think landfills, manure pits, waterlogged soils, rice paddies, <a href="https://www.earth.com/news/wetlands-are-a-hidden-source-of-rising-methane-emissions/">wetlands</a>, or the guts of anaerobic digesters - other organisms take over.&nbsp;



Among the most consequential are methanogens, microbes that churn out <a href="https://www.earth.com/news/microbes-have-emerged-as-major-source-of-methane-emissions/">methane</a>, a heat-trapping gas roughly 85 times more potent than CO₂ over the short term and responsible for about a third of current warming.



Chiu’s team showed that char gives many common soil microbes an alternative “breath.” In essence, char can stand in for oxygen as an electron sink, letting beneficial microbes keep metabolizing without ceding the field to methanogens. When that happens, methane production drops.



<h2 class="wp-block-heading" id="h-what-wildfires-have-to-do-with-it">What wildfires have to do with it</h2>



Wildfire char has been part of Earth’s carbon cycle for millions of years. That longevity led Chiu to a simple hypothesis: if char has been embedded in soils for eons, microbes likely evolved ways to use it.&nbsp;



Across a range of chars - those born in wildfires and those made in kilns - the team measured substantial ESC, enough to change who thrives in oxygen-limited environments.&nbsp;



<h2 class="wp-block-heading" id="h-how-much-charge-are-we-talking-about">How much “charge” are we talking about?</h2>



The numbers are eye-opening. In lab tests, a single gram of char - about a quarter teaspoon - could hold on the order of 10²¹ electrons. Scale that to real-world biomass and the potential grows fast.&nbsp;



U.S. agriculture alone generates roughly 140 million dry tons of crop residues each year (with corn stover and wheat straw leading the way), while forestry adds 60–70 million dry tons more.&nbsp;



Collectively, Chiu noted, chars represent an immense rechargeable, bioavailable reservoir of electrons - he likens it to a “trillion-trillion-trillion” (10³⁶) electrons injected into the global biogeochemical cycle annually.



<h2 class="wp-block-heading" id="h-turning-down-methane-naturally">Turning down methane - naturally</h2>



In controlled experiments, all wildfire chars and plant-based biochars tested suppressed methane formation.&nbsp;



The mechanism is elegant: by giving char-“breathing” microbes a competitive edge, the material helps outcompete methanogens, which still produce more than 50% of global methane today.&nbsp;



Unlike a chemical additive that’s used once and gone, char can be reused by microbes repeatedly, serving as a long-lived electron buffer in soils, sediments, and engineered systems.



<h2 class="wp-block-heading" id="h-cleaner-water-healthier-soils">Cleaner water, healthier soils</h2>



Steering electrons through char doesn’t only curb methane. The same microbial pathways can keep arsenic from mobilizing into drinking water or crops and can remove nitrate and perchlorate from stormwater and groundwater.&nbsp;



That dovetails with biochar’s existing uses in filtration and <a href="https://www.earth.com/news/planting-diverse-crops-traps-carbon-and-boosts-soil-health/">soil health</a>, suggesting one material can deliver multiple environmental services at once.



None of this minimizes the devastation of wildfires, which destroy ecosystems, businesses, and lives. But Chiu argues there’s value in learning from what’s left behind.&nbsp;



Wildfire char’s electron-trading ability points to a sustainable lever for <a href="https://www.earth.com/news/climate-mitigation-strategies-may-be-endangering-biodiversity/">climate mitigation</a> and pollution control - one built on microbes already common in nature and on carbon materials produced at massive scales, whether by accident (fires) or design (pyrolysis).



<h2 class="wp-block-heading" id="h-why-the-urgency-and-the-hope">Why the urgency - and the hope</h2>



CO₂ rightly dominates climate discussions, but it lingers for 50 to 200 years. Methane is different: far stronger in the near term and with an atmospheric lifetime of about 12 years. That makes near-term methane cuts an unusually fast-acting climate lever.&nbsp;



“If we can find ways to reduce methane, we could see the impact within our lifetimes,” said Professor Chiu.



That promise keeps his team pushing on the basic science: How exactly do microbes “breathe” a solid? How do different chars - from different fires, feedstocks, or kiln settings - shift ESC and microbial behavior?&nbsp;



And how can this knowledge be scaled into landfill covers, livestock waste systems, wetlands restoration, or post-fire land management so that nature’s own electron economy helps dial down a powerful greenhouse gas?



Char, in other words, may be the rare wildfire remnant that points forward.



Study co-authors include doctoral student Jiwon Choi and former graduate student Danhui Xin (now at the <a href="https://www.sccwrp.org/" target="_blank" rel="noreferrer noopener">Southern California Coastal Water Research Project</a>).



The research is published in the journal <a href="https://pubs.acs.org/doi/10.1021/acs.est.5c05709" target="_blank" rel="noreferrer noopener">Environmental Science &amp; Technology</a>.



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From ashes to action: Wildfire char holds a hidden climate solution

Wildfires leave behind loss and ruin - charred homes, scorched forests, communities upended. Yet even in those blackened remnants, Professor Pei Chiu sees an overlooked resource with climate potential.&nbsp; In his lab at the University of Delaware, Professor Chiu studies “char,” the carbon-rich residue produced when biomass burns without much oxygen. His team has probed both naturally produced wildfire char and its artificial cousin, biochar. The researchers uncovered a surprising role of chars: they can help starve methane-producing microbes and tilt microbial communities toward pathways that generate...

The,Changing,Seas,Of,The,Florida,Keys.,Growing,Corals,And

Sea levels have risen and fallen since Earth first held oceans. Until recently, scientists could only measure these shifts over million-year increments. 



Now, researchers from Utrecht, the UK, and the United States have mapped sea level changes across much shorter timeframes - spanning thousands of years and covering the last 540 million years.



Published in&nbsp;the journal Earth and Planetary Science Letters, the study combines paleoclimate data, sediment records, and orbital modeling.



"Taking these rapid sea level variations into account is important for understanding the structure of the subsurface and the applications to green energy resources," said Dr. Douwe van der Meer, guest researcher at <a href="https://www.uu.nl/en" target="_blank" rel="noreferrer noopener">Utrecht University</a> and lead author of the study.



<h2 class="wp-block-heading" id="h-measuring-sea-level-rise">Measuring sea level rise</h2>



Sea level changes depend on two main factors: plate tectonics and <a href="https://www.earth.com/news/land-exposed-by-melting-glaciers-transforms-into-a-greenhouse-gas-emitter/">land ice</a>. Tectonics control the shape of ocean basins. Ice determines how much water fills them. 



Previously, scientists could detect 200-meter (656 feet) swings in sea level over million-year periods using fossil and rock records.



"In time steps of about a million years, you can derive an average sea level for as far back as there are fossils, about 540 million years," said Van der Meer.



"That varied by as much as 200 meters. We suspected that sea level could go up and down enormously in much shorter periods as well, but there is not enough data to make those shorter time steps."



<h2 class="wp-block-heading" id="h-earth-s-orbit-affects-sea-level">Earth’s orbit affects sea level</h2>



To track faster <a href="https://www.earth.com/earthpedia-articles/a-simple-guide-to-understanding-sea-level-rise/">changes</a>, researchers used a clever method. They matched sediment records with Earth’s orbital cycles, called Milankovitch cycles, that change climate on scales of 20,000 to 400,000 years. These wobbles trigger glacial and interglacial phases, which affect sea levels.



"We see alternations, especially when the global climate is cold, and there is ice on the poles," said Van der Meer. 



"Then, the rhythmic wobbling of Earth's spin axis creates ice ages that last only tens of thousands of years, during which the sea level can go up and down by as much as 100 meters (328 feet)."



This new approach calculated how much ice volume could change due to orbital variations. Then, the researchers estimated how those changes would affect sea level during the last 540 million years.



<h2 class="wp-block-heading" id="h-greenhouse-vs-icehouse-worlds">Greenhouse vs. icehouse worlds</h2>



During warm, ice-free periods like the mid-Cretaceous, sea levels stayed relatively stable. In contrast, colder times like the late Carboniferous or modern ice age showed huge sea level swings.



Modeling showed that orbital cycles in the icehouse phases could cause sea levels to shift by over 328 feet within a few thousand years.



During the Permo-Carboniferous, for example, global temperatures may have ranged from 17°C (62.6°F) during interglacials to 10°C (50°F) during glacials. 



Such shifts drove large expansions and retreats of ice sheets, influencing sediment layers and fossil patterns.



<h2 class="wp-block-heading" id="h-past-sea-level-rise-helps-planning">Past sea level rise helps planning</h2>



Knowing when and how sea levels changed helps scientists better understand Earth’s climate and geography. These findings can also improve models for <a href="https://www.earth.com/news/geothermal-energy-is-cheap-and-clean-and-having-its-moment/">geothermal energy</a>, hydrogen storage, and radioactive waste disposal.



"High or low sea levels, it's all happened before in the geological past," said Van der Meer.



Sandstone, laid down during low sea levels, makes a good reservoir for storing gases or heat. Claystone, formed during high sea levels, can seal these reservoirs. Mapping these layers globally can help in safe subsurface use.



"If we know that at a certain time global sea level was high, we also know that a relatively continuous layer of claystone would have been deposited," said Van de Meer.



"We can use that information to create a global layer map of sand and claystone, which helps us in the safe use of the subsurface."



<h2 class="wp-block-heading" id="h-ancient-sea-level-rise-patterns">Ancient sea level rise patterns</h2>



The researchers tested their new model against known sedimentary records. For the Silurian, their orbital-scale sea level variation estimates - around 230 feet - match compiled data from five paleo-continents.



Similar matches appear in Cretaceous and Devonian records, with fluctuations ranging from 50 to 230 feet.



The model shows especially large short-term sea level swings during the late Ordovician, Permo-Carboniferous, and the past few million years. 



<figure class="wp-block-image aligncenter size-full"><a href="https://www.earth.com/wp-content/uploads/2025/07/earth_sea-level-history_graphic_credit-EPSL_1m.jpg"><img src="https://www.earth.com/wp-content/uploads/2025/07/earth_sea-level-history_graphic_credit-EPSL_1s.webp" alt="Paleogeographic reconstructions. A) Last Glacial Maximum (∼20 ka), an example of maximum glacial extent, low global mean sea level and more exposed continental shelf. As a result of changing continental ice-cover, glacio-eustasy results in changes in eustasy and flooding of continents. B) Present-Day, as example of an Interglacial with relatively high sea level. Long-term sea level reconstructions do not consider short-term changes in sea level due to orbital-scale variations. Credit: Earth and Planetary Science Letters (2025)" class="wp-image-1978010"/></a><figcaption class="wp-element-caption">Paleogeographic reconstructions. A) Last Glacial Maximum (∼20 ka), an example of maximum glacial extent, low global mean sea level and more exposed continental shelf. As a result of changing continental ice-cover, glacio-eustasy results in changes in eustasy and flooding of continents. B) Present-Day, as example of an Interglacial with relatively high sea level. Long-term sea level reconstructions do not consider short-term changes in sea level due to orbital-scale variations. Click image to enlarge. Credit: Earth and Planetary Science Letters (2025)</figcaption></figure>



In contrast, during the <a href="https://www.earth.com/news/jurassic-rocks-reveal-new-details-about-earths-climate-system/">Jurassic</a> and mid-Cretaceous, the shifts were much smaller, generally under 164 feet.



Some older reconstructions show higher variability, up to 328 feet, even during greenhouse phases. The new study argues that such large estimates may be inflated and not supported by physical models or isotope data.



Instead, this new work provides more grounded estimates using physics-based ice models, stratigraphy, and isotope geochemistry.



<h2 class="wp-block-heading" id="h-future-climate-and-geology-research">Future climate and geology research</h2>



This approach can help resolve long-standing questions about <a href="https://www.earth.com/news/ancient-climate-shift-sheds-light-on-future-global-warming/">ancient climates</a>, sedimentary patterns, and biodiversity changes. It also offers new tools for identifying reliable storage sites in the subsurface.



The authors suggest refining the method with non-linear models and more paleoclimate simulations. For now, their work marks a turning point in how we study ancient sea levels.



It is not just about history. It is a guide to understanding our dynamic planet.



The study is published in the journal <a href="https://www.sciencedirect.com/science/article/pii/S0012821X25003243?via%3Dihub" target="_blank" rel="noreferrer noopener">Earth and Planetary Science Letters</a>.



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New model reveals dramatic swings in Earth's sea levels

Sea levels have risen and fallen since Earth first held...

Greenland’s ice-covered landscape looks like an immovable block on satellite maps. Yet the story locked beneath its center suggests a very different past, one that places future coastal cities in a tight spot. 



During the <a href="https://www.sciencedirect.com/topics/social-sciences/pleistocene">Pleistocene</a> - the geologic chapter that began about 2.7 million years ago and ran through innumerable swings between cold and mild - the island’s ice waxed and waned in tune with global climate.



New evidence hints that those swings were more dramatic than scientists once believed.



In&nbsp;1993, drillers hauled a two‑mile‑deep ice core up from the island’s highest point and stowed the entire column in a Colorado freezer. 



The surprise awaited in the bottom three inches of sediment: perfectly preserved traces of a tundra ecosystem. 



That sliver of soil, shielded for ages by roughly 1.9 miles (3 km) of ice, now refocuses the conversation about <a href="https://www.earth.com/news/how-much-did-sea-levels-rise-after-the-last-ice-age-alarming-new-clues-revealed/">future sea level</a> and the stability of polar ice in a warming world.



<h2 class="wp-block-heading" id="h-tundra-hidden-beneath-greenland-s-ice">Tundra hidden beneath Greenland's ice</h2>



Once the drill broke through that 1.9‑mile roof of ice, the researchers retrieved those three inches of till. 



“These fossils are beautiful,” says Paul&nbsp;Bierman, a scientist at the <a href="https://www.uvm.edu/" target="_blank" rel="noreferrer noopener">University of Vermont</a> who co‑led the new study with UVM graduate student Halley&nbsp;Mastro and nine other researchers.



“But, yes, we go from bad to worse,” Bierman added, referring to what this finding implies about the impact of <a href="https://www.earth.com/news/indisputable-evidence-of-human-caused-climate-change/" target="_blank" rel="noreferrer noopener">human‑caused climate change</a> on melting of the Greenland ice sheet.



The till holds poppy, spike‑moss, woody willow tissue, fungal sclerotia, insect parts, and a band of soil capped by about&nbsp;16&nbsp;inches of erratic boulders. 



This is clear evidence that <a href="https://www.earth.com/news/drones-reveal-hidden-details-about-greenlands-melting-ice/" target="_blank" rel="noreferrer noopener">central Greenland</a> once lay ice‑free under a cold, dry sky where late‑lying snow lingered through early summer.



Because the material sits undisturbed, the team is confident it was not swept in from elsewhere as ice advanced.



<h2 class="wp-block-heading" id="h-inside-a-deep-greenland-ice-core">Inside a deep Greenland ice core</h2>



“Once we made the discovery at Camp&nbsp;Century, we thought, ‘Hey, what's at the bottom of&nbsp;GISP2?’” Bierman recalled.



High‑energy isotope ratios show that the summit last saw open air within the past 1.1 million years, while argon trapped in overlying clear ice indicates at least 250,000 years of continuous cover since then. 



<a href="https://www.nature.com/articles/s41467-024-47351-z" target="_blank" rel="noreferrer noopener">Basal ice</a> at another drilling site about 19 miles away is roughly 1 million years old.



A separate core from Camp&nbsp;Century <a href="https://www.earth.com/news/city-under-the-ice-secret-base-camp-found-in-greenland/" target="_blank" rel="noreferrer noopener">near the coast</a> yielded plant remains no older than&nbsp;416,000&nbsp;years, underscoring the ice sheet’s flickering presence across the Pleistocene. 



These findings draw on material that had been stored at the National Science Foundation <a href="https://icecores.org/" target="_blank" rel="noreferrer noopener">Ice Core Facility</a> in Lakewood, Colorado, for three decades.



<h2 class="wp-block-heading" id="h-fossils-divulge-a-warmer-greenland">Fossils divulge a warmer Greenland</h2>



Under the microscope, what had looked like no more than specks floating on the surface of the melted core sample was, in fact, a window into a <a href="https://www.earth.com/news/greenland-transformation-ice-melt-plant-growth-vegetation-cascading-effects/" target="_blank" rel="noreferrer noopener">tundra landscape</a>. 



“It was amazing,” Mastro exclaimed. 



<figure class="wp-block-image aligncenter size-full"><a href="https://www.earth.com/wp-content/uploads/2025/04/greenland-ice-core_soil-sample_fossils_recently-melted-ice_credit-UVermont_1m.jpg"><img src="https://www.earth.com/wp-content/uploads/2025/04/greenland-ice-core_soil-sample_fossils_recently-melted-ice_credit-UVermont_1s.webp" alt="Willow bud scale, arctic poppy seed, fungal bodies, and rock spikemoss megaspores found in the GISP2 soil sample viewed under a microscope at the University of Vermont. Click image to enlarge. Credit: Halley Mastro/University of Vermont" class="wp-image-1977508"/></a><figcaption class="wp-element-caption">Willow bud scale, arctic poppy seed, fungal bodies, and rock spikemoss megaspores found in the GISP2 soil sample viewed under a microscope at the University of Vermont. Click image to enlarge. Click image to enlarge. Credit: Halley Mastro/University of Vermont</figcaption></figure>



Mastro and colleagues picked out spores of spike‑moss, the bud scale of a young willow, and the compound eye of an insect - life‑forms adapted to chilly air and long summer daylight.



“And then we found Arctic poppy - just one seed of it. That is a tiny flower that's really good at adapting to the cold. It lets us know that Greenland's ice melted and there was soil, because poppies don't grow on top of miles of ice,”&nbsp;Mastro continued.



<h2 class="wp-block-heading" id="h-sea-level-risks-for-global-coasts">Sea‑level risks for global coasts</h2>



<a href="https://www.earth.com/news/fossil-corals-reveal-that-sea-level-rise-occurs-in-rapid-bursts/">Sea level today</a> is rising more than an inch each decade. “And it's getting faster and faster,” said Bierman. The extra water comes from a warming ocean that expands as well as from melting glaciers worldwide.



Near‑complete melting of Greenland’s ice over the next centuries to a few millennia would lead to some&nbsp;23&nbsp;feet of sea‑level rise. 



“Look at Boston, New&nbsp;York, Miami, Mumbai, or any other coastal city around the world, and add&nbsp;20‑plus feet of sea level. It goes underwater. Don't buy a beach house," Bierman advised.



<a href="https://www.earth.com/news/how-much-did-sea-levels-rise-after-the-last-ice-age-alarming-new-clues-revealed/" target="_blank" rel="noreferrer noopener">Sea level</a> is likely to be several feet higher by the end of this century, when today’s children are grandparents.



<h2 class="wp-block-heading" id="h-greenland-s-fragile-ice-fortress">Greenland's fragile ice fortress</h2>



Richard Alley, a leading climate scientist at <a href="https://www.psu.edu/" target="_blank" rel="noreferrer noopener">Penn State University</a>, reviewed the new research.



“This new study confirms, and expands upon earlier evidence, that significant sea‑level rise occurred at a time when the causes of warming were not especially extreme, providing a warning of the damage we might cause if we continue to warm the climate," Alley noted.



“We now have direct evidence that not only was the ice gone, but that plants and insects were living there,” Bierman concluded. “And that's unassailable. You don't have to rely on calculations or models.” 



The fossil soil at Greenland’s summit, locked beneath nearly two miles of ice, speaks plainly: polar ice sheets can retreat far and fast when the climate tips, and the coastlines of the future will trace that story in real time. 



Whether that warning is heeded remains a decision for policy makers and citizens alike.



The full study was published in the journal <a href="https://www.pnas.org/doi/10.1073/pnas.2407465121#supplementary-materials" target="_blank" rel="noreferrer noopener">Proceedings of the National Academy of Sciences</a>.



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Greenland ice discovery stuns and worries scientists: "Don't buy a beach house"

Greenland’s ice-covered landscape looks like an immovable block on satellite...

Sharks have survived five mass extinctions and ruled the oceans for over 400 million years. As apex predators, they play a critical role in maintaining the balance of marine ecosystems.&nbsp;But today, sharks are more threatened than ever. 



On Shark Awareness Day, we highlight the science behind their importance. Without sharks, ocean ecosystems would become unbalanced, leading to overpopulation of some species and the collapse of others.



This disruption would harm the overall health of the <a href="https://www.earth.com/news/ocean-climate-fixes-could-worsen-the-oxygen-crisis/">ocean</a>, ultimately affecting food security and coastal economies.



<h2 class="wp-block-heading" id="h-what-happens-when-sharks-disappear">What happens when sharks disappear?</h2>



A <a href="https://www.earth.com/news/top-predator-missing-what-happens-when-great-white-sharks-disappear/#google_vignette">long-term study</a> conducted in False Bay, South Africa, offers a real-world example of what happens when sharks disappear from an ecosystem.



The researchers found that by mid‑2018, great white sharks had vanished from the region. This led to dramatic shifts throughout the ecosystem.&nbsp;



With the disappearance of great whites, Cape fur seal and sevengill shark populations surged, while their prey - smaller fish and bottom-dwelling shark species - declined sharply.&nbsp;



The findings provide real-world evidence of a “trophic cascade,” where the loss of a top predator triggers a ripple effect through lower levels of the food web.



The researchers suggest that the sharks may have disappeared due to several potential causes, including targeted attacks by orcas - which have been observed killing and eating great white livers.&nbsp;



The study demonstrates the importance of apex predators in maintaining ocean health. The research highlights how their loss can destabilize marine webs and reduce biodiversity.



<h2 class="wp-block-heading" id="h-declining-shark-populations-nbsp">Declining shark populations&nbsp;</h2>



According to a <a href="https://www.earth.com/news/overfishing-has-caused-a-50-decline-in-sharks-and-rays/">study</a> led by researchers from Simon Fraser University, over half of all sharks and rays have disappeared globally since 1970 - with overfishing identified as the primary cause.&nbsp;



Sharks and rays, serving as critical predators and sediment stirrers, help maintain food webs and nutrient flows. The report revealed that around one-third of shark and ray species now face extinction. 



However, there is cause for hope: countries such as Australia, Canada, New Zealand, the US, parts of Europe, and South Africa have implemented science-based fishing limits, reduced bycatch, and protected critical habitats.



<h2 class="wp-block-heading" id="h-endangered-shark-species-nbsp">Endangered shark species&nbsp;</h2>



Among the most threatened are the great <a href="https://www.earth.com/news/why-some-great-hammerhead-sharks-rarely-leave-home/">hammerhead</a> and the scalloped hammerhead sharks - both of which have seen dramatic population declines worldwide.&nbsp;



These species are particularly vulnerable because they grow slowly and reproduce rarely, making it hard for their populations to bounce back once they decline.



The oceanic whitetip shark, once abundant across tropical and subtropical waters, has suffered steep losses from bycatch and targeted fishing - pushing it toward critical endangerment.&nbsp;



Many deep-sea sharks, like the bluntnose sixgill and the gulper shark, are also threatened due to slow reproduction rates combined with increased fishing pressures.



<h2 class="wp-block-heading" id="h-campaigns-around-the-world">Campaigns around the world</h2>



Around the world, numerous campaigns and organizations are dedicated to protecting sharks and raising awareness about their critical role in ocean ecosystems.&nbsp;



One of the most widely recognized efforts is <a href="https://www.discovery.com/shark-week/shark-week-2025-kicks-off-july-20">Shark Week</a>, a series on the Discovery Channel that draws millions of viewers each summer. Through documentaries and expert interviews, the series highlights both the awe-inspiring nature of sharks and the threats they face from human activity.



<a href="https://iucn.org/our-union/members/iucn-members/project-aware-foundation">Project AWARE</a> mobilizes scuba divers globally to advocate for shark conservation by pushing for bans on shark finning and the creation of marine protected areas.&nbsp;



On a larger scale, coalitions like the <a href="https://www.globalsharkmovement.org/">Global Shark Movement Project</a> work to influence policy and fisheries management worldwide.



The International Union for Conservation of Nature (IUCN) <a href="https://www.iucnssg.org/">Shark Specialist Group</a> also plays a vital role by assessing species status and guiding conservation strategies globally.&nbsp;



Together, these campaigns combine public education, advocacy, and policy efforts to reduce shark deaths and support healthier oceans for future generations.



<h2 class="wp-block-heading" id="h-celebrate-shark-awareness-day-nbsp">Celebrate Shark Awareness Day&nbsp;</h2>



Shark Awareness Day highlights the urgent need for stronger protections and <a href="https://www.earth.com/news/sustainable-fishing-must-be-redefined-to-halt-ocean-destruction/">sustainable fishing practices</a> to prevent the irreversible loss of these vital ocean predators.



Today, people around the world are encouraged to learn about sharks and the threats they face from human activities. We are also encouraged to take action by choosing sustainable seafood and speaking up for better laws to protect sharks.&nbsp;



Shark Awareness Day helps build a stronger global community committed to conservation efforts. Ultimately, protecting sharks is about protecting the entire ocean system - and a planet that depends on it.



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Shark Awareness Day: Protecting the balance of the ocean 

Sharks have survived five mass extinctions and ruled the oceans...

Niagara Falls pulls in tourists by the boatload. Angel Falls towers higher than city skyscrapers. Yet both pale in comparison to Earth's largest waterfall - an enormous, rushing torrent concealed below Arctic waves.



The Denmark Strait cataract drops in slow motion beneath the chilly surface between Iceland and Greenland. 



The chute begins thousands of feet down, rolls over a hidden ledge, and keeps sliding for 11,500 feet.



No roar reaches the surface, no mist fills the air, and passing ships glide on as if nothing remarkable lies below these crucial <a href="https://www.earth.com/news/atlantic-and-arctic-mixing-is-crucial-for-earths-climate-stability/">Arctic waters</a>, which drive Earth's climate.



<h2 class="wp-block-heading" id="h-the-denmark-strait-cataract">The Denmark Strait cataract</h2>



Most of Earth's largest waterfalls form when a river meets a cliff and spills over. Turbulent water gouges the rock, the lip grows steeper, and a postcard scene is born. 



<a href="https://www.nature.com/articles/s41598-024-75984-z" target="_blank" rel="noreferrer noopener">Submarine waterfalls</a> follow a different script. Here, colder, saltier water sinks below lighter layers, slipping along the seafloor like syrup down a tilted pan. The motion is silent, pulling entire water masses rather than a single stream.



Oceanographers first confirmed the Denmark Strait cataract decades ago by tracing temperature and salinity profiles through the channel. 



Sensors revealed a dense ribbon of <a href="https://www.earth.com/news/arctic-ocean-stayed-partly-open-during-harsh-ice-ages/">Nordic Sea</a> water sliding into the Atlantic basin, gathering speed until it tumbled past a submerged ridge. That ridge acts as the unseen cliff, setting off the tallest plunge on Earth.



<h2 class="wp-block-heading" id="h-where-arctic-chill-meets-atlantic-warmth">Where Arctic chill meets Atlantic warmth</h2>



Icy water leaving the Nordic seas is both colder and saltier than the milder Atlantic layer to the south. Density differences created by that contrast drive the flow. 



As the dense water reaches the sill between <a href="https://www.earth.com/image/rare-glimpse-of-iceland-amid-unusual-heatwave/">Iceland</a> and <a href="https://www.earth.com/news/greenland-ice-fossil-tundra-discovery-stuns-and-worries-scientists-sea-level-rise/">Greenland</a>, it spills downward, widening as it falls until the sheet stretches roughly 300 miles - about the driving distance from Chicago to St. Louis.



During the <a href="https://www.earth.com/news/lessons-from-the-ice-age-how-climate-change-reshapes-plant-life/">Last Ice Age</a>, roughly 17,500 to 11,500 years ago, glaciers carved trenches across the seabed and left behind the ridge that now serves as the cataract’s tipping point. 



Glacial debris, <a href="https://www.earth.com/news/rocks-explain-roman-empire-collapse-1500-years-ago-late-antique-little-ice-age/">volcanic eruptions</a>, and relentless currents have since hardened the structure, locking a geological funnel in place for the descending water.



<h2 class="wp-block-heading" id="h-climate-change-and-the-largest-waterfall">Climate change and the largest waterfall</h2>



More than 3.2 million cubic meters of water - around 113 million cubic feet - slip over the cataract every second, far outpacing the Amazon River’s flow into the Atlantic. 



This slide feeds the lower limb of the Atlantic Meridional Overturning Circulation (<a href="https://www.nature.com/articles/s43247-025-02403-0" target="_blank" rel="noreferrer noopener">AMOC</a>), the global “conveyor belt” that ferries heat, oxygen, and nutrients around the planet.



There is increasing evidence of the effects of global change on the phenomenon of undersea waterfalls. 



“A good example is on the <a href="https://www.earth.com/image/the-ebro-river-on-the-northeast-coast-of-spain/">Catalan coast</a>, where the decrease in the number of tramontane days in winter in the Gulf of Lion and north of the Catalan coast is causing a weakening of this oceanographic process, which is decisive in regulating the climate and has a great impact on deep ecosystems,” explains marine scientist <a href="https://www.researchgate.net/profile/Anna-Sanchez-Vidal" target="_blank" rel="noreferrer noopener">Anna Sanchez Vidal</a>.



<h2 class="wp-block-heading" id="h-size-of-the-denmark-strait-cataract">Size of the Denmark Strait cataract</h2>



<a href="https://en.wikipedia.org/wiki/Angel_Falls" target="_blank" rel="noreferrer noopener">Angel Falls</a> drops 3,212 feet in Venezuela. Niagara clears a modest 167 feet on the U.S.-Canada border. Stack all of Niagara’s water several dozen times, and you still won’t match the cataract’s flow. 



Even the Mississippi at flood stage would struggle. Yet the Denmark Strait cataract remains invisible, its roar muffled by more than a half-mile of seawater.



Instruments tell a different story: moored profilers register velocities topping three knots, while sediment cores show layers rearranged by the hidden torrent.



The phenomenon of dense water overflow is particularly intense in the Arctic and Antarctic. 



<figure class="wp-block-image aligncenter size-full"><a href="https://www.earth.com/wp-content/uploads/2024/12/denmark-strait-cataract_graphic-illustration_credit-NOAA_1m.jpg"><img src="https://www.earth.com/wp-content/uploads/2024/12/denmark-strait-cataract_graphic-illustration_credit-NOAA_1s.webp" alt="In the Denmark Strait, southward-flowing frigid water from the Nordic Seas meets warmer water from the Irminger Sea. The cold, dense water quickly sinks below the warmer water and flows over the huge drop in the ocean floor, creating a downward flow estimated over 123 million cubic feet per second. Credit: NOAA" class="wp-image-1977524"/></a><figcaption class="wp-element-caption">In the Denmark Strait, southward-flowing frigid water from the Nordic Seas meets warmer water from the Irminger Sea. The cold, dense water quickly sinks below the warmer water and flows over the huge drop in the ocean floor, creating a downward flow estimated over 123 million cubic feet per second. Click image to enlarge. Credit: NOAA</figcaption></figure>



“The poles are the regions where most of the dense water masses - generated by the formation of sea ice at the surface - eventually reach the global ocean floor," explains David Amblàs of the <a href="https://www.ub.edu/portal/web/earth-sciences/faculty" target="_blank" rel="noreferrer noopener">Department of Earth and Ocean Dynamics</a> at the University of Barcelona. 



"The polar areas are like the heart of the oceanic circulatory system: they pump cold, dense water into the great oceanic troughs through the ‘heartbeats’ made by overflows of dense water."



<h2 class="wp-block-heading" id="h-much-more-to-learn">Much more to learn</h2>



The cataract may slow or speed up as <a href="https://www.earth.com/news/drastic-warming-will-transform-the-arctic-beyond-recognition/">Arctic warming</a> alters salinity and temperature patterns. Researchers use autonomous gliders, deep-sea landers, and satellite altimetry to watch for any shift that could ripple through weather systems. 



A weakening flow might stall the North Atlantic’s heat pump, cooling Europe and nudging hurricanes onto new tracks.



Yet there is still no direct video of the full descent, and no sensor array captures every eddy. Each expedition peels back only a sliver of the story. 



Future projects aim to stitch those slivers together, mapping the plunge in three dimensions and tracking its pulse through the seasons.



<h2 class="wp-block-heading" id="h-why-earth-s-largest-waterfall-matters">Why Earth's largest waterfall matters</h2>



Anyone enjoying mild January weather or a fish fillet pulled from Icelandic waters owes thanks, in part, to the Denmark Strait cataract. 



By dragging cold, dense water southward, the cataract clears space for warmer <a href="https://www.earth.com/news/weakening-ocean-currents-could-cost-trillions-of-dollars/">Gulf Stream water</a> to flow north. That exchange tempers winter, nourishes plankton, and steers migratory species toward fertile feeding grounds.



When the torrent quickens, more carbon-rich deep water rises elsewhere, boosting ocean productivity. When it slackens, heat piles up in the tropics, whipping up stronger storms. 



In other words, the waterfall no one can see holds a backstage pass to everyday weather and the seafood aisle alike.



From a tourist’s point of view, the cataract offers nothing to watch. From a planetary perspective, it's a crucial lever, tilting climate and commerce with the quiet push of density-driven flow. 



Scientists will keep chasing its rhythm, because the better we know this hidden giant, the better we can forecast the moods of the sea and the sky above it.



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Earth’s largest waterfall, dwarfing all others, is hidden in the ocean

Niagara Falls pulls in tourists by the boatload. Angel Falls...

The Earth spins steadily, but not without a wobble. While we imagine the North and South Poles as fixed points, they’re not exactly anchored. Over time, they shift slightly, influenced by how mass is distributed across the globe. 



Ice sheets melt, tectonic plates shift, and oceans swell. But now, researchers have revealed that humans, through dam building, have also nudged the planet’s spin ever so slightly.



In a quiet but measurable way, our thirst for water control and hydroelectric energy has shifted the Earth's poles. From the earliest major dams in the 19th century to the massive reservoirs constructed in Asia and Africa during the 20th century, the <a href="https://www.earth.com/news/climate-change-is-now-impacting-earths-rotation/">effect</a> has grown stronger. 



According to a study published in the journal Geophysical Research Letters, this phenomenon has moved Earth’s rotational axis by more than a meter (3.3 feet) since 1835.



<h2 class="wp-block-heading" id="h-dam-building-shifts-earth-s-poles">Dam building shifts Earth’s poles</h2>



True polar wander refers to the shifting of <a href="https://www.earth.com/news/magnetic-north-pole-is-moving-faster-than-ever-as-it-races-toward-russia/">Earth</a>’s solid outer shell relative to its spin axis. This motion occurs when mass on the planet’s surface moves around. 



Think of Earth like a spinning basketball. Place a lump of clay on one side, and the ball shifts slightly to balance the extra weight. When this happens on Earth, the solid crust adjusts its position, moving relative to the axis of rotation. The poles then pass through new locations on the surface.



Traditionally, this phenomenon has been linked to natural processes like glacial melting. But the recent study by Natasha Valencic and her team at <a href="https://www.harvard.edu" target="_blank" rel="noreferrer noopener">Harvard University</a> shows that human activity, specifically water impoundment from dam construction, has become another significant contributor. 



The findings suggest that this artificial redistribution of mass has created a measurable shift in the Earth’s pole positions.



“As we trap water behind dams, not only does it remove water from the oceans, thus leading to a global sea level fall, it also distributes mass in a different way around the world,” said Valencic. That mass, once fluid and ocean-bound, is now stored in still reservoirs scattered across continents.



<h2 class="wp-block-heading" id="h-earth-s-poles-moved-in-two-phases">Earth’s poles moved in two phases</h2>



Using data from the Global Reservoir and Dam (GRanD) database, the researchers mapped the water storage of 6,862 artificial reservoirs from 1835 to 2011. The dam analysis revealed a striking, non-linear shift in the Earth’s poles. 



From 1835 to 1954, dam building focused heavily in North America and Europe. This caused the North Pole to move about eight inches toward 103.4°E, a direction passing through Russia and parts of Asia.



After 1954, the pattern of dam construction changed. Major projects emerged across East Africa and Asia. As a result, the pole reversed direction, moving 22.5 inches toward −117.5°E, roughly through the western United States and into the South Pacific. 



These changes did not follow a smooth path. The polar motion was highly variable, influenced by the size and location of dams being built over time.



Across the entire study period, the poles shifted about 44.6 inches. Notably, 40.9 inches of that motion occurred during the 20th century. This finding suggests that modern infrastructure, rather than long-term natural <a href="https://www.earth.com/news/this-is-what-the-total-collapse-of-the-earths-magnetic-field-sounded-like-41000-years-ago/">processes</a> alone, has become a key factor in Earth's orientation.



<h2 class="wp-block-heading" id="h-dams-and-earth-s-pole-positions">Dams and Earth's pole positions</h2>



To track these subtle shifts, the team used a detailed physical model. They combined gravitationally self-consistent sea level theory with equations for rotational stability. 



The researchers accounted for how Earth’s crust responds elastically to mass changes, and how these changes, in turn, influence Earth’s spin.



The Earth model used, known as PREM (Preliminary Reference Earth Model), includes variations in Earth’s density and elasticity. The team also incorporated seepage, the loss of stored water into surrounding soils, using a parameterization method from earlier work by Chao et al. (2008). 



Despite excluding about 28 percent of the <a href="https://www.earth.com/news/earths-magnetic-field-is-shifting-and-putting-navigation-at-risk/">global</a> impoundment volume, mainly from smaller dams, the results remained consistent. 



The missing volume came mostly from minor reservoirs, each contributing less than 0.024 cubic miles, and these had minimal influence on the final polar calculations.



To test the significance of these smaller dams, the team plotted how pole position changed with each added reservoir. After about 6,000 of the largest were included, the results stabilized. This confirmed that the many small, excluded dams had negligible overall effect.



<h2 class="wp-block-heading" id="h-dam-water-storage-and-sea-levels">Dam water storage and sea levels</h2>



Global sea levels are rising today, but during the 20th century, the creation of reservoirs temporarily offset this trend. The researchers found that the 6,862 dams in their study led to a sea level drop of 0.86 inches between 1900 and 2011.



This artificial dip matters. While it’s small compared to the rise caused by melting glaciers and warming oceans, it complicates calculations. 



“Depending on where you place dams and reservoirs, the geometry of sea level rise will change. That’s another thing we need to consider, because these changes can be pretty large, pretty significant," said Valencic.



In the first half of the 20th century, the mean polar motion rate from impoundment was about 0.12 inches per year. 



In the second half, it rose to 0.37 inches per year, a threefold increase. The pole's changing pace mirrors the rapid expansion of dam building after 1950.



<h2 class="wp-block-heading" id="h-revisiting-old-assumptions">Revisiting old assumptions </h2>



Previous studies underestimated the effect of dam-induced polar wander. One earlier estimate in 2008 suggested a mean movement of −0.06 inches per year in the east direction and −0.31 inches per year northward across the 20th century.



But Valencic’s team found it was actually −0.12 inches per year and −0.09 inches per year, respectively. This difference matters because it rebalances the budget of polar motion. 



Scientists trying to understand how much glaciers, groundwater, or ocean changes contribute to Earth's spin now have to subtract out the dam effect. Without this correction, estimates about ice loss and sea level rise remain incomplete.



Interestingly, the influence of dam building didn’t act alone in shifting Earth's poles. The researchers also modeled how the oceans responded to displaced water. 



While water impoundment dominated the first half of the century, the second half saw both dam storage and ocean mass redistribution playing nearly equal roles in shaping Earth’s polar path.



<h2 class="wp-block-heading" id="h-subtle-shift-in-earth-s-poles">Subtle shift in Earth's poles</h2>



This study began as a classroom project at Harvard but quickly grew into a deeper investigation of Earth’s shifting balance. It reveals that something as mundane as a dam, one of civilization’s most common tools, has reshaped the geography of our spinning planet.



The pole has not leapt across continents. It has crept, step by engineered step, with every new concrete wall holding back a river. While not disastrous on its own, this shift reveals a truth: our actions reach farther than we often imagine.



Every dam, every floodgate, becomes part of the Earth’s momentum. What we store on land doesn’t just change rivers. It nudges Earth’s rotation, redistributes the weight of water, and contributes silently to a planet that, while spinning, is never truly still.



The study is published in the journal <a href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025GL115468" target="_blank" rel="noreferrer noopener">Geophysical Research Letters</a>.



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Dams built by humans have shifted Earth’s poles

The Earth spins steadily, but not without a wobble. While...

Sediment hidden under ice for millennia is seeing daylight again as glaciers melt. At first, those fresh minerals mop up carbon dioxide. But over time, they switch roles and start leaking gases that trap heat in the air.



<a href="https://geology.ufl.edu/directory/dr-jonathan-martin/">Jonathan Martin</a>’s University of Florida team, along with colleagues from the <a href="https://www.umaryland.edu/">University of Maryland</a> traced that flip in Kobbefjord, Greenland. 



Researchers compared young glacial meltwater with soil water that had been exposed for about 10,000 years. Their <a href="https://www.nature.com/articles/s43247-025-02404-z">work</a> shows why every newly uncovered valley enters a long, slow countdown from sink to source.



<h2 class="wp-block-heading" id="h-after-glaciers-melt-methane-rises">After glaciers melt, methane rises</h2>



Lead author <a href="https://www.umces.edu/andrea-pain">Andrea Pain</a> and co‑author <a href="https://geology.ufl.edu/directory/dr-jonathan-martin/">Jonathan Martin</a> sampled streams that draw melt straight from small glaciers and others fed by seeps through mature tundra soils. 



The two waters could be told apart by their oxygen isotopes and by how clear they were. Meltwater ran chalky with rock flour, while seep water ran tea‑colored from dissolved organics.



“Our central hypothesis was that the transfer of <a href="https://www.earth.com/news/greenhouse-gas-emissions-reach-another-all-time-high/">greenhouse gases</a> between landscapes and the atmosphere has changed since the Last Glacial Maximum about 15,000 years ago,” said Martin.



Field data upheld that hunch, showing glacial streams still scrubbing carbon dioxide while older soils were busy making methane.



Freshly ground carbonates and silicates react with carbonic acid in cold meltwater, locking up carbon as bicarbonate. 



Once microbes colonize the maturing soil, they chew on buried plant matter and turn it into methane through <a href="https://www.sciencedirect.com/topics/earth-and-planetary-sciences/methanogenesis">methanogenesis</a>, reversing the sign of the gas ledger.



<h2 class="wp-block-heading" id="h-glacier-melt-reshapes-gas-timing">Glacier melt reshapes gas timing</h2>



<a href="https://www.earth.com/news/massive-new-source-of-methane-emissions-discovered-glacial-fracking-arctic/">Methane</a> packs a bigger punch than carbon dioxide, trapping about 28 times more heat over a century. <a href="https://www.ncbi.nlm.nih.gov/books/NBK532922/">Nitrous oxide</a>, the third‑place greenhouse gas, is even fiercer, with a global warming potential of 273 on the same scale.



Those numbers mean that a late rise in methane can wipe out the early carbon‑dioxide savings that bare sediment briefly earns. 



<a href="https://www.earth.com/news/climate-models-underestimate-sea-ice-melt-and-global-warming/">Climate models</a> trying to look centuries ahead need that timing baked in, or they risk undercounting the payback later in the game.



Martin’s crew found that the window of net uptake might last only a few centuries in the high Arctic. That’s just a blink compared to the ten‑thousand‑year age of most post‑ice soils. That insight adds a moving target to projections of future warming.



<h2 class="wp-block-heading" id="h-greenland-s-valley-tells-all">Greenland’s valley tells all</h2>



Kobbefjord lies about six miles southwest of Nuuk and covers roughly 12 square miles. Only 1.7 percent of the watershed still holds glacier ice, yet the lingering meltwater strongly flavors the downstream chemistry.



During a clear July stretch, meltwater from nearby glaciers ruled the flow, and carbon dioxide in the main channel stayed close to atmospheric equilibrium. 



A week later, cloudier weather cut the glacier melt pulse; seep water took over, and methane levels at the outlet jumped more than fourfold.



That flip also showed up in the strontium isotope gap between water and bedload sediment, a geochemical clock for weathering progress. 



Values near zero in seep streams told of <a href="https://www.earth.com/news/water-and-ice-may-reveal-where-rare-earth-elements-are-hiding/">minerals</a> already well chewed, while high values in the icy headwaters marked rock that had barely started to dissolve.



Field calculations revealed a net sink of 64 millimoles of carbon dioxide equivalents per second during the melt‑dominated period. 



Just days later, the same outlet turned into a 44-millimole-per-second source as methane outran the shrinking weathering sink.



<h2 class="wp-block-heading" id="h-reading-the-gases">Reading the gases</h2>



<a href="https://www.earth.com/news/massive-study-provides-answers-to-how-coral-reefs-can-survive-climate-change/">Carbonic acid weathering</a> of carbonates and silicates pulls carbon from the air, but sulfuric acid weathering of carbonates can add it back.



The balance between those paths hinges on how much fresh mineral surface and dissolved organic carbon each water source carries.



Runoff from glaciers had lower organic carbon, yet it was more labile, fueling acid generation that sped up mineral reactions. 



Seep water, richer in tougher humic carbon, fostered anaerobic pockets where methane‑making microbes thrived.



The study underscores that <a href="https://www.earth.com/news/greenland-ice-fossil-tundra-discovery-stuns-and-worries-scientists-sea-level-rise/">melting ice</a> and deglaciation is not a single event but a sequence of chemical stages. Understanding which stage a watershed occupies helps predict whether it will cool or warm the planet in any given decade.



<h2 class="wp-block-heading" id="h-warming-builds-after-glacier-melt">Warming builds after glacier melt</h2>



Pain and Martin now plan to test nitrous oxide dynamics in the same valley, because that gas can warm the air <a href="https://www.epa.gov/ghgemissions/nitrous-oxide-emissions" target="_blank" rel="noreferrer noopener">200 times faster</a> than carbon dioxide if it escapes.



Preliminary lab work hints that nitrous oxide might peak earlier than methane, suggesting a still more complex hand‑off among the three gases.



Other researchers are already noticing similar trends elsewhere: on the <a href="https://www.earth.com/news/why-the-roof-of-the-world-keeps-rising-over-time/">Tibetan Plateau</a>, lakes that no longer receive melt from glaciers emit about three times more methane than glacier‑fed lakes.



As more high‑altitude or high‑latitude basins lose ice input, those findings imply a widespread tilt toward methane dominance.



Martin cautions that rapid, human‑driven warming could briefly revive the negative feedback by boosting meltwater flow. 



Yet the reprieve would be short‑lived. Once the last ice patches vanish, soils everywhere will settle into the methane‑rich phase that the Kobbefjord team measured.



The study is published in <a href="https://www.nature.com/articles/s43247-025-02404-z" target="_blank" rel="noreferrer noopener">Communications Earth &amp; Environment</a>.



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Land exposed by melting glaciers transforms into a greenhouse gas emitter

Sediment hidden under ice for millennia is seeing daylight again...

A four week voyage across the North Atlantic has uncovered a pollutant so small that standard nets could never snag it. Researchers found that plastic particles under one micrometer, known as nanoplastics, saturate ocean water from the Azores to Europe.



When the team scaled their measurements up, they calculated roughly <a href="https://www.nature.com/articles/s41586-025-09218-1" target="_blank" rel="noreferrer noopener">twenty seven million tons</a> of these specks floating in the top 650 feet of the North Atlantic, rivaling every estimate of larger debris for the entire world <a href="https://www.earth.com/news/ocean-plastic-crisis-goes-way-deeper-than-we-thought/">ocean</a>.



This estimate comes from geochemist Helge Niemann of the <a href="https://www.nioz.nl/en" target="_blank" rel="noreferrer noopener">Royal Netherlands Institute for Sea Research</a> and <a href="https://www.uu.nl/" target="_blank" rel="noreferrer noopener">Utrecht University</a>, who worked with graduate student Sophie ten Hietbrink aboard the research vessel RV Pelagia.



<h2 class="wp-block-heading" id="h-detecting-invisible-plastic-particles">Detecting invisible plastic particles</h2>



Ten Hietbrink drew two‑liter samples at twelve stations, collecting <a href="https://www.earth.com/news/world-environment-day-2025-plastic-pollution-is-choking-our-planet/">water</a> from the surface, 3,300 feet, and near the seabed. She passed each sample through filters finer than a red blood cell.



Back in the Utrecht lab, the residue was baked inside a proton transfer reaction mass spectrometer, a device that fingerprints polymers by the gases they release. “By drying and heating the remaining material, we were able to measure the characteristic molecules of different types of plastics,” noted Ten Hietbrink.



The approach allowed the crew to log <a href="https://www.sciencedirect.com/topics/earth-and-planetary-sciences/polyethylene-terephthalate" target="_blank" rel="noreferrer noopener">polyethylene terephthalate</a>, polystyrene, and polyvinyl chloride even at 15,000‑foot depths. Every vial, no matter its origin, contained plastic.



Because the mass spectrometer ignores <a href="https://www.earth.com/news/ai-algorithms-can-increase-ocean-plastic-cleanup-efficiency/">pieces</a> above one micrometer, the expedition focused exclusively on bits far smaller than conventional <a href="https://oceanservice.noaa.gov/facts/microplastics.html" target="_blank" rel="noreferrer noopener">microplastic</a>, the fragments between one micrometer and five millimeters often photographed on beaches.



<h2 class="wp-block-heading" id="h-shocking-amount-of-ocean-plastic">Shocking amount of ocean plastic</h2>



When the numbers from each station were extended across latitudes eight to fifty-five degrees north, the tally reached masses never before assigned to <a href="https://www.earth.com/news/coca-cola-may-dump-1-3b-pounds-plastic-into-oceans-by-2030/">plastic</a> pollution. The final figure equals the combined cargo of almost 2,000 container ships.



Niemann described the result as a shocking amount and explained that it finally answers the puzzle of missing plastic that production statistics could not account for.



“There is more plastic in the form of nanoparticles floating in this part of the ocean than there is in larger particles floating in the Atlantic or even all the world's oceans,” said Niemann.



The data also reshape the popular image of ocean garbage patches. Nets that trap bottle caps and food wrappers sample only a thin veneer; the bulk of the load is invisible and dispersed.



Within the <a href="https://oceanservice.noaa.gov/facts/gyre.html" target="_blank" rel="noreferrer noopener">North Atlantic subtropical gyre</a>, currents corral microplastics at the surface, yet the researchers found the highest nanoplastic concentrations closer to the European shelf, hinting at strong land-based sources.



The nanoplastic concentration dropped by roughly one half at 3,300 feet, and fell to about a third of surface levels near the seabed - yet plastic still appeared at every depth.



<h2 class="wp-block-heading" id="h-nanoplastics-harm-animals-and-humans">Nanoplastics harm animals and humans</h2>



Laboratory and clinical <a href="https://www.sciencedirect.com/science/article/pii/S0160412022001258" target="_blank" rel="noreferrer noopener">studies</a> show that particles smaller than a micrometer can slip past the intestinal lining and enter the bloodstream, where they appear in human blood samples.



Once circulating, they can also cross the <a href="https://pubmed.ncbi.nlm.nih.gov/35302003/" target="_blank" rel="noreferrer noopener">blood‑brain barrier</a>, ferrying other contaminants into nervous tissue - as demonstrated in mice.



Marine life confronts the same risk. Bacteria may mistake nanoplastics for food, zooplankton ingest them, and the particles ascend the food web to fish and seabirds.



A recent <a href="https://pubmed.ncbi.nlm.nih.gov/30861380/" target="_blank" rel="noreferrer noopener">meta‑analysis</a> concludes that smaller pieces accumulate more readily than larger debris and may trigger oxidative stress in cells.



Field experiments in the Mediterranean have linked nanoplastic exposure to reduced filtration rates in farmed <a href="https://pubmed.ncbi.nlm.nih.gov/37379876/" target="_blank" rel="noreferrer noopener">filter feeder mussels</a>, a sector worth more than $4 billion to coastal economies.



Economic losses could rise if shellfish accumulate particles that lower growth or market appeal, adding a financial dimension to what was once viewed solely as an environmental issue.



<h2 class="wp-block-heading" id="h-where-the-fragments-come-from">Where the fragments come from</h2>



Sunlight bleaches and cracks larger items at the surface, eventually grinding them into nanoscale dust. River mouths add steady plumes of city trash each day.



The air itself delivers particles. Atmosphere monitors detect plastic aerosols over both continents and oceans, which settle by rainfall or dry deposition.



Once in seawater, nanoplastics no longer obey buoyancy rules. Their motion is governed by <a href="https://pmc.ncbi.nlm.nih.gov/articles/PMC11905425/" target="_blank" rel="noreferrer noopener">Brownian motion</a>, letting them drift vertically and reach depths where light never penetrates.



Sediment cores from the deep <a href="https://pmc.ncbi.nlm.nih.gov/articles/PMC10919090/" target="_blank" rel="noreferrer noopener">North Pacific</a> and equatorial trenches already hold threads of polyester and shards of polyvinyl chloride, proving that tiny plastics sink or hitchhike on marine snow to the seabed.



<h2 class="wp-block-heading" id="h-types-of-ocean-plastic-still-unclear">Types of ocean plastic still unclear</h2>



Curiously, the expedition detected no nanoparticles of polyethylene or polypropylene, the two polymers that dominate surface trash. Niemann suspects chemical weathering may hide their fingerprints, or the fragments may degrade faster than they form.



Future cruises will test other oceans and refine techniques to reveal modified polymers, because the Atlantic is unlikely to be unique.



Researchers also need time‑series records to track whether nanoplastic levels continue climbing or have reached a plateau.



Equally urgent is understanding how mixtures of plastic and natural organic matter interact, potentially altering toxicity.



<h2 class="wp-block-heading" id="h-choosing-prevention-over-cleanup">Choosing prevention over cleanup</h2>



Niemann stresses that the particles already adrift are beyond recovery; their size makes skimming devices useless. The logical path is to curb new emissions.



Several countries now restrict the use of microbeads in cosmetics and plan to phase out certain single‑use items, yet production of virgin plastic keeps rising faster than recycling capacity.



Standardized monitoring that includes nanoscale particles would give policymakers a clearer target and let them judge whether interventions are working.



Citizen science beach cleanups, while unable to net nanoparticles, still remove items that would otherwise weather into new fragments, providing a frontline defense against future invisible pollution.



The study is published in the journal <a href="https://www.nature.com/articles/s41586-025-09218-1" target="_blank" rel="noreferrer noopener">Nature</a>.



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Nanoplastic particles have infiltrated the ocean's food web at the most important levels

A four week voyage across the North Atlantic has uncovered...

Humans generated about 485 billion pounds of plastic waste in 2024 - an amount so large it's incredibly difficult to comprehend. One quick drink or single shipment box often lingers for centuries, so researchers keep hunting for materials that disappear safely after use. 



Now <a href="https://www.me.uh.edu/faculty/rahman-maksud" target="_blank" rel="noreferrer noopener">Maksud Rahman</a>, a mechanical engineer at the <a href="https://www.uh.edu/" target="_blank" rel="noreferrer noopener">University of Houston</a>, and collaborators at <a href="https://www.rice.edu/" target="_blank" rel="noreferrer noopener">Rice University</a> <a href="https://www.nature.com/articles/s41467-025-60242-1" target="_blank" rel="noreferrer noopener">report</a> bacterial cellulose sheets that rival <a href="https://www.earth.com/news/quantum-material-could-make-computers-1000-times-faster/">metal</a> for strength yet compost like paper.



<h2 class="wp-block-heading" id="h-why-bacterial-cellulose-sheet-is-useful">Why bacterial cellulose sheet is useful</h2>



This <a href="https://www.sciencedirect.com/topics/biochemistry-genetics-and-molecular-biology/biopolymer" target="_blank" rel="noreferrer noopener">biopolymer</a> is spun outside the cell wall of species such as <a href="https://www.ncbi.nlm.nih.gov/Taxonomy/Browser/wwwtax.cgi?mode=Info&amp;id=436" target="_blank" rel="noreferrer noopener">Novacetimonas hansenii</a>, forming ribbons only a few nanometers thick that lock together like Velcro and can reach <a href="https://www.sciencedirect.com/topics/biochemistry-genetics-and-molecular-biology/tensile-strength" target="_blank" rel="noreferrer noopener">tensile strength</a> values above 400 MPa.



Because the fiber network is pure, porous, and matches human tissue chemistry, clinicians already <a href="https://pmc.ncbi.nlm.nih.gov/articles/PMC9963514/" target="_blank" rel="noreferrer noopener">test</a> it as a transparent wound covering that eases pain and speeds healing.



<h2 class="wp-block-heading" id="h-microbes-build-strong-sheets">Microbes build strong sheets</h2>



“We envision these strong, multifunctional and eco‑friendly bacterial cellulose sheets becoming ubiquitous, replacing plastics in various <a href="https://www.earth.com/news/scientists-create-a-two-dimensional-carbon-material-eight-times-stronger-than-graphene/">industries</a> and helping mitigate environmental damage,” said Rahman.



Guided by a slow, continuous spin inside an oxygen‑permeable cylinder, the bacteria swim in one direction and lay each thread side‑by‑side, turning random mats into ordered cables that reach 436 MPa and a 32 GPa modulus.



“The resulting bacterial cellulose sheets display high tensile strength, flexibility, foldability, optical transparency, and long‑term mechanical stability,” noted doctoral researcher <a href="https://scholar.google.com/citations?user=Emevh2EAAAAJ&amp;hl=en" target="_blank" rel="noreferrer noopener">M.A.S.R. Saadi</a>.



<h2 class="wp-block-heading" id="h-boosting-bacterial-cellulose-sheet">Boosting bacterial cellulose sheet</h2>



The team then mixed in <a href="https://www.nature.com/articles/s41699-021-00231-2" target="_blank" rel="noreferrer noopener">hexagonal boron nitride</a> flakes, a 2‑D material whose <a href="https://www.sciencedirect.com/topics/materials-science/youngs-modulus" target="_blank" rel="noreferrer noopener">Young’s modulus</a> hovers near 0.8 TPa and whose <a href="https://www.sciencedirect.com/topics/materials-science/thermal-conductivity" target="_blank" rel="noreferrer noopener">thermal conductivity</a> can exceed 700 W m⁻¹ K⁻¹.



With the flakes wedged between cellulose ribbons, strength jumped to 553 MPa while heat dissipated three times faster, leading Rahman to call the single‑step process “a scalable, flexible biosynthesis method with various nanomaterials.”



<h2 class="wp-block-heading" id="h-uses-of-bacterial-sheet-in-real-life">Uses of bacterial sheet in real life</h2>



A sheet this tough could fold into a disposable water bottle, line a shipping pouch, or reinforce fiber‑based electronics without shedding microplastic shards.



Biomedical companies eye the same platform for burn dressings and tissue scaffolds, since bacterial cellulose absorbs fluid yet releases it slowly enough to keep wounds moist.



Petroleum‑based plastics <a href="https://www.sciencedirect.com/science/article/pii/S2405844021020211" target="_blank" rel="noreferrer noopener">persist</a> precisely because their carbon backbone resists microbial attack, whereas cellulose breaks down under ordinary composting <a href="https://www.earth.com/news/graphene-wonder-material-changing-the-world-is-officially-declared-safe-for-humans/">conditions</a> and spares the atmosphere extra fossil‑derived CO₂.



<h2 class="wp-block-heading" id="h-holding-up-over-time">Holding up over time</h2>



Yield now sits around 7.5 mg day⁻¹ in a lab reactor; industrial drums must multiply that figure without tilting the delicate oxygen balance the microbes require.



Boron nitride adds cost and mining footprints, so engineers will test other mineral plates or even plant‑derived nanofibers that could supply similar stiffness at lower price.



Durability testing showed the rotational <a href="https://www.sciencedirect.com/topics/biochemistry-genetics-and-molecular-biology/bacterial-cellulose" target="_blank" rel="noreferrer noopener">bacterial cellulose</a> sheets maintained their shape and strength even after 10,000 mechanical loading cycles. 



Under stress conditions simulating real-world fatigue, their structure stayed intact with no visible fractures or surface separation.



The material’s response to repeated tension suggests it could handle long-term use in flexible electronics, medical devices, or lightweight load-bearing applications where both elasticity and <a href="https://www.earth.com/news/new-ai-designed-material-is-light-as-foam-tough-as-steel/">toughness</a> are essential.



<h2 class="wp-block-heading" id="h-mixing-in-other-materials-for-new-traits">Mixing in other materials for new traits</h2>



The team used <a href="https://www.nature.com/articles/s41699-021-00231-2" target="_blank" rel="noreferrer noopener">boron nitride nanosheets</a> to enhance strength and thermal conductivity, but the same setup could accept other additives. 



Materials like <a href="https://www.earth.com/news/graphene-wonder-material-changing-the-world-is-officially-declared-safe-for-humans/">graphene oxide</a>, cellulose nanocrystals, or clay nanosheets might bring conductivity, flame resistance, or moisture control depending on the use case.



Because the bacteria spin cellulose in real time, the added particles get embedded directly into the fiber network. 



This lets researchers customize each sheet’s behavior during growth, rather than requiring extra manufacturing steps after production.



Life‑cycle assessments, regulatory scrutiny, and consumer perception studies still lie ahead, yet the flow‑guided approach hints at a future where packaging strength no longer means permanent pollution.



<h2 class="wp-block-heading" id="h-how-to-scale-bacterial-sheet-production">How to scale bacterial sheet production</h2>



Right now, the setup uses a <a href="https://suigenerisbrewing.com/index.php/2024/06/14/diy-culture-rotator/" target="_blank" rel="noreferrer noopener">custom-built rotational culture device</a> that spins at 60 rpm and yields about 7.5 mg of dry material per day. 



That works for lab testing, but industrial applications will need much larger volumes and faster throughput.



To scale up, engineers will have to optimize oxygen flow, nutrient cycling, and bacteria strain performance while keeping alignment intact. 



If successful, the method could be adapted to existing fermentation or bioreactor infrastructure with minor retrofitting.



<h2 class="wp-block-heading" id="h-bacterial-cellulose-sheet-vs-plastic-and-metal">Bacterial cellulose sheet vs plastic and metal</h2>



Aligned bacterial cellulose sheets already outperform many commercial polymers and glass when mapped on <a href="https://www.sciencedirect.com/topics/materials-science/material-selection-chart" target="_blank" rel="noreferrer noopener">Ashby plots</a> comparing tensile strength and Young’s modulus to density. 



These charts show the material achieving stiffness values close to some metals while remaining far lighter.



That balance of strength and low weight could make it attractive for aerospace, structural packaging, or thermal insulation where reducing load matters but performance cannot be compromised.



The study is published in <a href="https://www.nature.com/articles/s41467-025-60242-1.epdf" target="_blank" rel="noreferrer noopener">Nature Communications</a>.



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Scientists think their biotech breakthrough could end plastic waste forever

Humans generated about 485 billion pounds of plastic waste in...

Snowpack once reliably fed water into the Colorado River, yet winter precipitation across the Four Corners has dropped by roughly 23 percent since 1980. Reservoirs and ranchers feel the strain each spring.



Researchers have linked the ongoing shortage of rain directly to a warming Pacific and to <a href="https://www.nature.com/articles/s41561-025-01728-x">anthropogenic aerosols</a> - tiny pollution particles that alter atmospheric circulation. 



The evidence shows that drought conditions in the American Southwest are now effectively locked in as the climate continues to warm.



<h2 class="wp-block-heading" id="h-megadrought-becomes-the-new-normal">Megadrought becomes the new normal</h2>



“What we find is that precipitation is more directly influenced by climate change than we previously thought, and precipitation is pretty sensitive to these external influences that are caused by humans,” said Flavio Lehner, assistant professor of Earth and Atmospheric Sciences at <a href="https://cornellbigred.com/">Cornell University</a>.



Professor Lehner’s team combed through decades of climate‑model runs to untangle overlapping drivers.



Tree‑ring reconstructions show that the current Southwest megadrought is the driest 22‑year span since at least 800 CE. The finding puts today’s water crisis in a millennium‑scale context.



Lower precipitation, not just higher temperatures, sets this megadrought apart because it saps <a href="https://www.earth.com/news/how-soil-moisture-can-predict-severe-storms/">soil moisture</a> before summer even starts. That early‑season deficit undercuts the snowpack that supplies two‑thirds of regional river flow.



<h2 class="wp-block-heading" id="h-pollution-alters-storm-paths">Pollution alters storm paths</h2>



“In our models, if we see a warming trend in the tropical <a href="https://www.earth.com/news/pacific-sea-levels-are-rising-faster-than-anywhere-in-the-world/">Pacific</a>, we would expect more precipitation in the Southwestern United States - but that’s not the case here,” said Yan‑Ning Kuo, doctoral student at Cornell University.



Her point underscores the role that pollution‑driven circulation changes play in overriding ocean patterns.



Particles from coal burning, industrial smokestacks, and vehicle exhaust in East Asia rise into the atmosphere and scatter sunlight, cooling the surface and nudging the jet stream northward. 



That shift encourages a persistent high‑pressure ridge over the North Pacific that deflects winter storms away from Arizona, New Mexico, and Southern California.



China’s air‑quality campaign cut average <a href="https://www.sciencedirect.com/science/article/pii/S2590332221001081">PM2.5 levels</a> by about one‑third between 2013 and 2019. Still, the Cornell team warns that rising greenhouse gases will overpower those short‑term gains.



<h2 class="wp-block-heading" id="h-pacific-can-t-deliver-rain">Pacific can’t deliver rain</h2>



In a typical <a href="https://www.pmel.noaa.gov/elnino/what-is-la-nina">La Niña</a>, cooler Pacific waters push the jet stream north, leaving the Southwest dry. Conversely, <a href="https://www.usgs.gov/faqs/what-el-nino-and-what-are-its-effects">El Niño</a> usually drapes moisture over the region, yet models show that warming and aerosols erase that benefit.



A <a href="https://www.climate.gov/news-features/blogs/enso/enso-and-southwest-united-states-megadrought">teleconnection</a> is a long‑distance link between climate features, and the new analysis finds that the Pacific‑to‑Southwest link has weakened. That subtle change allows a stubborn North Pacific high‑pressure system to settle in more often.



Between 1980 and 2014, soil moisture in the Southwest declined faster than at any other time in the past century, dropping by about 0.15 inches per decade. Less moisture in the ground means more summer heat spikes, as dry soils can’t cool the air through evaporation.



<h2 class="wp-block-heading" id="h-water-stress-is-locked-in">Water stress is locked in</h2>



Lake Mead, the nation’s largest reservoir, has hovered at just 35 percent of capacity for three straight years. Mandatory cutbacks on <a href="https://www.earth.com/news/colorado-river-basin-has-lost-enough-water-to-fill-lake-mead/">Colorado River</a> allocations kicked in after the lake dropped below 1,075 feet.



<a href="https://www.ipcc.ch/report/ar6/wg1/chapter/chapter-8/">IPCC models</a> project that every 1.8°F of global warming could trim cool‑season precipitation in the Southwest by another four percent. That figure mounts because a warmer atmosphere pulls extra water from soils and plants, intensifying drought even if rain totals held steady.



Cities from Phoenix to Albuquerque already rely on indoor conservation and reclaimed water to stretch supplies. But climate‑induced precipitation losses eat into the margin of safety those programs provide.



<h2 class="wp-block-heading" id="h-slowing-the-southwest-megadrought">Slowing the Southwest megadrought</h2>



Sulfur‑cutting fuel rules and clean‑energy mandates have begun shrinking <a href="https://www.earth.com/news/reducing-aerosol-pollution-ironically-causes-more-wildfires/">aerosol emissions</a> from ships and factories. Cleaner air could, in theory, ease the North Pacific high and let more storms through.



The Cornell study warns that warming trends across the tropics may soon override any aerosol relief. Warmer seas pump extra heat into the atmosphere, reinforcing the pattern that steers wet winter systems elsewhere.



Scientists suggest ramping up soil‑moisture monitoring and forest‑thinning projects so managers can react quickly to dry spells. Improved early‑warning tools could buy precious time for farmers and power grid operators. 



For now, the Southwest must plan for decades of megadrought, not just dry years. Water managers, residents, and policymakers face a future where every raindrop matters.



The study is published in <a href="https://www.nature.com/articles/s41561-025-01728-x">Nature Geoscience</a>.



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Why the Southwest megadrought is here to stay

Snowpack once reliably fed water into the Colorado River, yet...

Many expect warmer winters to reduce cold snaps, but that isn't how it works. A new study reveals that the polar vortex, happening high in the stratosphere, still controls much of what happens at ground level.



In this study, scientists looked at how changes in that polar vortex - especially in the stratosphere (a layer of the atmosphere way above us) - affect winter weather in the U.S. 



They discovered that the shape and strength of the vortex at two different heights can look totally different, and this matters a lot.



The study was conducted by researchers from the <a href="https://www.uml.edu" target="_blank" rel="noreferrer noopener">University of Massachusetts Lowell</a>, <a href="https://en.huji.ac.il/" target="_blank" rel="noreferrer noopener">Hebrew University</a> of Jerusalem,&nbsp;and the Massachusetts Institute of Technology (<a href="https://www.mit.edu" target="_blank" rel="noreferrer noopener">MIT</a>).



“The public often hears about the ‘polar vortex’ when winter turns severe, but we wanted to dig deeper and understand how variations within this vortex affect where and when extreme cold hits,” the research team explained.



<h2 class="wp-block-heading" id="h-understanding-the-polar-vortex">Understanding the polar vortex</h2>



Imagine the atmosphere above the North Pole as a swirling dome of icy air - that’s the polar vortex, officially called the stratospheric polar vortex (<a href="https://www.climate.gov/news-features/understanding-climate/understanding-arctic-polar-vortex" target="_blank" rel="noreferrer noopener">SPV</a>). 



When it’s strong and stable, winter in the U.S. tends to stay fairly calm. But when this vortex gets stretched, twisted, or broken apart, cold air can spill southward, triggering severe winter weather across the country.



This study dug into how different shapes and behaviors of the polar vortex - not just at one level of the atmosphere but at two - affect winter storms in the U.S. 



Over the last decade, the worst <a href="https://www.earth.com/news/astonishing-global-heat-in-january-2025-defied-climate-expectations/">cold snaps</a> have been hitting farther west than before. That shift seems to line up with more frequent La Niña events - times when the Pacific Ocean is cooler than usual. 



La Niña tends to favor the version of the vortex that affects the western U.S., while El Niño, its warmer sibling, leans more toward the version that affects the east.



<h2 class="wp-block-heading" id="h-different-types-of-polar-vortexes">Different types of polar vortexes</h2>



The researchers used a technique called <a href="https://stanford.edu/~cpiech/cs221/handouts/kmeans.html" target="_blank" rel="noreferrer noopener">K-means clustering</a> (basically, pattern detection in big datasets) to spot five different types of stratospheric behavior. 



Two of these polar vortex classes stood out because they often came with extreme cold and snow.



One pattern (called P2) leads to severe weather in the Northwest U.S.. The other (P3) hits the Central and Eastern regions of the U.S.



P2 features a strong vortex centered over the pole with a stretched lower vortex. It often brings snow and cold to the Northwestern U.S. 



P3 shows a weaker, displaced vortex toward the North Atlantic, steering cold into the Central and Eastern U.S. These variations do not just depend on vortex position but also on how atmospheric waves behave.



Planetary waves can either be absorbed or reflected in the stratosphere. When reflected, they can send cold air barreling southward. 



P3 events consistently show this reflection during the cold wave itself. P2 events often have wave reflection before the <a href="https://www.earth.com/news/climate-equation-predicts-a-rapid-rise-in-extreme-heatwaves/">cold</a> snap hits.



<h2 class="wp-block-heading" id="h-where-the-cold-hits-and-why">Where the cold hits and why</h2>



The researchers used the <a href="https://ui.adsabs.harvard.edu/abs/2024EGUGA..26.2134C/abstract" target="_blank" rel="noreferrer noopener">rAWSSI index</a>, which considers temperature, snow depth, and snowfall.



The analysis revealed that P3 patterns produce the most extreme winter conditions in the Central and Eastern U.S., while P2 patterns primarily affect the Northwestern region with intense cold and snowfall. 



The findings help explain recent cold events, including the severe <a href="https://www.ncei.noaa.gov/news/great-texas-freeze-february-2021" target="_blank" rel="noreferrer noopener">Texas freeze of 2021</a>.



The Northwest has seen more P2 days recently. This increase matches a northwestward shift in cold air <a href="https://www.earth.com/news/global-warming-is-accelerating-beyond-control-as-co2-levels-rise/">outbreaks</a>. The central and eastern parts still get hit, but less often now.



Wave activity flux (WAF) offers clues. Before P2 events, reflection happens over Siberia and Alaska. During P3 events, strong reflection occurs over Asia and the Pacific. In P3, this reflection continues as the cold air descends.



Cold air starts in the east, spreads across the Midwest, and settles in the Northwest. These transitions help forecast where the next cold wave might land.



<h2 class="wp-block-heading" id="h-global-cycles-and-the-polar-vortex">Global cycles and the polar vortex</h2>



P2 is more frequent during La Niña conditions. P3 prefers El Niño phases. This suggests tropical ocean <a href="https://www.earth.com/news/earth-is-on-pace-to-surpass-1-5c-global-temperature-increase-for-second-year-in-a-row/">temperatures</a> influence how the polar vortex behaves.



Other climate patterns play a role as well. The westerly phase of the Quasi-Biennial Oscillation (<a href="https://www.sciencedirect.com/topics/earth-and-planetary-sciences/quasi-biennial-oscillation" target="_blank" rel="noreferrer noopener">QBO</a>) often coincides with P2 days.



On the other hand, the Arctic Oscillation (<a href="https://en.wikipedia.org/wiki/Arctic_oscillation" target="_blank" rel="noreferrer noopener">AO</a>) tends to be more negative during P3 events, a state that supports increased cold outbreaks in the Central and Eastern United States.



<h2 class="wp-block-heading" id="h-winter-cold-is-shifting">Winter cold is shifting</h2>



What makes this research unique is that it doesn’t just focus on surface temperatures like most studies. It includes snow cover and snowfall, too, giving a fuller picture of how the stratosphere connects to what we experience on the ground. 



Despite a warming climate, these findings suggest extreme cold will continue to return each year, even though its location may shift. In the past decade, the coldest anomalies moved westward, which is a change from decades of more common Eastern U.S. cold.



This deeper understanding could help forecasters predict harsh winter conditions weeks in advance by watching patterns in the stratosphere and tropical oceans.



In the end, this study shows that what happens high above the Earth - and even far across the ocean - can shape the winter weather we feel in a big way. And by getting better at reading those signals from way up in the sky, we might get better at preparing for the coming storms.



-----



The research was funded by the&nbsp;National Science Foundation (<a href="https://www.nsf.gov/" target="_blank" rel="noreferrer noopener">NSF</a>)&nbsp;, the&nbsp;U.S.–Israel Binational Science Foundation (<a href="https://www.bsf.org.il/" target="_blank" rel="noreferrer noopener">BSF</a>)&nbsp;, the&nbsp;U.S. Department of Energy (<a href="https://www.doe.gov/" target="_blank" rel="noreferrer noopener">DOE</a>)&nbsp;, and the&nbsp;National Oceanic and Atmospheric Administration (<a href="https://www.noaa.gov/" target="_blank" rel="noreferrer noopener">NOAA</a>).



The study is published in the journal <a href="https://www.science.org/doi/10.1126/sciadv.adq9557" target="_blank" rel="noreferrer noopener">Science Advances</a>.



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Why global warming hasn't ended extreme winter cold, and why you shouldn't expect it to

Many expect warmer winters to reduce cold snaps, but that...

As oceans heat up, coastal sharks are adjusting their calendars. Instead of swimming south in early fall, many are now sticking around longer due to global warming. 



Researchers at <a href="https://www.stonybrook.edu" target="_blank" rel="noreferrer noopener">Stony Brook University</a> tracked this trend by following six shark species along the U.S. East Coast. They used acoustic tags and detection models to uncover how ocean warming delays the sharks’ southern migrations by up to 29 days.



"Both temperature and photoperiod (length of sunlight) influenced the timing of the <a href="https://www.earth.com/news/greenland-sharks-survive-for-centuries-in-icy-waters/">sharks</a>’ southernly migration, and it is likely that they both cumulatively influence migratory patterns,” said lead author Maria Manz.



<h2 class="wp-block-heading" id="h-sharks-delay-migration-due-to-warming">Sharks delay migration due to warming</h2>



The study observed blacktip, dusky, sand tiger, sandbar, thresher, and white <a href="https://www.earth.com/news/how-the-sharks-body-grows-with-geometric-precision/">sharks</a>. Among them, sandbar sharks showed the longest delay of up to 29 days. They also used the widest range of latitudinal zones, from the New England Shelf to Florida.



White sharks, by contrast, showed the least delay. Being partially warm-bodied (regional endotherms), they are less dependent on external temperature shifts. Their migration changed by only one day under future climate scenarios.



<h2 class="wp-block-heading" id="h-east-coast-is-warming-fast">East Coast is warming fast</h2>



The study focused on the Mid-Atlantic Bight. This region, especially the New York Bight and New England Shelf, is heating faster than many other parts of the Atlantic. 



According to projections based on the high-emissions SSP5 8.5 scenario, the New England Shelf could warm by over 2°C (3.6°F) by 2049.



This rise in temperature affects not just the water, but everything in it. Fish prey species may move earlier or later, altering food availability for predators like sharks.



“Results of the models suggested that projected increases in SST across decades may delay southern autumn <a href="https://www.earth.com/news/rare-video-footage-of-an-elusive-deep-sea-predator-pacific-sleeper-shark/">migrations</a> of coastal sharks with many species remaining in northern habitats for longer durations," wrote the researchers.



<h2 class="wp-block-heading" id="h-how-sharks-were-tracked-in-warming-waters">How sharks were tracked in warming waters</h2>



The researchers tagged 155 sharks and monitored their movements using over 390 acoustic receivers. These receivers picked up signals from the tags whenever sharks came within 900 meters (2,953 feet).



The sharks’ migrations were tracked across five defined zones: New England Shelf (NES), New York Bight (NYB), Mid-Atlantic (MA), Southern Atlantic (SA) and Florida (FL).



Some species, like sandbar and thresher sharks, appeared in all zones. Others, like white sharks, showed more restricted ranges.



<h2 class="wp-block-heading" id="h-predictors-of-migration-timing">Predictors of migration timing</h2>



To understand what drives sharks to migrate, the researchers fed their data into mixed-effect Cox models. 



The team tested sea surface temperature (SST), photoperiod, and lunar phase. Photoperiod emerged as a consistently strong predictor, especially for thresher <a href="https://www.earth.com/news/shark-skeletons-could-lead-to-technological-innovations/">sharks</a>.



Interestingly, lunar phase had less influence than expected. Only sandbar sharks showed some sensitivity to moonlight patterns. 



Most migration timing was better explained by combinations of light and temperature, which can vary regionally.



<h2 class="wp-block-heading" id="h-warming-delays-and-shark-survival">Warming delays and shark survival</h2>



If sharks delay migration but human activities continue on schedule, it could spell trouble. For example, commercial fishing in the Northeast typically ramps up in the fall. Sharks that remain in the area face a higher risk of accidental catch.



“Our findings suggest that climate change could increase vulnerability to bycatch, particularly in mixed-use areas like the New York Bight,” the authors wrote.



There is also concern that shark diets and reproductive cycles may shift out of sync with prey availability. A mismatch in timing could reduce feeding success or breeding success.



<h2 class="wp-block-heading" id="h-new-strategies-for-a-changing-ocean">New strategies for a changing ocean</h2>



Static conservation policies will not hold up if shark behavior keeps changing. The researchers suggest dynamic management tools, like adjusting fishery closures based on temperature data.



Sandbar sharks, which showed the most migration delay, may require special focus. They are already listed as vulnerable due to previous overfishing and slow reproduction.



Successful conservation now depends on real-time data and predictive modeling. As this study shows, changes in migration are not hypothetical. They are already underway.



<h2 class="wp-block-heading" id="h-shark-migration-is-shifting-with-warming">Shark migration is shifting with warming</h2>



The timing of shark migrations is shifting. Some species are adapting by staying longer in warming northern waters. While that may suit them for now, it raises questions about long-term ecological impacts.



Maria Manz and her team stress the importance of using both regional climate data and shark movement models. Doing so can improve predictions and help managers adjust strategies before the ocean changes even more.



"Our study adds to the growing body of evidence demonstrating how migratory populations will respond to a warming climate, potentially altering regional ecosystem dynamics and exposure to anthropogenic threats."



The research is published in the journal <a href="https://conbio.onlinelibrary.wiley.com/doi/10.1111/cobi.70080" target="_blank" rel="noreferrer noopener">Conservation Biology</a>.



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Warming oceans are changing shark migration patterns

As oceans heat up, coastal sharks are adjusting their calendars....

Central Asia is running faster than nature can keep up. The latest region‑wide audit shows that human claims on land, water, and ecosystem productivity have blown past levels scientists call safe.



The research was led by Professor Duan Weili of the <a href="http://english.egi.cas.cn/" target="_blank" rel="noreferrer noopener">Chinese Academy of Sciences</a> and post‑doctoral researcher Zhu Ziyang. Together with an international team, they tracked six environmental <a href="https://www.earth.com/news/world-water-day-2025-preserving-glaciers-protecting-our-future/">footprints</a> from 2000 to 2020.



<h2 class="wp-block-heading" id="h-asia-s-rising-water-crisis">Asia’s rising water crisis</h2>



Across the five republics the land footprint already triples the share allowed under the down‑scaled <a href="https://www.stockholmresilience.org/research/planetary-boundaries.html" target="_blank" rel="noreferrer noopener">planetary boundaries</a>. Meanwhile, the metric known as <a href="https://wad.jrc.ec.europa.eu/humanappropriation" target="_blank" rel="noreferrer noopener">human appropriation of net primary production</a> climbs even higher. 



Kazakhstan and Uzbekistan are the two biggest borrowers from nature, earning a “priority management” label in the study for their outsized ecological withdrawals.



The <a href="https://www.earth.com/news/new-discovery-water-molecules-will-force-chemistry-textbooks-to-be-rewritten/">pattern</a> is lopsided in another way: more than 80 percent of every footprint originates inside the region, so trade alone cannot solve the crunch. 



Researchers link the spike to rapid population growth and a construction boom fueled by fossil fuel revenues. They also point to an agricultural model inherited from Soviet central planning.



<h2 class="wp-block-heading" id="h-land-use-threatens-wildlife-and-soil">Land use threatens wildlife and soil</h2>



Converting pasture and desert fringe into irrigated farms strips wild vegetation of the carbon it once fixed and fragments habitats needed by pollinators and large herbivores. 



By 2020, Tajikistan’s sustainability ratio for land‑based productivity had climbed above 90 - a level ecologists regard as ecological emergency territory.



Heavy harvesting of photosynthetic energy thins the soil. Downstream, dust storms take over, carrying eroded silt hundreds of miles into parched <a href="https://www.earth.com/news/earths-land-based-water-storage-has-drastically-diminished-and-its-not-being-replaced/">basins</a>. Biodiversity follows the same downward slope, squeezing ancient steppe communities that evolved with far lighter grazing pressure.



<h2 class="wp-block-heading" id="h-asia-s-old-farming-wastes-water">Asia’s old farming wastes water</h2>



Irrigated farming absorbs roughly 90 percent of diverted water, and aging Soviet‑era canals leak about 40 percent of that volume before it ever reaches a field. 



Cotton, the historic export staple, drinks more than twice as much water per pound of lint as winter wheat, further draining the Amu Darya and Syr Darya rivers of Central Asia.



Field trials in the Fergana Valley show that drip lines trimmed water use by 18-42 percent while boosting <a href="https://www.researchgate.net/publication/222181065_Water_use_efficiency_of_irrigated_cotton_in_Uzbekistan_under_drip_and_furrow_irrigation" target="_blank" rel="noreferrer noopener">irrigation efficiency</a> by up to 103 percent. 



Yet only a sliver of cropland currently benefits from such technology, largely because farmers lack capital and clear water‑pricing <a href="https://www.earth.com/news/water-might-have-formed-long-before-galaxies/">signals</a>.



<h2 class="wp-block-heading" id="h-pollution-from-farming-and-factories-nbsp">Pollution from farming and factories&nbsp;</h2>



Greenhouse‑gas <a href="https://longreads.cabar.asia/climatechangecentralasia_en" target="_blank" rel="noreferrer noopener">inventories</a> put the region’s annual emissions near 470 million metric tons of CO2‑equivalent, roughly one percent of the global load. 



Nitrogen fertilizer use has increased alongside emissions, adding 628 million kilograms of reactive nitrogen over two decades. This surge has fueled algal blooms that clog irrigation gates.



<figure class="wp-block-image aligncenter size-full"><a href="https://www.earth.com/wp-content/uploads/2025/07/central-asia_climate-change_illustration_credit-Earths-Future_1m.jpg"><img src="https://www.earth.com/wp-content/uploads/2025/07/central-asia_climate-change_illustration_credit-Earths-Future_1s.webp" alt="Schematic diagram of the main components of human appropriation of net primary production in arid Central Asia. Credit: Earth's Future (2025)" class="wp-image-1977470"/></a><figcaption class="wp-element-caption">Schematic diagram of the main components of human appropriation of net primary production in arid Central Asia. Click image to enlarge. Credit: Earth's Future (2025)</figcaption></figure>



Domestic energy burning, petrochemical refining, and steel production together dominate the carbon tally, leaving little room for expansion without efficiency gains.



Because phosphorus runoff is smaller but more concentrated, it acts as a chronic pulse that degrades reservoir water quality. It also shortens canal life through biofouling.



<h2 class="wp-block-heading" id="h-asia-s-farming-can-save-water">Asia’s farming can save water</h2>



Uzbekistan’s gradual pivot from cotton to wheat and fruit since 2010 has already slowed land‑footprint growth, offering a glimpse of how crop diversification pays ecological dividends. 



Livestock policy is another lever; rotational <a href="https://thescipub.com/abstract/ojbsci.2025.209.218" target="_blank" rel="noreferrer noopener">t</a>r<a href="https://thescipub.com/abstract/ojbsci.2025.209.218" target="_blank" rel="noreferrer noopener">ials</a> in northern Kazakhstan improved pasture biomass and soil organic matter within three seasons, even under heavy stocking rates.



Integrated crop-livestock systems recycle manure locally, cutting both chemical fertilizer demand and methane emissions from open lagoons.



 Precision seeding and deficit‑irrigation scheduling, common in U.S. Southwest farming, could translate readily to the warm, dry climate zones of the Kazakh steppe and the Karshi plain.



<h2 class="wp-block-heading" id="h-simple-solutions-can-save-nature">Simple solutions can save nature</h2>



“Our study shows that Central Asia's environmental pressure mainly stems from its domestic consumption," said study lead author Zhu Ziyang. "That calls for policies like better irrigation and scientific land management to bring development back inside a safe space.”



Canal lining, pressurized pipe networks, and solar‑powered pump retrofits each deliver quick water savings that postpone contentious upstream‑downstream negotiations.



On rangelands, subsidies that reward seasonal rests or herd rotation cost less than reseeding bare hillsides once degradation sets in. 



International lenders have begun to take notice. In May 2025, the World Bank approved a $200 million credit to modernize Uzbekistan’s irrigation and drainage grid. Disbursements are tied to measurable reductions in leaks.



<h2 class="wp-block-heading" id="h-asia-s-future-depends-on-water">Asia’s future depends on water</h2>



Scientists warn that six of nine planetary guardrails are already breached worldwide, so the region’s overshoot lands on a planet with shrinking shared headroom. 



Achieving absolute environmental <a href="https://www.earth.com/news/scientists-urgent-plea-sustainable-climate-solutions-save-earth-humanity/">sustainability</a> will demand that Central Asia cap resource use even as its population edges toward 45 million and summers grow hotter and drier.



How the five republics respond will shape whether future generations inherit a livable, functioning landscape. Their response will determine whether scarce resources are stabilized or continue to unravel under rising demand and outdated systems.



The study is published in the journal <a href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025EF006129" target="_blank" rel="noreferrer noopener">Earth's Future</a>.



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Central Asia has surpassed climate safety limits and now faces 'extreme unsustainability'

Central Asia is running faster than nature can keep up....

<figure class="wp-block-embed is-type-video is-provider-youtube wp-block-embed-youtube wp-embed-aspect-16-9 wp-has-aspect-ratio"><div class="wp-block-embed__wrapper">
https://www.youtube.com/watch?v=WXXGGiynIjs
</div><figcaption class="wp-element-caption">Greenland is not sinking. In fact, it is the opposite.</figcaption></figure>



<h2 class="wp-block-heading" id="h-a-contrasting-climate-response">A contrasting climate response</h2>



Most coastal towns are <a href="https://www.earth.com/news/sinking-land-will-intensify-the-effects-of-rising-sea-levels/" target="_blank" rel="noreferrer noopener">preparing for higher sea levels</a>, but <a href="https://www.earth.com/news/greenland-no-longer-has-to-worry-about-rising-sea-levels/" target="_blank" rel="noreferrer noopener">Greenland presents</a> a different scenario during climate change. The ground there is rising at a remarkable rate. Over the past decade, some areas have lifted about 20 centimeters, which translates to roughly 2 meters per century. This rate significantly exceeds current projections for sea level rise.



<h2 class="wp-block-heading" id="h-geological-rebound-process-through-climate-change">Geological rebound process through climate change</h2>



The mechanism behind this phenomenon is straightforward. As the ice sheet melts, the immense weight is removed from the bedrock, causing the land to rebound upward. This process resembles the way compressed material springs back when pressure is released.



<h2 class="wp-block-heading" id="h-scientific-monitoring-networks">Scientific monitoring networks</h2>



Researchers at the <a href="https://www.dtu.dk/english/" target="_blank" rel="noreferrer noopener">Technical University of Denmark</a> are documenting this uplift using the GNET network, consisting of 61 GPS stations positioned around Greenland's coast. These sensors can detect movement with millimeter precision, providing detailed measurements of the ongoing changes.



The data reveal that current uplift rates exceed the gradual rebound occurring since the last ice age ended approximately 12,000 years ago. This acceleration corresponds directly with increased ice sheet melting rates.



<h2 class="wp-block-heading" id="h-coastal-transformation">Coastal Transformation</h2>



This uplift is actively reshaping Greenland's coastline. New islands and rocky formations, called "skerries," are emerging as previously submerged land surfaces rise above the water level. This represents a notable contrast to global concerns about rising seas.



The study, published in Geophysical Research Letters, demonstrates the varied regional impacts of climate change. While many locations face rising water levels, Greenland's bedrock is literally rising above the surrounding seas.



The full study was recently published in <a href="https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2023GL104851" target="_blank" rel="noreferrer noopener">Geophysical Research Letters</a>.



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Greenland's ground rises while coasts worldwide face higher seas

https://www.youtube.com/watch?v=WXXGGiynIjs Greenland is not sinking. In fact, it is the...

<figure class="wp-block-embed is-type-video is-provider-youtube wp-block-embed-youtube wp-embed-aspect-16-9 wp-has-aspect-ratio"><div class="wp-block-embed__wrapper">
https://www.youtube.com/watch?v=DSM3EVeGHJU
</div><figcaption class="wp-element-caption">Companies like MindStudio help companies train their employees to implement the latest AI Agent building platform.</figcaption></figure>



<h2 class="wp-block-heading" id="h-ai-agent-training-transforms-the-workplace-fear-factor-into-a-competitive-advantage">AI agent training transforms the workplace 'fear factor' into a competitive advantage</h2>



Organizations that offer comprehensive artificial intelligence training to their workers find remarkable value that extends well beyond basic <a href="https://www.earth.com/news/mind-wandering-might-be-more-productive-than-you-think/" target="_blank" rel="noreferrer noopener">productivity improvements</a>. Emerging research demonstrates that carefully crafted AI training programs <a href="https://www.earth.com/news/ai-does-not-replace-human-creativity-but-enhances-it/" target="_blank" rel="noreferrer noopener">enhance</a> corporate performance, lower operational costs, and dramatically improve employee psychological well-being by turning workplace uncertainty into professional empowerment.



<h2 class="wp-block-heading" id="h-addressing-the-widespread-ai-anxiety-crisis-among-us">Addressing the widespread 'AI anxiety' crisis among us</h2>



A staggering 53% of employees expressed concern that the use of AI tools to automate work tasks could make them appear disposable to their employers, according to <a href="https://www.microsoft.com/" target="_blank" rel="noreferrer noopener">Microsoft</a>'s 2024 workplace survey. Such pervasive worry about being substituted by machines has caused what researchers have termed "AI technostress" – a psychological state that can result in occupational burnout and poorer mental well-being.



Data published in <a href="https://www.nature.com/palcomms/" target="_blank" rel="noreferrer noopener">Humanities and Social Sciences Communications</a> showed that belief in AI learning ability was a moderator in the link between technology adoption and work pressure, and higher confidence significantly lowered negative psychological responses. Workers provided ample training to become competent with AI software have significantly lower stress.



Companies like <a href="https://www.mindstudio.ai/" target="_blank" rel="noreferrer noopener">MindStudio</a> have platforms for building what are known as "AI Agents". In essence, AI Agents are simply tools that employees can build for themselves or their teams quickly and inexpensively. MindStudio will even train entire companies, from the CEO on down, at no cost. By letting MindStudio empower employees, companies avoid hiring more IT staff, buying more software, and implementing solutions to problems that do not exist.



MindStudio even has partners locally for companies, like <a href="http://www.dominnus.com" target="_blank" rel="noreferrer noopener">Dominnus</a> with offices in the Carolinas, California, and Denver, to help build AI Agents and support employees as they become resident AI experts for their organization. The training provided by MindStudio is applicable across other AI Agent building platforms as well.



<h2 class="wp-block-heading" id="h-revolutionary-productivity-through-focused-learning">Revolutionary productivity through focused learning</h2>



Organizations that implement large-scale AI training programs achieve dramatic outcomes. Employees performed tasks significantly better when they utilized AI support compared to when they didn't, according to <a href="https://www.nngroup.com/" target="_blank" rel="noreferrer noopener">Nielsen Norman Group</a> research findings. Their study documented productivity increases of 66% for a variety of professional tasks.



Federal Reserve Bank of St. Louis research finds workers record 33% higher productivity in time working with generative AI tools. The benefit is equivalent to 5.4% of work time savings for AI users – around 2.2 hours per week for full-time workers.



<h2 class="wp-block-heading" id="h-psychological-well-being-benefits-through-ai-competence">Psychological well-being benefits through AI competence</h2>



The emotional transformation when employees are provided with proper technology training is a fundamental transformation from fear to professional confidence. A survey of 600 employees across industries, carried out by ScienceDirect, proved that AI capabilities strengthen work environment commitment and improve job satisfaction.



A <a href="https://www.lut.fi/en" target="_blank" rel="noreferrer noopener">LUT University</a> study discovered that AI adoption has no direct effect on workers' well-being but does so indirectly through working conditions like task optimization and safety protocols. Strategically deployed AI that involves correct training can actually increase workplace mental well-being.



<h2 class="wp-block-heading" id="h-from-replacement-anxiety-to-partnership-confidence">From 'replacement anxiety' to 'partnership confidence'</h2>



Although 35% of those interviewed in recent McKinsey studies were concerned about workforce displacement, firms with large-scale training initiatives witness such fears dissipate quickly. The World Economic Forum found that two out of three respondents believe AI competencies will enhance their career prospects and job marketability.



This shift from fear to trust has measurable implications for job satisfaction. Applied Sciences research indicates AI can create tailored wellness programs based on individual employee requirements.



<h2 class="wp-block-heading" id="h-financial-benefits-of-increased-retention">Financial benefits of increased retention</h2>



The mental health advantages of AI learning have a direct impact on organizational bottom lines in the form of a positive feedback cycle with high retention of employees. Recent ROI research validates that artificial intelligence learning has a beneficial impact on employee turnover and satisfaction levels.



PriceWaterhouseCoopers' research documents 20% to 30% improvements in productivity, market speed, and revenue in organizations that attempt systematic AI adoption through comprehensive training.



<h2 class="wp-block-heading" id="h-environmental-advantages-of-ai-enabled-teams">Environmental advantages of AI-enabled teams</h2>



AI training has unforeseen environmental benefits as it makes the work environment more efficient. According to a study in Scientific Reports, the carbon footprint in writing and illustrating work is significantly lower when AI performs it compared to humans. AI software produces 130 to 1,500 times less CO2 equivalent per page of text created than human authors.



In addition, AI-driven remote work functionality significantly reduces environmental impact. Research by Cornell University and Microsoft indicates that remote workers reduce greenhouse gas emissions by up to 54% by not commuting daily to offices. Hybrid workers working remotely two to four days a week can reduce their carbon footprint by 11% to 29%.



<h2 class="wp-block-heading" id="h-cumulative-organizational-advantages">Cumulative organizational advantages</h2>



The compounding gains of better mental well-being, reduced turnover, increased productivity, and environmental benefits flow to enterprises from the pairing. McKinsey analysis estimates the long-term AI potential at $4.4 trillion in incremental productivity growth opportunity from business use cases.



As of now, 75% of knowledge workers globally utilize generative AI, mirroring widespread adoption patterns. Organizations that provide organized training and assistance see the most favorable results in productivity, worker satisfaction, and ecological sustainability.



The research overwhelmingly indicates that companies that invest in proper AI education, like that offered through <a href="https://www.mindstudio.ai" target="_blank" rel="noreferrer noopener">MindStudio</a>, establish win-win scenarios where employees are both more empowered and less stressed, and companies enjoy the gains of increased productivity, reduced turnover, and improved mental health outcomes throughout their workforce.



For more on MindStudio's free AI training for companies, visit the website's of MindStudio and Dominnus from the links below.



The research was published across a variety of peer-reviewed journals, including <a href="https://www.nature.com/palcomms/" target="_blank" rel="noreferrer noopener">Humanities and Social Sciences Communications</a>, <a href="https://www.frontiersin.org/journals/artificial-intelligence" target="_blank" rel="noreferrer noopener">Frontiers in Artificial Intelligence</a>, and <a href="https://www.mdpi.com/journal/applsci">Applied Sciences</a>.



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MindStudio.AI: <a href="https://www.mindstudio.ai" target="_blank" rel="noreferrer noopener">https://www.mindstudio.ai</a>



Dominnus: <a href="https://www.dominnus.com" target="_blank" rel="noreferrer noopener">https://www.dominnus.com</a>

AI agent training boosts mental health and profits

https://www.youtube.com/watch?v=DSM3EVeGHJU Companies like MindStudio help companies train their employees to...

<figure class="wp-block-embed is-type-video is-provider-youtube wp-block-embed-youtube wp-embed-aspect-16-9 wp-has-aspect-ratio"><div class="wp-block-embed__wrapper">
https://www.youtube.com/watch?v=0HDXqTGEmi4
</div><figcaption class="wp-element-caption">Scientists give plants superpowers against bacterial disease</figcaption></figure>



<h2 class="wp-block-heading" id="h-a-natural-solution-to-disease-through-crop-modification">A natural solution to disease through crop modification.</h2>



The agricultural industry stands at a crossroads between productivity and environmental responsibility, and crop modification often carries a negative connotation. While chemical pesticides have long been the go-to solution for crop protection, their harmful effects on ecosystems and human health have prompted scientists to seek alternatives. The recent breakthrough by <a href="https://www.southampton.ac.uk/" target="_blank" rel="noreferrer noopener">University of Southampton</a> researchers offers a promising path forward through the precise manipulation of plant-associated microbial communities.



<h2 class="wp-block-heading" id="h-the-science-behind-microbial-partnerships">The science behind microbial partnerships</h2>



Plants naturally harbor diverse ecosystems of bacteria, fungi, and other microorganisms that function as biological allies. These microscopic partners contribute to disease resistance, nutrient absorption, and stress tolerance. However, until now, scientists lacked the tools to deliberately reshape these communities to enhance crop protection.



The Southampton team's approach centered on <a href="https://www.earth.com/news/engineered-plant-microbiomes-the-future-of-crop-protection/" target="_blank" rel="noreferrer noopener">modifying lignin biosynthesis genes in rice plants</a>. This strategic intervention altered the plant's metabolic output, creating conditions that favored beneficial bacterial populations while suppressing harmful ones. The result was a living defense system embedded within the plant itself.



<h2 class="wp-block-heading" id="h-implications-for-global-food-security">Implications for global food security</h2>



The successful demonstration against Xanthomonas oryzae, the pathogen responsible for bacterial blight in rice, represents more than a laboratory achievement. Rice feeds nearly half the world's population, and bacterial blight causes devastating crop losses annually. Traditional control methods rely heavily on pesticides that contaminate soil and water systems.



<h2 class="wp-block-heading" id="h-looking-beyond-disease-resistance">Looking Beyond Disease Resistance</h2>



While disease protection represents the immediate application, the research framework opens doors to broader agricultural improvements. Future developments could engineer microbiomes to enhance nutrient uptake, reducing dependence on synthetic fertilizers. This dual benefit addresses both crop productivity and environmental sustainability.



<h2 class="wp-block-heading" id="h-the-path-forward">The path forward</h2>



As this technology advances from laboratory to field applications, it promises to reshape sustainable agriculture. The ability to program plants with their own biological defense systems could herald a new era where crops protect themselves naturally, reducing chemical inputs while maintaining yields necessary for global food security.



The study is published in the journal&nbsp;<a href="http://dx.doi.org/10.1038/s41467-023-44335-3" target="_blank" rel="noreferrer noopener">Nature Communications</a>.



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Revolutionizing agriculture through microbiome engineering

https://www.youtube.com/watch?v=0HDXqTGEmi4 Scientists give plants superpowers against bacterial disease A natural...

<figure class="wp-block-embed is-type-video is-provider-youtube wp-block-embed-youtube wp-embed-aspect-16-9 wp-has-aspect-ratio"><div class="wp-block-embed__wrapper">
https://www.youtube.com/watch?v=prrq8Ql81zk
</div><figcaption class="wp-element-caption">Acid rain and a crisis solved.</figcaption></figure>



<h2 class="wp-block-heading" id="h-why-don-t-we-ever-hear-about-acid-rain-anymore-the-environmental-crisis-that-was-solved">Why don't we ever hear about "acid rain" anymore? The environmental crisis that was solved</h2>



Remember the 1980s when acid rain dominated headlines? Dire warnings about rain eating buildings, killing fish, and destroying forests filled every news cycle. Then, almost like magic, acid rain vanished from public discourse. What happened? Did we actually solve one of the late 20th century's most pressing environmental challenges?



The answer might surprise you. Unlike many environmental issues that drag on indefinitely, acid rain represents one of modern history's most successful ecological recovery stories. It's a tale of science, politics, and technology working together to tackle what seemed impossible.



<h2 class="wp-block-heading">What was acid rain?</h2>



Acid rain isn't regular rain having a bad day – it's precipitation that became significantly more acidic due to air pollution. When power plants, factories, and vehicles burn fossil fuels, they release sulfur dioxide (SO2) and nitrogen oxides (NOx) into the atmosphere.



<h2 class="wp-block-heading">The science behind it</h2>



Think of acid rain as nature's chemistry experiment gone wrong. These compounds react with water, oxygen, and other chemicals to form sulfuric and nitric acids. When mixed with water vapor in clouds, they create precipitation with dangerously low pH levels.



While clean rain has a pH of about 5.6, acid rain could drop as low as 4.2 to 4.4 – roughly as acidic as tomato juice or coffee. According to US Geological Survey documentation, Scottish chemist Angus Smith first coined "acid rain" in 1872, but it didn't become a household phrase until the 1960s and 1970s when Swedish scientist Svante Odén documented its devastating effects on Scandinavian lakes and European forests.



<h2 class="wp-block-heading">The crisis at its peak</h2>



During the height of public concern, environmental damage was both widespread and visible. This wasn't some abstract future threat – people could see destruction happening in real-time.



<h2 class="wp-block-heading">Environmental devastation</h2>



The most dramatic impacts were impossible to ignore. Research documented by the Adirondack Lakes Survey Corporation and the New York State Department of Environmental Conservation shows that in the Adirondack Mountains, more than 200 lakes became so acidic they couldn't support fish life. The Adirondack Council reports that 409 lakes once supported brook trout, but many lost their fish populations due to acid rain.



By 1976, when scientists cataloged all acidified lakes in the Adirondack Park, researchers found that half of the lakes over 2,000 feet above sea level had no fish, according to studies published in environmental journals. The acidification process worked like a slow-motion disaster. As acid rain fell into watersheds, it gradually lowered pH levels. Fish couldn't survive in acidic water, and their food sources died off too.



Trees at high elevations showed stress directly linked to acid rain. It weakened them by leaching nutrients and making them susceptible to disease. Historical records show Germany's Black Forest saw nearly half its trees damaged by the mid-1980s.



<h2 class="wp-block-heading">Economic impact</h2>



Acid rain wasn't just environmental – it was expensive. Acidic precipitation corroded infrastructure, buildings, and monuments. Historic stone structures deteriorated at accelerated rates. Tourism suffered as lakes became fishless and forests declined. EPA economic analyses from the period documented repair costs mounting into billions annually.



<h2 class="wp-block-heading">The solution: government action and technology</h2>



Transformation from crisis to success required unprecedented cooperation between governments, industries, and environmental groups.



<h2 class="wp-block-heading">The Clean Air Act of 1990</h2>



The turning point came with the Clean Air Act Amendments of 1990, signed by President George H.W. Bush. This represented a fundamentally new approach to environmental regulation, as documented in EPA historical records.



<h2 class="wp-block-heading">Cap-and-trade success</h2>



Instead of mandating specific technologies, the 1990 amendments introduced something revolutionary: a cap-and-trade system for sulfur dioxide emissions. EPA program documentation shows this market-based approach set overall limits but allowed companies to trade emission allowances.



The genius was harnessing market forces to find cost-effective pollution reduction. Companies reducing emissions cheaply could sell excess allowances to those facing higher costs. Research published in environmental economics journals and EPA progress reports shows this resulted in dramatic SO2 reduction at a fraction of projected costs.



<h2 class="wp-block-heading">Technology advances</h2>



Policy provided the framework, but technology made reductions possible. Studies in atmospheric science journals document the widespread adoption of flue gas desulfurization systems ("scrubbers") that removed sulfur dioxide before it reached the atmosphere. By the 2000s, new installations could remove over 95% of SO2 emissions, according to EPA technical reports.



The push coincided with cleaner energy development. Natural gas produces fewer sulfur compounds than coal. Wind and solar, emerging in the 1990s, captured growing market share, reducing reliance on high-sulfur coal.



<h2 class="wp-block-heading" id="h-why-we-don-t-hear-about-it-today">Why we don't hear about it today</h2>



Why did acid rain disappear from headlines? Simple: the problem was largely solved.



<h2 class="wp-block-heading">Success doesn't make news</h2>



There's an old journalism saying: "If it bleeds, it leads." Environmental success stories don't generate urgency like crisis reporting. Media attention shifted to other challenges: climate change, plastic pollution, and biodiversity loss. There's only so much environmental anxiety the public can absorb, and newer concerns replaced acid rain.



<h2 class="wp-block-heading">Mission accomplished</h2>



The primary reason is beautifully simple: interventions worked. EPA monitoring data shows sulfur dioxide emissions dropped over 90% since 1990. Academic research published in environmental science journals confirms pH levels in formerly affected areas returned closer to normal. This represents one of history's most dramatic environmental recoveries. Studies by the Adirondack Lakes Survey Corporation show fishless lakes now support healthy populations. Forests recovered, and building damage slowed dramatically.



<h2 class="wp-block-heading" id="h-is-it-really-gone">Is it really gone?</h2>



The crisis is largely resolved, but monitoring data shows the problem isn't completely eliminated – it's managed to acceptable levels. Some areas still experience occasional events during high pollution periods. International environmental research indicates that rapidly industrializing Asian countries face similar problems to what we experienced decades ago, though they're implementing successful strategies.



EPA research shows nitrogen oxide emissions proved more challenging than sulfur dioxide, coming from vehicles and mobile sources. Climate science studies suggest changing weather patterns add complexity to how acid rain forms and falls.



<h2 class="wp-block-heading">What this teaches us</h2>



The acid rain experience proves that seemingly intractable environmental problems can be solved with scientific understanding, political will, and technological innovation. Environmental monitoring data shows recovery speed was remarkable – within a decade, measurable improvements appeared in air quality and ecosystem health.



Success came from bipartisan support across party lines. Policy analysis studies show the market-based approach appealed to those preferring economic incentives while achieving environmental goals. This support created lasting policy surviving political changes.



<h2 class="wp-block-heading">Conclusion</h2>



Acid rain's disappearance from public consciousness represents environmental science's greatest success stories. Through effective regulation, technological innovation, and international cooperation, we transformed an overwhelming crisis into a manageable challenge.



Today's silence isn't because we forgot – it's because we solved it. The 1990 Clean Air Act, combined with technology and energy market changes, reduced acid rain emissions over 90%, according to comprehensive EPA data analysis.



This success offers hope for current challenges. It proves complex problems can be solved when science, policy, and technology work together. As we face climate change and plastic pollution, acid rain reminds us that dramatic positive change is possible.



Next time someone asks whether environmental regulations work, remember acid rain. It's proof that sometimes, we get it right.



<hr class="wp-block-separator has-alpha-channel-opacity"/>



Sources: This article draws from EPA official documentation and progress reports, peer-reviewed research published in environmental and atmospheric science journals, historical data from the Adirondack Lakes Survey Corporation, New York State Department of Environmental Conservation records, US Geological Survey publications, policy analysis studies, and environmental monitoring data collected over three decades.



<h2 class="wp-block-heading">Frequently Asked Questions</h2>



1. Is acid rain completely gone? No, but EPA monitoring shows it's reduced to manageable levels. US sulfur dioxide emissions dropped over 90% since 1990, making acid rain much less severe than the 1980s crisis.



2. How long did solving take? Environmental monitoring data shows significant improvements began within 5-10 years of 1990s emission controls. Full ecosystem recovery took longer – some areas need 20-30 years for complete recovery.



3. What made the solution successful? Clear scientific understanding, visible damage motivating action, bipartisan support, available technology, and innovative market-based policies like cap-and-trade.



4. Do other countries have acid rain problems? Yes, particularly rapidly industrializing Asian countries. However, international environmental research shows many implement similar successful control strategies.



5. Could acid rain return? Potentially, if regulations weaken or we return to high-sulfur coal without controls, though effects would take years to become severe according to environmental projections.



6. Can you recommend any teaching tools on the subject of "acid rain"? The United States Environmental Protection Agency produced a wonderful teacher's guide for ages 14 and under that you can find on the EPA website here: <a href="https://www.epa.gov/sites/default/files/2017-03/documents/teachersguide.pdf" target="_blank" rel="noreferrer noopener">https://www.epa.gov/sites/default/files/2017-03/documents/teachersguide.pdf</a>



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The environmental problem we actually solved

https://www.youtube.com/watch?v=prrq8Ql81zk Acid rain and a crisis solved. Why don't we...

Green,Ecoduct,Over,An,Empty,Highway,During,Sunset.

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A new long-term study in Monkton, Vermont, reveals that wildlife tunnels significantly reduce amphibian road mortality during seasonal migrations. 



Frogs and salamanders often cross roads to reach breeding ponds each spring, but many are killed by vehicles. 



Researchers from the <a href="https://www.uvm.edu/" target="_blank" rel="noreferrer noopener">University of Vermont</a>, in collaboration with local citizens and the Vermont Agency of Natural Resources, installed two underpass tunnels in 2015. 



Over a 12-year monitoring period, they observed an 80.2% reduction in amphibian deaths, and up to 94% for non-climbing species like salamanders. 



The study used a before-after-control-impact design and documented more than 5,200 amphibians, highlighting the tunnels’ effectiveness even in nearby buffer zones.



Funded at $342,397 - far cheaper than wildlife crossings for large mammals - the project showcased the power of community-led conservation.



Local groups initiated the effort after observing mass amphibian deaths. Wildlife cameras later captured over 2,200 amphibians using a tunnel in just one spring, along with other species like raccoons and bobcats, indicating wider ecosystem benefits.



This marks the first peer-reviewed, long-term data set in the northeastern U.S. confirming amphibian-specific underpasses work. 



The study urges transportation departments to incorporate these designs into road planning and highlights how community action, thoughtful infrastructure, and persistence can make a real difference for biodiversity.



The full study was published in the <a href="https://linkinghub.elsevier.com/retrieve/pii/S1617138125000780" target="_blank" rel="noreferrer noopener">Journal for Nature Conservation</a>.



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Wildlife tunnels save millions of amphibians

https://youtu.be/XYgiPzmNBTU?si=eFYY7gPHU1JznLvU A new long-term study in Monkton, Vermont, reveals that...

Scientists are transforming chocolate into a functional food by infusing it with probiotics and prebiotics, aiming to create a treat that satisfies cravings while supporting gut health. 



The challenge lies in maintaining chocolate's beloved texture and flavor while adding health benefits.



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Probiotics - beneficial microbes that balance gut bacteria and aid digestion - are typically fragile and can be destroyed by stomach acid or processing. 



Prebiotics act as food for these microbes, helping them thrive. Together, they form "synbiotics," a powerful health combination.



Researchers Smriti Gaur and Shubhi Singh from India's Jaypee Institute of Information Technology took an innovative approach, using natural prebiotics like corn and honey instead of complex processing methods. 



They created five chocolate varieties: a control and four synbiotic versions containing different combinations of prebiotics, probiotics (Lactobacillus strains), and flavor enhancers (cinnamon or orange).



Laboratory simulations of human digestion showed the probiotics remained viable for over five hours, suggesting they could survive long enough to benefit gut health.



Taste tests were positive, with researchers particularly enjoying the orange-flavored variety, describing it as having "vibrant citrus notes" complementing the "rich cocoa" with a "luxurious" texture.



This research represents just the beginning. With further refinement of strains, textures, and flavors, chocolate could evolve beyond mere indulgence to become a functional food that nourishes while it delights.



The study is published in the journal <a href="https://pubs.acs.org/doi/10.1021/acsfoodscitech.4c00741" target="_blank" rel="noreferrer noopener">ACS Food Science &amp; Technology</a>.

Is chocolate the next nutritional powerhouse?

Scientists are transforming chocolate into a functional food by infusing...

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Today’s Video of the Day from <a href="https://www.igb.illinois.edu/">Carl R. Woese Institute for Genomic Biology</a> reveals how scientists can modify common crops like soybean, rice, and wheat to protect them from heat stress.



“We need to double crop production by 2050 to feed a growing global population, and not only are we not on track to do that, but climate change is further complicating things,” said Amanda Cavanagh, a lecturer at the University of Essex. 



The study is part of Realizing Increased Photosynthetic Efficiency (RIPE), an international research project that aims to develop food crops that turn the sun’s energy into food more efficiently.



“Using an engineering approach we designed multiple alternative metabolic pathways to photorespiration. Testing them in the field showed increases in productivity which led Amanda to significantly move the project forward by showing our engineered plants can withstand pretty extreme temperature stress,” said study co-author and RIPE researcher Paul South.&nbsp;



“As the climate changes and temperature stresses increase the pressure on our global food supply, farmers will need every tool available including engineering approaches like the synthetic biology used here to maintain safe and productive harvests.”



The experts tested plants modified to have more efficient photorespiration to see if they were better adapted to warmer temperatures.&nbsp;



The team found that the engineered plants produced 26 percent more biomass than the wild-type plants exposed to the same temperatures, and had 15 percent less yield loss under the higher temperatures.



Video Credit: Amanda Nguyen/University of Illinois



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



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Designing crops that can beat the heat

[sendtonews key="QGPzYnXEtN-1712599-12187" type="single"] Today’s Video of the Day from Carl...

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Today's Video of the Day from <a href="https://www.nasa.gov/goddard">NASA Goddard</a> describes the first comprehensive estimate of carbon density in the Saharan, Sahel, and Sudanian zones of Africa. In an effort to measure the amount of carbon stored across these drylands, a team of scientists used high-resolution satellite images and artificial intelligence to map nearly 10 billion individual trees. 



"The high spatial resolution (50 cm) combined with AI and field measurements used in this study is key to improving tree inventories in drylands," said Pierre Hiernaux, a French researcher working for NASA. "The ever-increasing availability of very high-resolution satellite imagery will make it possible to assess carbon pools and their dynamics at the individual tree level on a global scale."



"This study is exceptional because it is pioneering a type of approach that will revolutionize the monitoring of trees and forests on a global scale: in the short term, it will be possible to map the world's trees from the centre of the Amazon to our schoolyards," said <a href="https://www.inrae.fr/en">INRAE</a> researcher Jean-Pierre Wigneron.



"Many fields of application will become much more efficient and accurate, such as tracking carbon stocks, biodiversity, monitoring logging and protection against illegal forest degradation, in near real time.”



Video Credit: NASA Goddard&nbsp;



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



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Remote sensing will revolutionize the way we monitor trees

[sendtonews key="EjmSP20gQK-2593093-12187" type="single"] Today's Video of the Day from NASA...

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Lesotho: Africa's "Kingdom in the Sky" Today’s Video of the Day from the <a href="https://www.esa.int/">European Space Agency</a> features northwest Lesotho in South Africa.



According to ESA, Lesotho is the only nation in the world that lies completely above 1,000 m in elevation. The country is famous for its tall mountains and narrow valleys, and is known as Africa's "Kingdom in the Sky."



Out of a population of around two million people, about 80 percent live in rural areas. More than 75 percent of these people are engaged in <a href="https://www.earth.com/news/climate-change-will-have-a-global-impact-on-agriculture/">agriculture</a>, including rainfed cereal production and animal grazing.&nbsp;



ESA reports that the country’s agricultural system faces a growing number of issues, with climate-related vulnerabilities such as drought, floods and extreme temperatures occurring more frequently. 



Diamonds are amongst the minerals found in the mountains. Indeed, Lesotho can truly be called the Kingdom in the Sky. Beautiful, culturally rich, safe, affordable, and easily accessible from Durban and Johannesburg, mountainous Lesotho is a vastly underrated travel destination. the Kingdom of Lesotho (Sotho: 'Muso oa Lesotho) is an enclaved country in southern Africa. It is just over 30,000 km2 (11,583 sq mi) in size and has a population of around 2 million.



Video Credit: ESA&nbsp;&nbsp;



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Staff Writer 



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Lesotho: Africa's "Kingdom in the Sky"

[sendtonews key="uV9Lh2fQbV-1760058-12187" type="single"] Lesotho: Africa's "Kingdom in the Sky" Today’s...

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Today's Video of the Day from <a href="https://www.nasa.gov/goddard">NASA Goddard</a> features a visual dataset of.methane emissions from wetlands across the globe. Atmospheric methane levels have reached record highs in recent years, and wetlands are a major source of these emissions.&nbsp;



"Methane is an important greenhouse gas that contributes substantially to global warming. On a molecule by molecule basis, methane is much more efficient at trapping heat than carbon dioxide, the main driver of warming," says NASA.



"Though human activities, including agriculture, oil and natural gas production and use, and waste disposal, collectively contribute the majority of methane to the atmosphere, about a third of total methane emissions comes from wetlands."&nbsp;



According to NASA, understanding methane emissions from wetlands and other natural sources is critically important for scientists and policymakers who are working to combat climate change by reducing emissions from human activities.



Video Credit: NASA Goddard



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



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Wetlands are a major source of methane emissions

[sendtonews key="f8fukm28Vz-2491833-12187" type="single"] Today's Video of the Day from NASA...

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Today’s Video of the Day from <a href="https://earthobservatory.nasa.gov/">NASA Earth Observatory</a> reveals the evolution of the Columbia Glacier in southeastern Alaska. Columbia is among the fastest shrinking glaciers in the world, and the video documents its rapid retreat over the years.&nbsp;



Columbia Glacier is a large, multi-branched calving glacier that flows out of the Chugach Mountains to the Prince William Sound.&nbsp;



According to USGS, Columbia had a long history of stability prior to 1980, with a length 41 miles, and small, short-lived advances or retreats.



In the years since 1980, however, satellite images have captured Columbia’s alarming retreat. By using false-color images, scientists can distinguish between snow and ice, open water, vegetation, and rocky debris on the glacier’s surface.



The series of false-color images featured in today's video were acquired over the span of 35 years. You can see that by 2021, the glacier’s main branch had retreated about 15 miles from its initial position.



The Columbia Glacier has also lost more than 50 percent of its volume, mostly due to calving. <a href="https://www.earth.com/video/nasa-reveals-3d-visual-of-an-atmospheric-river/">NASA</a> reports that while climate change likely started the retreat, mechanical processes kept the disintegration going.



The NASA images are provided by Jesse Allen, Robert Simmon, Joshua Stevens, and Lauren Dauphin using data from Landsat satellites, from the U.S. Geological Survey, and data from MODIS on NASA’s Terra satellite. The structure of Columbia’s moraine played a large role in the stability of the glacier before 1980. 



Like other tidewater glaciers, the Columbia built up a moraine over time, and the mixture of ice and rock functioned like a dam keeping out the sea. It was supported on one end by the shoreline and by the underwater terminal moraine at the other.



Video Credit: NASA Earth Observatory/&nbsp; NASA’s Scientific Visualization Studio



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



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The rapid retreat of the Columbia Glacier

[sendtonews key="0879czfG3k-1785905-12187" type="single"] Today’s Video of the Day from NASA...

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Today's Video of the Day from <a href="https://www.nasa.gov/goddard">NASA Goddard</a> describes how record-breaking heat expressed itself around the world in 2022.



Scientists have determined that 2022 was the 5th warmest year since 1880. Furthermore, the last nine consecutive years have been the warmest on record.



From devastating floods and wildfires to natural disasters like Hurricane Ian, 2022 showed us yet again how a warming climate affects people across the globe.&nbsp;



"As we look back at 20:22 and years past, we see that each year we better understand the challenges we face and how important it is to meet them," says NASA.



Video/ Image Credit: NASA Goddard



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



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2022 illustrated the consequences of a warming climate

[sendtonews key="3UUsNkFOuS-2487333-12187" type="single"] Today's Video of the Day from NASA...

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Satellites reveal how Earth's systems are interconnected Today’s Video of the Day from <a href="https://www.nasa.gov/goddard">NASA Goddard</a> describes Earth’s interconnected systems, and how this network is affected by rising temperatures.&nbsp;



During 2020, average global temperatures matched the hottest year on record. The hurricane season was also record-breaking, with many of the storms intensifying at extraordinary speeds. Hot water in the ocean is fuel for hurricanes. The satellite data shows that it's all one interconnected system showing how Satellites reveal how Earth's systems are interconnected.



According to NASA, dust swept up from Northern Africa plays a major role in the formation of hurricanes, and is also a key source of fertilization in the Amazon rainforest. As a result of<a href="https://www.earth.com/news/seagrass-wasting-disease-is-fueled-by-climate-change/"> climate</a> change, dust plumes are expected to decline, which will have an effect on vegetation far away.&nbsp;



Images from Earth-observing satellites show how the world’s plant life is affected by natural disasters, fires, and deforestation. Satellites also reveal how widespread changes in vegetation impact waterways,&nbsp; the climate, air quality. Satellites communicate by using radio waves to send signals to the antennas on the Earth. "Earth From Space" is a groundbreaking two-hour special that reveals a spectacular new space-based vision of our planet. 



Video Credit: NASA Goddard&nbsp;



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



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Satellites reveal how Earth's systems are interconnected

[sendtonews key="JbW4VsY53O-1632195-12187" type="single"] Satellites reveal how Earth's systems are interconnected...

Today’s Video of the Day from the <a href="https://welcome.miami.edu/">University of Miami</a> Rosenstiel School of Marine and Atmospheric Science explores how changes in water temperatures have affected tiger shark habitats and movements in the North Atlantic Ocean. The study reveals that rising temperatures have caused the sharks to shift toward the poles over the past 40 years.



“Tiger shark annual migrations have expanded poleward, paralleling rising water temperatures,” explained study lead author Neil Hammerschlag. “These results have consequences for tiger shark conservation, since shifts in their movements outside of marine protected areas may leave them more vulnerable to commercial fishing.”



The researchers analyzed nine years of tracking data from satellite-tagged tiger sharks, combined with four decades of conventional tag and recapture data provided by National Oceanic and Atmospheric Administration (NOAA) Cooperative Shark Tagging Program.



The experts found that during the last decade of record heat, for every one-degree Celsius increase in water temperatures, tiger sharks migrated further poleward by over 400 kilometers. They also migrated two weeks earlier than usual to waters off the northeastern coast of the United States.



“Given their role as apex predators, these changes to tiger shark movements may alter predator-prey interactions, leading to ecological imbalances, and more frequent encounters with humans,” concluded Professor Hammerschlag.



Video Credit: University of Miami Rosenstiel School of Marine and Atmospheric Science



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



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Tiger sharks are shifting poleward as temperatures rise

Today’s Video of the Day from the University of Miami...

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Today’s Video of the Day from the <a href="https://www.esa.int/">European Space Agency</a> is focused on the melt ponds that emerge during the spring and summer on the Greenland Ice Sheet, which is the largest ice mass in the northern hemisphere.



"Melt ponds are vast pools of open water that form on both sea ice and ice sheets and are visible as turquoise-blue pools of water in this Copernicus Sentinel-2 image," says ESA.



"When snow and ice melts atop glaciers, water flows in channels and streams and collects in depressions on the surface. These melt ponds can speed up the melting of the surrounding ice since they greatly reduce the ice’s ability to reflect sunlight."



"This can create a positive feedback where an increasing number of melt ponds absorb more heat which causes ice cover to melt even faster."



According to ESA, Greenland has been hit with a late-season heatwave that began in early September. This caused the type of melt event that usually occurs in the middle of summer.



"In a recent paper published in Nature Climate Change, scientists found that major sea-level rise from the melting of the Greenland ice cap is now ‘inevitable’ even if the burning of fossil fuels were to halt overnight," says ESA. "Using satellite observations of Greenland ice loss and ice cap from 2000 to 2019, the team found the losses will lead to a minimum rise of 27 cm regardless of climate change."



Video Credit: ESA&nbsp;



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



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Melt ponds on the Greenland Ice Sheet

[sendtonews key="qARzJPSabQ-2270617-12187" type="single"] Today’s Video of the Day from the...

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Today’s Video of the Day from the <a href="https://www.esa.int/">European Space Agency</a> describes how Earth is unique in our solar system for its ability to sustain liquid water on its surface. But now, the water cycle is shifting as the climate warms, and scientists must find ways to predict how these changes will affect water availability.



Overall, 96 percent of Earth's water is saltwater, and nearly all of freshwater is found in ice and groundwater. These sources of water are linked as it passes through solid, liquid and gas phases.



In a warmer climate, the water cycle will be transformed. It will be easier for water to evaporate and form clouds, and storms will become more frequent and intense. Some regions will get too much water, while others will be left without enough water. In addition, soil moisture will be lost - which threatens food security.



Scientists are using satellite data from over the last 40 years to track changes that are happening in the water cycle. This will ultimately help us prepare for extreme events and better manage our water resources, according to ESA.



Video Credit: ESA



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



Check us out on <a href="https://www.earth.com/earthsnap/">EarthSnap</a>, a free app brought to you by Eric Ralls and Earth.com.

Tracking changes in Earth's water cycle

[sendtonews key="fxH3eJHEkQ-2010196-12187" type="single"] Today’s Video of the Day from the...

Saturn,-,High,Resolution,3d,Images,Presents,Planets,Of,The

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Today's Video of the Day from <a href="https://www.nasa.gov/goddard">NASA Goddard Space Flight Center</a> features images of Saturn from NASA’s Hubble Space Telescope. The photographs capture the start of the mysterious "spoke season" on Saturn - when unexplained features appear on its rings. 



According to NASA, both the cause of the spokes and their seasonal variability have yet to be fully explained by planetary scientists.



"Like Earth, Saturn is tilted on its axis and therefore has four seasons, though because of Saturn's much larger orbit, each season lasts approximately seven Earth years. Equinox occurs when the rings are tilted edge-on to the Sun," explains NASA.



"The spokes disappear when it is near summer or winter solstice on Saturn. (When the Sun appears to reach either its highest or lowest latitude in the northern or southern hemisphere of a planet.) As the autumnal equinox of Saturn's northern hemisphere on May 6, 2025, draws near, the spokes are expected to become increasingly prominent and observable."



Experts believe that the spokes may be a product of the planet's variable magnetic field. When magnetic fields interact with solar wind, an electrically charged environment is created. This phenomenon is visible on Earth as the northern lights.&nbsp;



"Scientists think that the smallest, dust-sized icy ring particles can become charged as well, which temporarily levitates those particles above the rest of the larger icy particles and boulders in the rings," says NASA.



The spokes were first observed in the early 1980s by NASA's Voyager mission. Depending on the angle of the rings, the spokes can appear dark or light.



"Thanks to Hubble's OPAL program, which is building an archive of data on the outer solar system planets, we will have longer dedicated time to study Saturn’s spokes this season than ever before," said NASA senior planetary scientist Amy Simon, head of the Hubble Outer Planet Atmospheres Legacy (OPAL) program.



"Despite years of excellent observations by the Cassini mission, the precise beginning and duration of the spoke season is still unpredictable, rather like predicting the first storm during hurricane season."



Video Credit: NASA Goddard&nbsp;



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



Check us out on <a href="https://www.earth.com/earthsnap/">EarthSnap</a>, a free app brought to you by Eric Ralls and Earth.com.

Mysterious "spoke season" captured on Saturn

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Today’s Video of the Day from <a href="http://www.ntu.edu.sg/">NTU Singapore</a> reveals that some plants can remove toxic heavy metals from soil.&nbsp;



The researchers analyzed samples of various tropical plant species to test for levels of heavy metals and metalloids. The study showed that there are existing plants with high levels of these contaminants, which means that these species are great candidates for drawing pollutants out of the soil.&nbsp;



Among the plants examined in the study, 12 species had accumulated several types of heavy metals and metalloids. These plants are widely available, including species that are native to Singapore.



“In a small nation like Singapore, land may be repurposed to support new development plans, so it is important that we have a green and sustainable way to remediate land that is contaminated," said Professor Lam Yeng Ming.



"We set out to uncover how to better make use of tropical plants to do phytoremediation and through advanced characterization techniques, we showed how some of these tropical plant species can be an environmentally friendly and literally a 'green' way to remove contaminants in soil."&nbsp;



"Phytoremediation also has benefits of cost effectiveness, simplicity of management, aesthetic advantages, and long-term applicability and sustainability. The strategy prevents erosion and metal leaching by stabilizing or accumulating heavy metals, so that helps reduce the risk of contaminant spread.”



Video Credit: NTU Singapore



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



Check us out on <a href="https://www.earth.com/earthsnap/">EarthSnap</a>, a free app brought to you by Eric Ralls and Earth.com.

Plants help remove heavy metals from contaminated soil

[sendtonews key="6SdlLLbt0t-1988946-12187" type="single"] Today’s Video of the Day from NTU...

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Today’s Video of the Day from the <a href="https://www.acs.org/">American Chemical Society</a> describes why herbicides are not as effective in killing weeds anymore. In the 20th century, chemical companies developed thousands of herbicides. The most commonly used herbicide was glyphosate, which was introduced in 1974.



Over the past few decades, dozens of species of weeds have evolved resistance to glyphosate. Depending on the site of action, the part of the plant that an herbicide interacts with, weeds may even be resistant to herbicides that have not been developed yet.&nbsp;



With increasing resistance to glyphosate and other herbicides, weeds are - once again - becoming a major concern for farmers.&nbsp;



Video Credit: American Chemical Society&nbsp;



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



Check us out on <a href="https://www.earth.com/earthsnap/">EarthSnap</a>, a free app brought to you by Eric Ralls and Earth.com.

Weeds are becoming increasingly resistant to herbicides

[sendtonews key="gRpsplpwpe-2251464-12187" type="single"] Today’s Video of the Day from the...

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Today’s Video of the Day from the <a href="https://www.jpl.nasa.gov/">NASA Jet Propulsion Laboratory</a> (JPL) describes a dust storm on Mars that was nearly twice the size of the United States. As the storm covered the southern hemisphere of the planet, some of NASA’s explorers had to delay their normal activities.



NASA’s Insight lander put itself in a "safe mode" for 11 days to conserve battery power because solar power was disrupted by the dust. The Ingenuity Mars Helicopter postponed flights until conditions improved.



"A fleet of NASA orbiters monitor Martian dust storms like this one and serve as lifelines to Earth by relaying data from the rovers and lander on the ground back to the team. This includes the Mars Reconnaissance Orbiter, MAVEN, and Odyssey," reports JPL.



"Dust storms like this recent one start close to the ground and are spread by wind as they rise – warming the cold Martian atmosphere."



The images in the video were captured by NASA’s Curiosity as the dust rolled in. A fleet of orbiters monitored the dust storm from above, relaying data from Mars’ explorers back to scientists on Earth.



Video &amp; Image Credit: NASA/JPL-Caltech/ASU/MSSS



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By <a href="mailto:csexton@earth.com">Chrissy Sexton</a>, <a href="https://www.earth.com/staff/">Earth.com</a> Editor



Check us out on <a href="https://www.earth.com/earthsnap/">EarthSnap</a>, a free app brought to you by Eric Ralls and Earth.com.

NASA monitors giant dust storms on Mars

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