The Arctic, known for its icy landscapes and frozen permafrost, is rapidly transforming due to the intensifying effects of climate change. As temperatures rise, a silent but potent threat emerges: methane emissions. Unlike carbon dioxide, methane is not as widely discussed, yet its impact on global warming is profound. 



A new study published in the journal Nature highlights the growing concern over methane emissions in the <a href="https://www.earth.com/news/arctic-climate-will-permanently-change-by-2050-scientists-warn/" target="_blank" rel="noreferrer noopener">Arctic</a> and their role in creating a feedback loop that could accelerate climate change.



<h2 class="wp-block-heading" id="h-why-methane-traps-more-heat">Why methane traps more heat </h2>



Methane isn’t as abundant as carbon dioxide, but it’s far more potent. Over a century, it traps 30 times more heat. 



Xin (Lindsay) Lan, a climate scientist at <a href="https://www.colorado.edu" target="_blank" rel="noreferrer noopener">CU Boulder</a>’s Cooperative Institute for Research in Environmental Sciences (CIRES), sees the urgency.



“Methane is a very potent greenhouse gas that we need to address urgently,” Lan said. “Our study suggests that a significant portion of the recent rise in atmospheric methane originates from natural <a href="https://www.earth.com/news/arctic-warming-may-fuel-the-spread-of-diseases-by-unleashing-frozen-viruses/" target="_blank" rel="noreferrer noopener">sources</a> driven by climate change. Our emission reduction efforts need to be more aggressive.”



<h2 class="wp-block-heading" id="h-arctic-methane-levels-climb-steadily">Arctic methane levels climb steadily</h2>



For years, Lan has tracked methane levels at NOAA’s <a href="https://gml.noaa.gov" target="_blank" rel="noreferrer noopener">Global Monitoring Laboratory</a> in Boulder. Methane emissions have steadily climbed since 2007. 



Scientists had pointed fingers at fossil fuels, responsible for 30% of emissions. Yet, Lan’s research points elsewhere - to tiny, ancient microbes thriving in new, warmer habitats.



Archaea - microbes that have lived for millennia in wetlands, landfills, and the guts of livestock - produce methane. They may be small, but they’re mighty emitters. Microbial emissions now make up nearly half of all global methane output. Yet, pinpointing specific sources remains tricky.



Lan isn’t just watching long-term trends. Seasonal fluctuations in methane also reveal what’s <a href="https://www.earth.com/news/arctic-meltdown-is-accelerating-global-warming-already-changing-earth-in-unimaginable-ways/" target="_blank" rel="noreferrer noopener">changing</a> underground.



<h2 class="wp-block-heading" id="h-permafrost-fuels-methane-emissions">Permafrost fuels methane emissions</h2>



Lan’s team dove into decades of data. Methane’s seasonal amplitude - the swing from highest to lowest levels in a year - is shrinking in northern latitudes. 



Why? Wetlands in the Arctic are expanding. Thawing permafrost is unlocking ancient carbon stores, creating perfect conditions for archaea.



Computer models show the Arctic’s wetlands have grown by 25% in the warmer months, feeding the microbes with more decomposing organic matter. The result: more methane.



<h2 class="wp-block-heading" id="h-the-feedback-loop-accelerates">The feedback loop accelerates</h2>



When permafrost melts, more carbon enters the <a href="https://www.earth.com/news/drastic-warming-will-transform-the-arctic-beyond-recognition/" target="_blank" rel="noreferrer noopener">atmosphere</a>. As temperatures rise, more permafrost melts. A cycle begins. Lan’s research shows that since 2007, this loop has intensified. What was once a trickle of methane is becoming a flood.



“This study, along with a few previous studies, has provided indirect evidence on potential climate feedback on methane emissions, which would be beyond our ability to control directly,” Lan said.



In previous work, Lan's team analyzed connections between today’s methane surge and dramatic warming events that ended past ice ages.



As Arctic ice sheets melted, vast stores of methane escaped, causing rapid temperature increases. That was thousands of years ago. Now, it’s happening again - but faster.



<h2 class="wp-block-heading" id="h-underestimated-methane-removal">Underestimated methane removal</h2>



Methane doesn’t linger forever. Hydroxyl (OH) radicals act like atmospheric scrubbers, breaking down methane. Lan’s team discovered that since 1984, these radicals have increased by 10%.



Unfortunately, OH levels are hard to measure - they disappear within seconds - scientists had assumed they remained constant. But Lan’s study suggests that the atmosphere has been removing more methane than previously thought.



“Our result showed that we’ve been underestimating how much methane the atmosphere has been removing, which means that there’s actually more methane being emitted than we previously estimated,” Lan said.



<h2 class="wp-block-heading" id="h-arctic-methane-feedback-loop">Arctic methane feedback loop</h2>



If the atmosphere is cleaning itself more efficiently, then methane emissions are higher than we realized. 



That’s a big problem. Emission reduction plans rely on accurate data. If those numbers are off, efforts to control methane may miss the mark.



Lan stresses that understanding methane’s sources is critical. Microbial emissions are surging, but fossil fuels still account for a major chunk of global output. 



And the Arctic’s permafrost holds double the carbon currently in the atmosphere. If warming continues, thawing permafrost could unleash catastrophic carbon releases.



“We need to aggressively cut all greenhouse gas emissions from the sources we can control,” Lan said. “We need to address the feedback loop before reaching that tipping point.”



<h2 class="wp-block-heading" id="h-urgency-amid-uncertainty">Urgency amid uncertainty</h2>



Time is not on our side. Methane’s rise mirrors past warming events, but this time, human activities amplify the effect. 



Lan’s work highlights a critical truth: the Arctic is changing faster than expected, and methane is slipping through the cracks.



Now, the question is - how much longer before the feedback loop spirals beyond control?



The study is published in the journal <a href="https://www.nature.com/articles/s41586-025-08900-8" target="_blank" rel="noreferrer noopener">Nature</a>.



-----



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Arctic warming fuels dangerous methane feedback loop

The Arctic, known for its icy landscapes and frozen permafrost, is rapidly transforming due to the intensifying effects of climate change. As temperatures rise, a silent but potent threat emerges: methane emissions. Unlike carbon dioxide, methane is not as widely discussed, yet its impact on global warming is profound. A new study published in the journal Nature highlights the growing concern over methane emissions in the Arctic and their role in creating a feedback loop that could accelerate climate change. Why methane traps more heat Methane isn’t...

Many people are concerned about conservation of the planet’s cute and cuddlies. But in a world of global climate change, sometimes we must prioritize species survival and which species we can and should save from extinction. Dr. Alycia Stigall and her colleagues are leading the charge in studies to help us make those determinations by looking at the fossil record. She will report their findings at the Annual Meeting of the Geological Society of America on 25 September in Denver, Colorado, USA.

As a paleontologist, Stigall has looked at seven different events in deep time that experienced dramatic shifts in the biodiversity (number of species) and the size of species populations from as recent as 15,000 to 30,000 years ago (Beringia dispersals) to 485 to 460 million years ago (Great Ordovician Biodiversification Event).

So how does biodiversity generate on Earth? Stigall and her colleagues (all of whom are former students of hers) have found evidence for a cycle that explains how species diversify and disappear over time. Some animals living on a continent are generalists (able to thrive in multiple environments and/or from multiple resources). These animals spread out across the continent so that they reduce the amount of competition for resources. Over time, the continent breaks apart into numerous islands and the animals are isolated from each other. This leads to speciation (formation of new species) because the animals are all competing for limited resources and thus specialize into ecological niches in order to coexist peacefully. This speciation increases biodiversity, but if the environment changes, those specialized species are less likely to survive. So as those islands begin to form a new continent, the generalists invade the ecological niches of specialists and drive speciation, and thus biodiversity, down.

This information is critical for understanding modern conservation efforts because it tells us that specialist species are going to need a lot more help surviving global climate change than generalist species. As we undergo this changing environment, invasive species will become more of a common occurrence. Stigall explains that while this pattern keeps occurring throughout time, there are always going to be idiosyncrasies associated with the multitude of different drivers in each of those geological events. And when you start taking human interferences into account, predictive modeling becomes even more difficult.

“Places that are tropical and stable, regions that have similar climate year-round, will likely be impacted the most by invasive species,” Stigall explains. “Data sets for modern species are usually limited in terms of the number of species and years available when talking about biodiversity, so hopefully we can use the fossil record to expand our knowledge and use the past to make informed decisions about the future.”

--

<a href="http://www.geosociety.org/" target="_blank" rel="noopener">Geological Society of America</a>

Scientists are using fossils to predict future species survival

Many people are concerned about conservation of the planet’s cute...

Sea surface temperatures dipped dramatically during a period from 7 million to 5.4 million years ago, a time of massive global ecological change.

Around 7 million years ago, landscapes and ecosystems across the world began changing dramatically. Subtropical regions dried out and the Sahara Desert formed in Africa. Rain forests receded and were replaced by the vast savannas and grasslands that persist today in North and South America, Africa and Asia.

Up to now, these events have generally been explained by separate tectonic events — the uplift of mountain ranges or the alteration of ocean basins — causing discrete and local changes in climate. But in a new study, a team of researchers has shown that these environmental changes coincided with a previously undocumented period of global cooling, which was likely driven by a sharp reduction in atmospheric carbon dioxide.

The research, led by a Brown University geologist and published in Nature Geoscience, is based on a newly developed record of global sea surface temperatures spanning the past 12 million years. The record reveals a distinct period of cooler sea surface temperatures spanning 7 million to 5.4 million years ago, the end of the Miocene epoch. The global climate during the Miocene is known to have been much warmer than the present. During the cool period detected in this study, sea surface temperatures dropped to near modern levels.

“This is the first time the late Miocene has been put in a context of global sea surface temperatures, and we were surprised to see the amount of cooling we found,” said Timothy Herbert, professor in the Department of Earth, Environmental and Planetary Sciences at Brown, who led the study. “In light of this temperature change, the paleobiological observations from this period start to make a lot more sense.”

The new record of sea surface temperatures was derived from ocean sediment sampled at 17 different sites around the world. The sediment preserves the remains of a plankton species that varies cellular chemistry with temperature. By measuring amounts of those temperature-sensitive molecules, scientists can recreate temperature through time.

The late Miocene cool period was detected at every site sampled, in both hemispheres and in every ocean basin on the planet. The cooling was strongest toward the poles and more moderate toward the equator. That pattern, Herbert says, suggests a global atmospheric cause for the temperature decline. The most likely suspect is carbon dioxide (CO2).

“The hemispheric symmetry and the fact that cooling is much greater at the high latitudes — these are the fingerprints of CO2-related temperature change,” Herbert said. “We haven’t proven that it was a decline in CO2 because we’re not measuring it directly, but we’re making a circumstantial case for a reduction in CO2.”

The cooler temperatures would likely have played a role in the drying of the subtropics in the late Miocene, the researchers say. “A cooler world — particularly a cooler ocean — would have decreased moisture in the atmosphere,” Herbert said. “The hydrological cycle basically slows down with cooling.”

And if the cooling was indeed driven by a reduction in atmospheric CO2, it could explain a critical shift in global vegetation that occurred during the late Miocene: the transition from forests to grassland and savanna in the subtropical regions of North and South America, Asia and Africa. These ecosystems are still present today. In Africa, these are the habitats associated with the evolution of our early human ancestors.

Many of the grassy plant species that began thriving during this period are “C4” plants. These species use a slightly different photosynthetic pathway than trees and other plants. The C4 pathway is more efficient in low CO2 environments. “It could be that that if CO2 declined, these C4 species were favored,” Herbert said. “So we can associate that shift in vegetation with the same thing that we suspect was driving the late Miocene cooling.”

It isn’t clear at this point what might have driven a reduction in CO2 during this period, Herbert says. It could be that there were large-scale geological changes occurring at this time that affected the carbon cycle. Herbert’s lab is looking into that possibility now.

But what is clear is that there was a significant global shift in global temperatures during the late Miocene.

“The prevailing view was that this wasn’t a particularly exciting time in terms of global climate,” Herbert said. “It turns out to be more interesting than people thought.”

---

<a href="http://www.brown.edu" target="_blank" rel="noopener">Brown University</a>

Study: Global cooling led to modern ecosystems

Sea surface temperatures dipped dramatically during a period from 7...

A recent spate of whale entanglements off of New England could help shape future regulations to preserve the endangered animals, federal authorities said Tuesday.
A North Atlantic right whale was found dead about 12 miles off the Maine coast over the weekend, entangled in fishing gear. Two other right whales were also found entangled recently. One of them was reported alive, and researchers plan to reassess its condition.
The National Oceanic and Atmospheric Administration said the 45-ton animal's death near Maine was still being investigated, including whether the gear can be traced back to its owner.
The agency is using gear recovered from the entanglements to see if the fishermen who owned them were in compliance with fishing regulations, NOAA Marine Mammal and Sea Turtle Program Coordinator David Gouveia said. Gouveia said the investigation could also inform future regulations.
"We're on par for the course with the averages for the year for entanglements," he said. "Overall, if you look at entanglements of all large whale species, we're a little bit above our average."
Entanglement is a key cause of death among North Atlantic right whales, which are among the rarest whales.
The population of the whales has crept up from about 300 in 1992 to about 500 in 2010, but a recent study in the journal Frontiers in Marine Science stated that the number of baby right whales born every year has steeply declined since. The study's author, Scott Kraus, said the whales' population suffers even when the animals survive entanglements in fishing gear because of negative effects to reproduction.
It's too early to say what form any new regulations could possibly look like. Patrice McCarron, executive director of the Maine Lobstermen's Association, said it's unlikely that the rope that entangled the Maine whale was from a Maine lobsterman because of how thick it was.
"It's not the kind of gear that we typically see in Maine," she said.
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Call to action as whale entanglements increase

A recent spate of whale entanglements off of New England...

A crowd of several hundred people gathered in the growing darkness outside Chapman Elementary School in Portland, Oregon, before the first Vaux's Swift darted into view high above.
Minutes later, thousands of the tiny birds were swooping and swirling like a cloud of pulsating black ink as they circled a tall brick chimney silhouetted by the fading light.
The humans below, watching from a patchwork of blankets and empty picnic baskets, cheered as the flock poured into the chimney all at once, like water spiraling down a drain.
The swifts' noisy migratory stopover each fall has made this chimney famous with bird lovers as far away as Europe and is a quirky Portland tradition so embraced by locals that the school keeps the diminutive Vaux's Swift as its mascot.
But in recent years, fewer of the beloved birds have shown up. The migratory birds were already struggling because of the destruction of old-growth forests and now some scientists believe they are being further impacted by the destruction of old brick chimneys along their migratory path.
The birds can fly for about 100 miles at a time between stops as they travel from Canada to Mexico and back each year and roost in large numbers in tight, enclosed spaces because their body temperature drops at night.
But the decades-old smoke stacks they've adopted are getting torn down and capped off along the West Coast because of redevelopment, seismic concerns and an urban annoyance with swift poop and noisy flocks. When a chimney that's been a major roosting site disappears, no one is sure exactly where they go.
After adapting to live alongside humans in an urban landscape, the graceful birds are being evicted once again. Now, a movement has taken flight to build concrete towers to replace the chimneys that are lost.
"It's obvious, it's going (to) be real easy for a time to come when the swifts cannot find a nice, brick roost site," said Larry Schwitters, an expert on the West Coast swift species who lives outside Seattle. "The problem at this point is us. We're the ones causing their decline."
The birds are 4 inches long and grayish-brown with a jaunty black eyepatch that makes them look like tiny, winged Zorros. Their wings make elegant crescents in the air.
The West Coast cousins to the more well-known East Coast chimney swifts can only perch vertically and must cling to hollowed out trees or, in urban settings, the insides of old chimneys. Only brick smoke stacks erected before 1940 will work because newer chimneys have a liner that makes it impossible for them to gain a foothold.
The official estimate of the Vaux's Swift population in North America is 390,000, but Schwitters believes there may be far fewer based on his work to document all the roosting spots on the West Coast and tally all-time high roosting numbers at each one.
The birds aren't listed as a threatened or endangered species, but their population has been falling 2 to 4 percent a year and has declined about 50 percent since 1970, said John Alexander, co-author of a regional conservation plan for Partners in Flight, a national alliance of bird-focused nonprofits and wildlife agencies.
"We haven't found a new roosting site on the West Coast in five years," Schwitters said. "They're tearing them down all the time."
A brick chimney in downtown Los Angeles that attracted as many as 23,000 Vaux's Swifts - one of the largest roosting spots in North America - was capped several years ago to make way for trendy lofts. Another chimney in San Diego has been all but abandoned after a skyscraper went up next to it. And a 66-year-old fire station in Albany, Oregon, that hosted up to 10,000 swifts was torn down this summer because of seismic dangers.
Now, the city is working with the Audubon Society in nearby Corvallis to attract the displaced swifts to a 30-foot-tall replacement tower made of concrete culvert tubes.
The tower is on city land next to a park and within feet of a busy railroad track.
Conservationists have been broadcasting swift calls at 1,100 watts and have smeared swift guano inside the tower, but it hasn't worked yet.
"It might be you have to just get the first one to try it and say, 'Hey guys! It's good in here,'" said Joel Geier, an Audubon Society volunteer bird counter.
If the birds do return, bird lovers hope to set up towers along the West Coast as a safety net for Vaux's Swifts that have lost their chimney roosts.
"We could put these up with donated services for $10,000 apiece, which would be definitely doable when you're looking at the continued decline of the species throughout Western North America," said Jim Fairchild, conservation chair for the Audubon Society of Corvallis. "If it's used in the first couple of years, we'll try another one in another location."
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Migratory birds face new hurdles in their journey

A crowd of several hundred people gathered in the growing...

Donald Trump's running mate is breaking with the Republican nominee's claim that climate change is not the result of human activity.
Vice presidential nominee Mike Pence said Tuesday "there's no question" that human activity affects both the climate and the environment.
At Monday's presidential debate, Democrat Hillary Clinton challenged Trump's views, saying: "Donald thinks that climate change is a hoax perpetrated by the Chinese. I think it's real." Trump interrupted with "I did not, I do not say that."
But in 2012, Trump tweeted that the "concept of global warming was created by and for the Chinese in order to make U.S. manufacturing non-competitive." He later claimed he was kidding, but he's also repeated the assertion that climate change is a hoax benefiting China. And in 2014, Trump tweeted: "Snowing in Texas and Louisiana, record setting freezing temperatures throughout the country and beyond. Global warming is an expensive hoax!"
Trump's campaign manager, Kellyanne Conway, tried to move discussion away from those comments Tuesday, saying on CNN that Trump believes "that climate change is naturally occurring" but the causes are not man-made.
The world's scientific organizations say the Earth's climate is changing because of the buildup of heat-trapping gases, especially carbon dioxide, from the burning of coal, oil and gas.
Pence, appearing separately on CNN, said, "let's follow the science," but he warned against rushing into environmental restrictions that drive jobs out of the country and put Americans out of work.
"What Donald Trump said was a hoax is that bureaucrats in Washington, D.C., can control the climate of the Earth," Pence said. "There's no question that the activities that take place in this country and in countries around the world have some impact on the environment and some impact on climate."
Conway dismissed Trump's previous tweets on climate change.
She questioned how "we're supposed to understand all of his policies" based on tweets or casual remarks he gave before entering politics - such as expressing support for the Iraq war on the Howard Stern show.
But she emphasized that Trump does not believe climate change is man-made.
"He believes climate change is naturally occurring. We don't know what Hillary Clinton believes because nobody ever asks her," Conway said. She derided Clinton's response in the debate, where she said that climate change is real, as "canned" and "scripted."
Clinton has proposed spending $60 billion to switch from dirty fossil fuels to cleaner energy. She promises to deliver on President Barack Obama's pledge that by 2025 the U.S. will be emitting 30 percent less heat-trapping gases than in 2005.
---
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Pence breaks with Trump acknowledging human impact on climate change

Donald Trump's running mate is breaking with the Republican nominee's...

Earth has been losing oxygen for the past 800,000 years. Princeton University researchers have compiled 30 years of data to construct the first ice core-based record of atmospheric oxygen concentrations spanning the past 800,000 years, according to a paper published today in the journal Science.

The record shows that atmospheric oxygen has declined 0.7 percent relative to current atmospheric-oxygen concentrations, a reasonable pace by geological standards, the researchers said. During the past 100 years, however, atmospheric oxygen has declined by a comparatively speedy 0.1 percent because of the burning of fossil fuels, which consumes oxygen and produces carbon dioxide.

Curiously, the decline in atmospheric oxygen over the past 800,000 years was not accompanied by any significant increase in the average amount of carbon dioxide in the atmosphere, though carbon dioxide concentrations do vary over individual ice age cycles. To explain this apparent paradox, the researchers called upon a theory for how the global carbon cycle, atmospheric carbon dioxide and Earth’s temperature are linked on geologic timescales. Earth has been losing oxygen for the past 800,000 years

“The planet has various processes that can keep carbon dioxide levels in check,” said first author Daniel Stolper, a postdoctoral research associate in Princeton’s Department of Geosciences. The researchers discuss a process known as silicate weathering in particular, wherein carbon dioxide reacts with exposed rock to produce, eventually, calcium carbonate minerals, which trap carbon dioxide in a solid form. As temperatures rise due to higher carbon dioxide in the atmosphere, silicate-weathering rates are hypothesized to increase and remove carbon dioxide from the atmosphere faster.

Stolper and his co-authors suggest that the extra carbon dioxide emitted due to declining oxygen concentrations in the atmosphere stimulated silicate weathering, which stabilized carbon dioxide but allowed oxygen to continue to decline.

“The oxygen record is telling us there’s also a change in the amount of carbon dioxide [that was created when oxygen was removed] entering the atmosphere and ocean,” said co-author John Higgins, Princeton assistant professor of geosciences. “However, atmospheric carbon dioxide levels aren’t changing because the Earth has had time to respond via increased silicate-weathering rates.

“The Earth can take care of extra carbon dioxide when it has hundreds of thousands or millions of years to get its act together. In contrast, humankind is releasing carbon dioxide today so quickly that silicate weathering can’t possibly respond fast enough,” Higgins continued. “The Earth has these long processes that humankind has short-circuited.”

The researchers built their history of atmospheric oxygen using measured ratios of oxygen-to-nitrogen found in air trapped in Antarctic ice. This method was established by co-author Michael Bender, professor of geosciences, emeritus, at Princeton.

Because oxygen is critical to many forms of life and geochemical processes, numerous models and indirect proxies for the oxygen content in the atmosphere have been developed over the years, but there was no consensus on whether oxygen concentrations were rising, falling or flat during the past million years (and before fossil fuel burning). The Princeton team analyzed the ice-core data to create a single account of how atmospheric oxygen has changed during the past 800,000 years.

“This record represents an important benchmark for the study of the history of atmospheric oxygen,” Higgins said. “Understanding the history of oxygen in Earth’s atmosphere is intimately connected to understanding the evolution of complex life. It’s one of these big, fundamental ongoing questions in Earth science.”

---

<a href="http://www.princeton.edu" target="_blank" rel="noopener">Princeton University</a>

Earth has been losing oxygen for the past 800,000 years

Earth has been losing oxygen for the past 800,000 years....

The deep, dark twilight zone a kilometer down in the ocean is home to most of the world’s fish, but how they get enough food has largely been a mystery. Now, thanks to satellites and floating sensors, scientists have worked out how much energy is being pumped to the depths.

The ‘mesopelagic region’ is between 100 m and 1000 m below the surface and sustains one of the largest ecosystems on the planet. Sometimes called the twilight zone, because very little light penetrates this far, it remains vastly unexplored and poorly understood.

It was thought that this ecosystem is fed by a ‘rain’ of fast-sinking organic aggregates of dead plankton and waste products from organisms that live near the surface.

While this source of organic carbon is very important, marine scientists have come to realize that it simply is not enough to support the vast numbers and variety of organisms that live in this deep layer of the ocean.

Thanks to a unique approach that combines satellite measurements of ocean color made available through ESA’s Climate Change Initiative and in situ floats, which take direct measurements as they descend and ascend through the water column, it transpires that a ‘seasonal mixed-layer pump’ is responsible for supplying an important additional vital food source.

[caption id="attachment_87590" align="alignleft" width="150"]<img class="size-thumbnail wp-image-87590" src="http://www.earth.com/wp-content/uploads/2016/09/sea-gooseberry_1big_esa-150x150.jpg" alt="Sea gooseberry" width="150" height="150" /> Sea gooseberry[/caption]

During the spring in each hemisphere, strong winds and storms mix the surface waters with the organic carbon it contains and carry non-sinking particles and dissolved organic carbon from the surface down into the depths of the twilight zone.

Critically, in summer, a shallow mixed layer forms at the surface. This effectively ‘traps’ this deeply mixed carbon inside the mesopelagic region – making this energy source available to organisms there.

While it was known that variations in the surface mixed layer could pump part of the missing carbon into the mesopelagic, there has never been a concerted effort to estimate the total amount of organic carbon that is supplied in this way across the world’s oceans.

A paper published in Nature Geoscience describes how scientists at the UK’s Plymouth Marine Laboratory used satellite and local measurements to estimate that the pump moves around 300 million tonnes of carbon each year.

In high-latitude regions, the figure represents an average of 23%, but possibly in excess of 100%, of the better-studied flux of faster-sinking, larger particles and aggregates.

Lead researcher Giorgio Dall’Olmo said, “Most methods for measuring carbon transport into the deep ocean have concentrated on the particles that sink at relatively fast rates, but have not measured how neutrally buoyant or slowly sinking organic particles are redistributed through the water column.

“This means that current global estimates of carbon export in the ocean are missing the potentially important contribution from the seasonal mixed-layer pump.

“Our new global estimates should be considered as an additional flux of organic carbon to the mesopelagic region that was previously not accounted for, and that’s important when we try to understand what sources of energy fuel the mesopelagic ecosystem.”

---

<a href="http://www.esa.int" target="_blank" rel="noopener">European Space Agency</a>

Most of the world's fish live in the oceans' twilight zone

The deep, dark twilight zone a kilometer down in the...

The federal appeals court in Washington is set to hear arguments Tuesday in the legal fight over President Barack Obama's plan to curtail greenhouse gas emissions.
The U.S. Court of Appeals for the District of Columbia Circuit is scheduled to hear oral arguments on the Clean Power Plan, which aims to slow climate change by reducing power-plant emissions by one-third.
The plan has been challenged by more than two dozen mostly Republican-led states, including Texas, and allied business and industry groups tied to fossil fuels. The states deride the carbon-cutting plan unveiled by the Environmental Protection Agency as an "unlawful power grab" that will kill coal-mining jobs and drive up electricity costs.
The Supreme Court has delayed implementation until the legal challenges are resolved.
Implementation of the rules is considered essential to the United States meeting emissions-reduction targets in a global climate agreement signed in Paris last year. The Obama administration and environmental groups also say the plan will spur new clean-energy jobs.
Regardless of which side prevails at the appeals level, the issue is considered likely to end up being decided by the Supreme Court.
The federal plan aims to help stave off the worst predicted impacts of climate change by reducing carbon dioxide emissions at existing power plants by about one-third by 2030. The plan also encourages further development of alternative energy sources such as wind and solar by further ratcheting down any emissions allowed from new coal-fired power plants.
Under the Clean Air Act, certain challenges to new EPA rules skip the federal district court and go directly to the appeals court. A three-judge panel had been scheduled to hear the case in June, but whichever side lost was considered likely to seek a review by the full appeals court.
In a rare step, the full court elected to hold an "en banc" review prior to the smaller panel's decision, which is allowed under procedural rules when the case at issue "involves a question of exceptional importance." By using its discretion to skip a step, the appeals judges are potentially shaving months off the time before the case could be heard by the high court.
The 10 appeals judges set to hear the case could lean toward Obama's position. Six were appointed by Democratic presidents.
Chief appeals judge Merrick Garland, who was nominated by Obama to fill a vacant Supreme Court seat, has recused himself from the case.
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Follow Michael Biesecker on Twitter at <a href="https://twitter.com/mbieseck">https://twitter.com/mbieseck</a>
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Federal appeals court set to hear Clean Power Plan case

The federal appeals court in Washington is set to hear...

More than nine out of 10 people worldwide live in areas with excessive air pollution, contributing to strokes, heart disease, lung cancer and other problems, the World Health Organization said Tuesday.
The U.N. health agency said in a new report that 92 percent of people live in areas where air quality exceeds WHO limits, with southeast Asia, eastern Mediterranean and western Pacific regions hardest hit.
The country-by-country figures come from new satellite data over rural areas to complement traditional ground measurements of pollution, mostly in cities, in about 3,000 places worldwide. A similar WHO report released in May that said 98 percent of residents in large cities of low- and middle-income countries face excessively high air pollution.
WHO says one in nine deaths worldwide is linked to indoor and outdoor pollution.
Turkmenistan has the highest rate of deaths per capita due to ambient air pollution in the WHO's classification, followed by Tajikistan, Uzbekistan, Afghanistan, Egypt and China.
Tuesday's report focuses on outdoor air pollution, which is estimated to kill about 3 million people per year based on 2012 figures, the most recent available.
"There are two things happening. One is: rich countries are getting much better in improving the quality of the air. And two: poorer countries are getting worse. That is the overall trend," said Dr. Carlos Dora, WHO coordinator for environmental and social determinants of health.
The aim is to educate both policymakers and individuals about the risks, at a time of spiraling health care costs. Dora noted, for example, that doctors could advise their patients about higher risks of heart disease in some countries, or how solar lamps could substitute for kerosene lamps that are used in many parts of the developing world.
He said WHO has no evidence that face masks like those worn in many parts of Asia and beyond help reduce exposure to fine particles.
He noted that North America is faring well compared with Europe, mostly due to Europe's greater dependence on diesel fuel and partially due to farm policies that generate agricultural ammonia and methane.
While China ranked sixth among countries with the highest number of deaths per capita tnxdue to ambient air pollution, Dora said the country is doing "an amazing amount of stuff" to fight it, such as with clean cars. But coal-fired power plants, household burning of coal and wood to produce energy, and transportation remain big generators of pollution in China, he said.
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92% of global citizens suffer from excessive air pollution

More than nine out of 10 people worldwide live in...

A common marine crustacean has shown researchers that it’s all set to beat climate change – the males will get more attractive to the females, with a resulting population explosion.

The University of Adelaide study is the first to show how mating behavior could change under the warmer waters and more acidic oceans brought by climate change.

PhD student Katherine Heldt and University of Adelaide ecologist and evolutionary biologist Dr Pablo Munguia studied the herbivorous amphipod, Cymadusa pemptos, in large tanks under the elevated temperature and CO2 predicted for 100 years from now. This work was in collaboration with Professor Sean Connell, Dr Bayden Russell and PhD student Kathryn Anderson.

The amphipod family includes the land-based beach-hopper or sand flea commonly seen hopping around on beaches. In Cymadusa pemptos, like other marine amphipods, males have larger claws than females, which are used as a display to attract females or a weapon to fend off other males.

Published in the journal Scientific Reports, the study found the population increased twenty-fold under predicted warmer waters and high CO2.

“Climate change most usually comes with predictions of severe negative impacts on population sizes, if not extinctions,” says Dr Munguia, in the University’s Environment Institute. “In general, booming populations are not predicted.

“It got even more interesting, however, when we dug deeper and found that males were much larger in size than in previous generations under cooler waters and lower CO2, and their bigger claws were disproportionately larger still. Females stayed the same size.

“On top of that, where there had been variation in large claw size throughout the population, suddenly all the males had large claws. This happened within a few generations.

“It seems that sexual selection for this attractiveness trait could mean that every male was equally attractive to the females, resulting in very large numbers of females – almost 80% – becoming pregnant, causing a massive population explosion.”

Because the future climate change conditions also promoted increased growth of the marine algae which amphipods eat, constraints on competition for food were removed, allowing males to support their energy-demanding bigger claws and enabling the population to grow.

“We know that climate change will be cataclysmic for many species but in some cases it will not,” says Dr Munguia. “This is the first quantitative example of how it will be beneficial for some individual species, albeit with massive consequences to the environment overall.

“We’ve also shown how mating systems may potentially change. If all males are equals in claw size, then perhaps claws will no longer become a key trait. Our research shows how we can start remapping ideas on how mating systems may become modified under future climate.”

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<a href="http://www.adelaide.edu.au/" target="_blank" rel="noopener">University of Adelaide</a>

Some species are combating climate change by getting sexier

A common marine crustacean has shown researchers that it’s all...

Tiny ocean fossils distributed widely across rock surfaces in the Transantarctic Mountains point to the potential for a substantial global sea level rise under conditions of continued global warming, according to a new study.

The study, led by Northern Illinois University geologist Reed Scherer, indicates the massive East Antarctic Ice Sheet (EAIS) has a history of instability during ancient warm periods and could be vulnerable to significant retreat and partial collapse induced by future climate change. The EAIS is the world’s largest ice sheet and most significant player in potential sea-level rise.

The evidence is in the microscopic ocean fossils, known as diatoms, the researchers say.

For decades, scientists have been embroiled in a heated debate over how the diatoms, which were first discovered in the 1980s, became incorporated into the "Sirius Group," a series of glacial sedimentary rocks exposed along the Transantarctic Mountains.

One group of scientists argued that the diatoms accumulated in a marine basin after ice sheet retreat and later, after it got much colder, were moved by the growing glaciers to the mountains. This interpretation suggested a dramatic retreat of the ice sheet between 3 million and 4.5 million years ago, during warm periods of the Pliocene Epoch. But other scientists contended the ice sheet remained stable for at least the past 5 million years, arguing that the diatoms were carried by the wind and deposited atop older sediments.

[caption id="attachment_87577" align="alignleft" width="150"]<img class="size-thumbnail wp-image-87577" src="http://www.earth.com/wp-content/uploads/2016/09/mount-fleming-antarctica_1big_NIU-150x150.jpg" alt="Mt. Fleming in Antarctica" width="150" height="150" /> Mt. Fleming in Antarctica[/caption]

The new study, published Sept. 20, in <a href="http://www.nature.com/ncomms/2016/160920/ncomms12957/full/ncomms12957.html" target="_blank" rel="noopener">Nature Communications</a>, suggests that both sides were partially right and partially wrong—the ice sheet did retreat, and the wind did carry the diatoms.

Using sophisticated ice sheet and climate models, Scherer and colleagues found the ice sheet experienced a series of retreats and re-advances during the Pliocene warm periods, but the retreats were not as dramatic as some scientists earlier suggested. They were significant enough to uncover bays of open seawater in the Aurora and Wilkes basins, with conditions ripe for production of copious amounts of plankton diatoms.

But the retreat removed the weight of the ice, allowing previously submerged land strewn with diatoms to rise above sea level over the next few thousand years. Cyclonic winds then sent plumes of diatoms airborne, depositing them across the Transantarctic Mountains.

“The computer models indicate that the East Antarctic Ice Sheet retreated during the Pliocene by some 300 miles into the interior of East Antarctica,” Scherer said, adding that most of the West Antarctic Ice Sheet also disappeared. “So our findings indicate the Sirius diatoms were windblown, but they came from areas of reduced ice in East Antarctica, where extensive diatom-rich lands became exposed to the air.”

The Antarctic ice cap holds the majority of the world’s fresh water, and a substantial melting and retreat of the ice sheet in the future would result in raised sea levels, with devastating consequences for the world’s coastal regions.

“During certain intervals of Pliocene warmth, the sea level could have been as much as 75 feet higher than it is now,” Scherer said.

[caption id="attachment_87576" align="alignleft" width="150"]<img class="size-thumbnail wp-image-87576" src="http://www.earth.com/wp-content/uploads/2016/09/diatom-Thalassiosira_vulnifica-600x450-150x150.jpg" alt="Diatom Thalassiosira vulnifica" width="150" height="150" /> Diatom Thalassiosira vulnifica[/caption]

“The rise in atmospheric carbon dioxide from burning fossil fuel has now elevated the concentration to 400 parts per million, matching for the first time the levels of the warm Pliocene,” he added. “This makes the old debate about whether the ice sheet was notably smaller than it is now more relevant than ever.”

Models used for the research were developed by co-authors David Pollard of Pennsylvania State University and Robert M. DeConto of the University of Massachusetts.

“The question is always how quickly could sea levels rise, and we’re probably looking at several hundred years into the future before reaching a peak high that matches the Pliocene, but the problem of progressive sea-level rise is already upon us,” Scherer said. “The DeConto/Pollard models assume we continue to burn fossil fuels at the current pace. If we make improvements for the better, ice sheet reduction could be significantly delayed. We’d still have a problem, but we could keep the sea-level rise small and slow.”

The new research represents the first published study on the Sirius fossils that presents data directly related to or indicative of East Antarctic Ice Sheet thickness during the Pliocene.

“This latest work, together with other recent ice sheet modeling studies by DeConto and Pollard, clearly demonstrates the sensitivity of modern ice sheets to warming,” Scherer said. “No model is ever perfect, but these scientists use sophisticated physics and the latest data to produce atmospheric and ice models that are truly state-of-the-art, providing a picture of the past and glimpse into our future.”

Noted climate scientist Richard Alley, also of Penn State, rounds out the author list on the Nature Communications publication.

“This is another piece of a jigsaw puzzle that the community is rapidly putting together, and which appears to show that the ice sheets are more sensitive to warming than we had hoped,” Alley said. “If humans continue to warm the climate, we are likely to commit to large and perhaps rapid sea-level rise that could be very costly. No one piece of the puzzle shows this, but as they fit together, the picture is becoming clearer.”

The authors’ research was supported by funding from the National Science Foundation.

--

<a href="http://www.niu.edu" target="_blank" rel="noopener">North Illinois University</a>

Ocean fossils found in mountains cause for concern over sea level rise

Tiny ocean fossils distributed widely across rock surfaces in the...

A new study paints a picture of an Earth that is warmer than it has been in about 120,000 years, and is locked into eventually hitting its hottest mark in more than 2 million years.
As part of her doctoral dissertation at Stanford University, <a href="http://www.carolynsnyder.com/">Carolyn Snyder</a> , now a climate policy official at the U.S. Environmental Protection Agency, created a continuous 2 million year temperature record, much longer than a previous 22,000 year record. Snyder's temperature reconstruction, published Monday in the journal <a href="http://www.nature.com/nature">Nature</a> , doesn't estimate temperature for a single year, but averages 5,000-year time periods going back a couple million years.
Snyder based her reconstruction on 61 different sea surface temperature proxies from across the globe, such as ratios between magnesium and calcium, species makeup and acidity. But the further the study goes back in time, especially after half a million years, the fewer of those proxies are available, making the estimates less certain, she said.
These are rough estimates with large margins of errors, she said. But she also found that the temperature changes correlated well to carbon dioxide levels.
Temperatures averaged out over the most recent 5,000 years - which includes the last 125 years or so of industrial emissions of heat-trapping gases - are generally warmer than they have been since about 120,000 years ago or so, Snyder found. And two interglacial time periods, the one 120,000 years ago and another just about 2 million years ago, were the warmest Snyder tracked. They were about 3.6 degrees (2 degrees Celsius) warmer than the current 5,000-year average.
With the link to carbon dioxide levels and taking into account other factors and past trends, Snyder calculated how much warming can be expected in the future.
Snyder said if climate factors are the same as in the past - and that's a big if - Earth is already committed to another 7 degrees or so (about 4 degrees Celsius) of warming over the next few thousand years.
"This is based on what happened in the past," Snyder said. "In the past it wasn't humans messing with the atmosphere."
Scientists give various reasons for past changes in carbon dioxide and heat levels, including regular slight shifts in Earth's orbital tilt.
Four outside scientists praised the study's tracking of past temperatures, with caveats about how less certain it is as it gets deeper in the past. Jeremy Shakun of Boston College said "Snyder's work is a great contribution and future work should build on it."
But many of the same scientists said Snyder's estimate of future warming seems too high. Shakun called it unrealistic and not matching historical time periods of similar carbon dioxide levels.
A fifth scientist, Michael Mann of Pennsylvania State University, called the study provocative and interesting but said he remains skeptical until more research confirms it. He found the future temperature calculations "so much higher than prevailing estimates that one has to consider it somewhat of an outlier."
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Online:
Nature: <a href="http://www.nature.com/nature">http://www.nature.com/nature</a>
---
Follow Seth Borenstein at http://twitter.com/borenbears and his work can be found at<a href="http://bigstory.ap.org/content/seth-borenstein">http://bigstory.ap.org/content/seth-borenstein</a>
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Study: Earth is hotter than it has been in over 120,000 years

A new study paints a picture of an Earth 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"

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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



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.

Melt ponds on the Greenland Ice Sheet

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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

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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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Closeup,Of,Fresh,Green,The,Napier,Bush,Grass,As,Animal

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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

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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

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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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Today's Video of the Day from the <a href="http://www.esa.int/">European Space Agency</a> features Qeshm Island in the Strait of Hormuz. This strait provides the only sea passage from the Persian Gulf to the open ocean.



Qeshm is separated from the Iranian coast by the Clarence Strait, also known as Khuran.&nbsp;The Hara Forest Protected Area is a network of shallow waterways and forest located between the island and the mainland. This protected region is home to sea turtles, snakes, and more than 150 species of migrating birds.



Qeshm is famous for its wide range of&nbsp;ecotourist&nbsp;attractions, such as the&nbsp;Hara marine forests. According to environmentalists, about 1.5 percent of the world birds and 25 percent of Iran's native <a href="https://www.earth.com/news/female-hummingbirds-avoid-sexual-harassment-by-looking-like-males/">birds</a> annually migrate to the forests, which are the first national geo park in Iran.



Tourists are also drawn to the island to see an age-old Portuguese&nbsp;fort, historic mosques, the&nbsp;Seyyed Mozaffar&nbsp;and&nbsp;Bibi Maryam&nbsp;shrines, and the "Valley of Stars."



The average temperature on the island is 81 degress and the region is often hot and humid. From June to August, the island is described as being oppressively hot. The ideal time to visit is during the winter season. 



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



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.

Qeshm Island in the Strait of Hormuz

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Today’s Video of the Day from the <a href="https://www.esa.int/">European Space Agency</a> features Inhambane Bay in southeast Mozambique.&nbsp;



"Inhambane Bay is a deep inlet into which the small Mutamba River flows," says ESA. "On one side of the bay lies the historical city of Inhambane, capital of the Inhambane Province, while the sister city of Maxixe, the economic capital of Inhambane, sits across from it. The province is the second largest grower of cashews, after Nampula, and it also produces coconut and citrus fruits."



The beaches of Barra and Tofo are popular with tourists. There are also coral reefs along the long coastline of Inhambane, making it an ideal destination for scuba diving and snorkeling.



"Mozambique’s extensive coastline heightens the country’s vulnerability to tropical cyclones that develop in the Indian Ocean as well as storm surge flooding," says ESA.



"More than half of the population lives in low lying coastal areas, putting communities at risk. Inhambane Bay was dangerously close to where Cyclone Idai made landfall in 2019 causing widespread destruction to the country."



Video/ Image 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.

Inhambane Bay in southeast Mozambique

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Today’s Video of the Day from the <a href="https://www.esa.int/">European Space Agency </a>&nbsp;features the Kangerlussuaq Glacier, one of the largest tidewater outlet glaciers in Greenland. The glacier is located on the east coast of the Greenland ice sheet.



As human-induced climate change continues to drive up temperatures, global ice loss is accelerating at an alarming rate. ESA reports that, over the past decade alone, 3.5 trillion tons of ice have melted from the Greenland ice sheet. This is enough to cover the UK with meltwater 15 meters deep.



Based on satellite imagery, researchers determined that Kangerlussuaq entered a new phase of rapid retreat and acceleration in 2017. In their study, published in <a href="https://www.frontiersin.org/articles/10.3389/feart.2019.00123/full">Frontiers in Earth Science</a>,&nbsp; the experts report that the glacier's ice front is now at its most retreated position since the early 20th century.



"Given Kangerlussuaq’s previous impacts on both the magnitude and pattern of ice sheet wide mass loss, we predict that its new phase of retreat, acceleration and thinning will markedly enhance the south-east region’s contribution to increasing discharge from the ice sheet," wrote the study authors.&nbsp;&nbsp;



"More broadly, accurate forecasting of the ice sheet’s contribution to sea level rise will require a deeper understanding of, and responses to, these non-linear ice dynamic processes."



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.

Kangerlussuaq Glacier on the Greenland ice sheet

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Today’s Video of the Day from the <a href="https://www.esa.int/">European Space Agency</a> describes the complex relationship between ocean and climate. ESA's Climate Change Initiative will help us understand how oceans influence the climate and how climate change is impacting the oceans.&nbsp;



"Earth’s oceans are huge heat stores, soaking up 93% of the excess heat from human activity over the past 70 years. Ocean currents redistribute heat around the planet, from the Equator to the poles. Where this ocean heat goes influences weather patterns and regional climate," explains ESA.



"As well as absorbing heat, oceans are a natural carbon sink, absorbing a quarter of carbon dioxide emissions from human activity. This has led to the acidification of ocean water, threating marine life."



The amount of heat and carbon dioxide soaked up by the ocean depends on specific variables, including phytoplankton, temperatures, waves, salinity, and ice cover. Satellites can be used to measure these variables from space.



"From their unique vantage point, satellites provide key information for understanding the complexities of our planet and monitoring environmental issues," says 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.

Ocean heat influences regional climate

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Today’s Video of the Day from the <a href="https://www.esa.int/">European Space Agency</a> describes the importance of monitoring the shape of the sea surface, which is constantly changing. These observations have many applications, such as ship routing, <a href="https://www.earth.com/news/the-modem-ocean-is-a-tough-place-for-whales-to-survive/">ocean</a> current forecasting, and debris tracking.



"A project supported by the Discovery element of ESA’s Basic Activities recently investigated a new technique to measure sea surface topography very precisely," reports ESA.



"The technique involves looking at satellite navigation (GNSS) signals that have been reflected off of the sea surface at very low angles. At these so-called grazing angles, waves and surface roughness have very little impact on the reflection process; the sea surface acts as a very smooth mirror."



Estel Cardellach is the principal investigator at the Institute for Space Studies of Catalonia, who first submitted the idea for the project.



“In a mirror-like reflection the phase of the signal can be tracked – it is continuous," said Cardellach. "Different surface heights result in different phase measurements. It gives a very precise measurement of the surface altitude at a few centimetres’ precision.”



The researchers developed a GNSS receiver and set up an experiment in the Balaeric Islands to collect signals from the receiver that were reflected off the sea surface. Ultimately, these signals will provide improved measurements of the shape of the sea surface.



Image/ Video Credit: ESA



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

Monitoring the dynamic shape of the sea surface

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