Rare earth elements are everywhere - in your smartphone screen, in the MRI machine at the hospital, in the battery of an electric vehicle, and even in oil and gas refining. They are a key ingredient of modern life.



As global tensions rise, so does the competition for access to these minerals. Recent headlines show the stakes: China has halted rare earth exports to the United States, and a deal was just signed to secure U.S. access to Ukraine’s mineral resources.



Despite their name, rare earth elements aren’t actually scarce; what’s rare is finding them in high enough concentrations to mine economically. These deposits are scattered unevenly across the globe and often buried deep underground, shaping who controls their production and the global supply chain.



Scientists at <a href="https://www.tufts.edu/" target="_blank" rel="noreferrer noopener">Tufts University</a> are trying to better understand how and why rare earth minerals ended up where they did. Their research reveals how the movement of continents over billions of years helped form - and hide - these valuable deposits.



<h2 class="wp-block-heading" id="h-supercontinents-shaped-rare-deposits">Supercontinents shaped rare deposits</h2>



To explain how this mineral drama began, we need to go back in time. Way back. Earth's surface is always on the move. Over millions of years, massive landmasses shift, collide, and break apart, reshaping the planet in the process.



"Most of us are familiar with <a href="https://www.earth.com/earthpedia-articles/supercontinents-101-pannotia-gondwana-and-pangea/" target="_blank" rel="noreferrer noopener">Pangea</a> - the supercontinent that formed about 300 million years ago and that the current seven continents broke off from to form their present-day arrangement," said Jill VanTongeren, professor and chair of the Department of Earth and Climate Sciences.



"But Pangea is only the most recent supercontinent. Throughout Earth history, there have been at least five major <a href="https://www.earth.com/news/australia-north-america-supercontinent/" target="_blank" rel="noreferrer noopener">supercontinent</a> cycles - periods when continents all come together and then spread back out again into different pieces. We think this process happens roughly every 500 million years."



<h2 class="wp-block-heading" id="h-where-minerals-begin">Where minerals begin</h2>



As these continents drifted apart, they created rifts - places where the Earth's tectonic plates pulled away from each other. These rifting zones became birthplaces for rare earth element-rich magmas.



"As the rocks are pushed apart, they decompress, causing melting. It's kind of like taking the lid off a soda bottle, and the bubbles rise to the surface," said VanTongeren.



"Those early magmas contain the highest abundance of rare earth and other incompatible elements that then enter the crust, either erupting in volcanic centers or solidifying at depth."



Some of these mineral-rich magmas cooled and stayed near the surface. Others got dragged back down into the mantle or remain buried too deep to mine with today’s technology.



<h2 class="wp-block-heading" id="h-a-race-for-control-resources">A race for control resources</h2>



Today, the number of economically viable rare earth deposits is limited. China dominates the market, with nearly 70% of global production coming from its Bayan Obo mine. The <a href="https://www.earth.com/news/crucial-rare-earth-elements-discovered-coal-mines-united-states/" target="_blank" rel="noreferrer noopener">U.S.</a> has a smaller operation at Mountain Pass in California, and a few other countries have scattered deposits.



In the late 1990s and early 2000s, China flooded the market with rare earth minerals, driving down prices and shutting down other global producers. That move reshaped global dependence.



In response, the U.S. government took steps to re-establish a domestic supply. Recent investments from the 2021 Infrastructure and Jobs Act and the Department of Defense aim to restart full operations at the Mountain Pass mine, though it could take up to a decade.



There’s also hope that Ukraine's <a href="https://www.earth.com/news/nasa-is-on-a-mission-to-map-americas-mineral-wealth/" target="_blank" rel="noreferrer noopener">mineral deposits</a> could help diversify supply. But for now, their potential remains unclear.



"Political boundaries and the desire to obtain access to mineral resources have been the source of economic and military conflicts throughout human history," said VanTongeren. "This is likely to continue as the world shifts toward green energy and a greater dependence on rare earth elements in the future."



<h2 class="wp-block-heading" id="h-hunting-for-mineral-deposits">Hunting for mineral deposits</h2>



VanTongeren’s work tracks these mineral stories from source to surface. Her fieldwork has taken her from a ship near Antarctica to platinum mines in South Africa, Morocco’s mountains, and even a <a href="https://www.earth.com/news/huge-lithium-deposit-from-volanic-ash-found-in-pennsylvania/" target="_blank" rel="noreferrer noopener">lithium</a> discovery in Maine.



"It's a fascinating area of study partly because it lies at the intersection of science, economics, and politics," she said. Back on the Tufts campus, this intersection takes a more visual form.



<h2 class="wp-block-heading" id="h-tufts-secret-mineral-vault">Tufts' secret mineral vault</h2>



Tucked into the basement of Lane Hall, the P.T. Barnum Mineral Collection offers a glimpse into the Earth’s treasures. It includes thousands of mineral specimens, some collected by Barnum himself. He was an early supporter of Tufts and a major collector of natural history in the 1800s.



"In the late 1800s, it was considered fashionable for many prominent individuals to accumulate their own natural history collections," noted VanTongeren.



"P.T. Barnum was one of the biggest collectors of the time. His collection of animals, plants, and minerals was among the first gifts to Tufts University and part of an endowment to establish Tufts as one of the major natural history museums in the country."



After a fire destroyed the Barnum Museum in 1975, the mineral collection moved to Lane Hall. Now, it’s about to move again - this time to Bacon Hall, the new home for the Department of Earth and Climate Sciences.



<h2 class="wp-block-heading" id="h-global-hunt-for-rare-earth-elements">Global hunt for rare earth elements</h2>



VanTongeren hopes this new home will be more than just a storage site. She wants it to become a space that encourages curiosity and exploration, not just for scientists, but for everyone.



"My pie-in-the-sky vision is to set up a mineral gallery with both a permanent exhibit as well as pop-up exhibitions every semester highlighting minerals important for technology, related to other research at the university, or to global events," said VanTongeren.



"I'd like to help bring back Barnum's vision of bringing the beauty of, and an appreciation for, the natural world to campus."



-----



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Global hunt for rare earth elements is underway

Rare earth elements are everywhere - in your smartphone screen, in the MRI machine at the hospital, in the battery of an electric vehicle, and even in oil and gas refining. They are a key ingredient of modern life. As global tensions rise, so does the competition for access to these minerals. Recent headlines show the stakes: China has halted rare earth exports to the United States, and a deal was just signed to secure U.S. access to Ukraine’s mineral resources. Despite their name, rare earth elements...

Sierra Exif JPEG

Regional Differences In Sea Level Rise Becoming More Apparent. When you fill a sink, the water rises at the same rate to the same height in every corner. That's not the way it works with our rising seas.

According to the 23-year record of satellite data from <a href="https://www.bing.com/search?q=Nasa&amp;cvid=99708273b699490ab7869a0486cfbb3a&amp;FORM=ANAB01&amp;PC=HCTS">NASA</a> and its partners, the sea level is rising a few millimeters a year -- a fraction of an inch. If you live on the U.S. East Coast, though, your sea level is rising two or three times faster than average. If you live in Scandinavia, it's falling. Residents of China's Yellow River delta are swamped by sea level rise of more than nine inches (25 centimeters) a year. Regional Differences In Sea Level Rise Becoming More Apparent

These regional differences in sea level change will become even more apparent in the future, as ice sheets melt. For instance, when the Amundsen Sea sector of the West Antarctic Ice Sheet is totally gone, the average global sea level will rise four feet. But the East Coast of the United States will see an additional 14 to 15 inches above that average.

Tides, winds and ocean currents play a role in these regional differences, but an increasingly important mover and shaker is the solid Earth itself. Global warming is not just affecting the surface of our world; it's making the Earth move under our feet. Regional Differences In Sea Level Rise Becoming More Apparent

Unless a volcano or earthquake are in the news, we tend to think of our home planet as solid rock. But 50 miles below our feet, there's a layer thousands of miles thick that can flow like a liquid over thousands of years. The tectonic plates of Earth's crust float on this viscous layer, called the mantle, like a vanilla wafer on a very thick pudding.

[caption id="attachment_2384134" align="alignleft" width="150"]<a href="http://cff1.greenatom.net/uploads/2015/08/27091856/greenland-bedrock-rise_1big_nasa.jpg"><img class="size-thumbnail wp-image-2384134" src="http://cff1.greenatom.net/uploads/2015/08/27091856/greenland-bedrock-rise_1big_nasa-150x150.jpg" alt="Greenland's rising bedrock interacts with its ice loss from global climate change." width="150" height="150" /></a> Greenland's rising bedrock interacts with its ice loss from global climate change.[/caption]

If you were to put a strawberry on top of that vanilla wafer, the added weight would make the cookie sink into the pudding. In the same way, heavy weights on Earth's crust push it down into the mantle, which flows away and bulges out elsewhere. The miles-thick ice sheets of <a href="http://www.earth.com/image/nearly-all-of-greenlands-glaciers-are-retreating/">Greenland</a> and Antarctica have been depressing the crust beneath them for millennia. That weight has a second effect that you won't see in your dessert: its gravitational pull on the surrounding ocean makes seawater pile up around the coastlines.

These weight-filled dents in the mantle don't make a permanent scar. When the extra weight lifts, the mantle rebounds. This doesn't just happen at the majestic pace of mountain ranges crumbling. It happens every day.

"The solid earth can respond very quickly -- nearly instantaneously," said Mark Tamisiea, a scientist at the National Oceanography Centre, Liverpool, England, who studies the connection between sea levels and Earth processes. Tamisiea cited the example of solid-Earth tides, which pull the crust outward as much as a foot (30 centimeters) toward the moon as it passes overhead. Similarly, Earth has an instant initial response to glaciers and ice sheets melting, called the elastic response.

Since NASA launched the Gravity Recovery and Climate Experiment twin satellites in 2002, scientists have had an extremely precise measurement of the contribution that ice sheets' loss of mass contributes to changes in gravity and what it is adding to sea level rise. "Because of GRACE, we've had a pretty good idea of what's happening since 2002," said Steve Nerem of the University of Colorado, head of NASA's Sea Level Change Team. "We know how much [of sea level rise] is from Greenland, how much is from Antarctica, how much is from glaciers."

Because every ice sheet and glacier has a unique location and size, each one creates a pattern of response in the ocean as individual as a fingerprint. "The physics behind understanding these fingerprints is very well understood," Tamisiea said. "It's like the tides." He and Jerry Mitrovica of Harvard University have calculated the fingerprints of East and West Antarctica and Greenland around the globe. "We do each ice sheet individually so we can use the latest GRACE analysis," Tamisiea explained. "You can sort of add the effects up and see what the result is for any given location."

As any ice sheet melts, sea levels along coastlines as much as 1,500 miles (2,000 kilometers) away will fall as seawater escapes from the reduced gravitational pull and the crust lifts. The escaping seawater flows clear across the equator: the melting of Antarctica affects the U.S. East and West coasts, and Greenland's disappearance impacts the coastline of Brazil. These regional differences are significant – such as in the case of the East Coast of the United States.

The East Coast is also on the losing end of another important solid-Earth process that affects regional sea levels: post-glacial rebound. After the elastic response to a crustal weight loss, uplift continues more slowly for many millennia. North America is still responding to the massive melt-off at the end of the last ice age 6,000 years ago. The North American tectonic plate wasn't evenly loaded during that ice age: ice sheets were sitting on what is now Canada and Greenland, while most of today's United States remained ice free. This ice load pushed the mantle out from under Canada and buoyed up the United States. Today, the U.S. side of the North American plate is sinking like the downhill end of a seesaw as the northern side continues to lift.

Greenland's uplift from postglacial rebound means the island is gaining mass from below and its bedrock is continuously rising. At the same time, it is losing mass from above as its ice melts. GRACE measures the net result of these opposing processes, not just the result of melting ice alone. A National Science Foundation- and NASA-funded program called the Greenland GPS Network is working to overcome this problem. Led by Michael Bevis of Ohio State University, the program is using more than 50 GPS stations in Greenland to measure Greenland's rise and fall. The network is dense enough, and the instruments record elevation precisely enough, to distinguish the steady, long-term rise caused by postglacial rebound from shorter-term changes in elevation caused by the weight of the winter snows and loss of weight in summer. The goal of the project is to provide a "correction factor" for postglacial rebound that can be applied to measurements by GRACE and succeeding missions so that the remainder is an accurate measurement of the loss of mass from melting.

Scientists currently believe that ice sheet fingerprints will be the major driver of future regional variations in sea levels. They are working on questions of how these solid-Earth processes interact with other global and local drivers of sea level rise. "We have to understand global and larger-scale regional changes to do localized impact studies," Tamisiea explained. "In some places, it may very well be that regional processes will be the most important signal. There has to be a continuum of understanding of the global average, regional changes, and more localized processes. We'll need all of those layers to make viable predictions."

---

<a href="http://www.nasa.gov" target="_blank" rel="noopener noreferrer">NASA</a>

Regional Differences In Sea Level Rise Becoming More Apparent

Regional Differences In Sea Level Rise Becoming More Apparent. When...

Regional Differences In Sea Level Rise Becoming More Apparent. When you fill a sink, the water rises at the same rate to the same height in every corner. That's not the way it works with our rising seas.

According to the 23-year record of satellite data from <a href="https://en.wikipedia.org/wiki/NASA">NASA</a> and its partners, the sea level is rising a few millimeters a year -- a fraction of an inch. If you live on the U.S. East Coast, though, your sea level is rising two or three times faster than average. If you live in Scandinavia, it's falling. Residents of China's Yellow River delta are swamped by sea level rise of more than nine inches (25 centimeters) a year.

These regional differences in sea level change will become even more apparent in the future, as ice sheets melt. For instance, when the Amundsen Sea sector of the West <a href="http://www.earth.com/video/business-as-usual-in-antarctica/">Antarctic</a> Ice Sheet is totally gone, the average global sea level will rise four feet. But the East Coast of the United States will see an additional 14 to 15 inches above that average. Regional Differences In Sea Level Rise Becoming More Apparent

Tides, winds and ocean currents play a role in these regional differences, but an increasingly important mover and shaker is the solid Earth itself. Global warming is not just affecting the surface of our world; it's making the Earth move under our feet.

Unless a volcano or earthquake are in the news, we tend to think of our home planet as solid rock. But 50 miles below our feet, there's a layer thousands of miles thick that can flow like a liquid over thousands of years. The tectonic plates of Earth's crust float on this viscous layer, called the mantle, like a vanilla wafer on a very thick pudding.

[caption id="attachment_2384134" align="alignleft" width="150"]<a href="http://cff1.greenatom.net/uploads/2015/08/27091856/greenland-bedrock-rise_1big_nasa.jpg"><img class="size-thumbnail wp-image-2384134" src="http://cff1.greenatom.net/uploads/2015/08/27091856/greenland-bedrock-rise_1big_nasa-150x150.jpg" alt="Greenland's rising bedrock interacts with its ice loss from global climate change." width="150" height="150" /></a> Greenland's rising bedrock interacts with its ice loss from global climate change.[/caption]

If you were to put a strawberry on top of that vanilla wafer, the added weight would make the cookie sink into the pudding. In the same way, heavy weights on Earth's crust push it down into the mantle, which flows away and bulges out elsewhere. The miles-thick ice sheets of Greenland and Antarctica have been depressing the crust beneath them for millennia. That weight has a second effect that you won't see in your dessert: its gravitational pull on the surrounding ocean makes seawater pile up around the coastlines.

These weight-filled dents in the mantle don't make a permanent scar. When the extra weight lifts, the mantle rebounds. This doesn't just happen at the majestic pace of mountain ranges crumbling. It happens every day.

"The solid earth can respond very quickly -- nearly instantaneously," said Mark Tamisiea, a scientist at the National Oceanography Centre, Liverpool, England, who studies the connection between sea levels and Earth processes. Tamisiea cited the example of solid-Earth tides, which pull the crust outward as much as a foot (30 centimeters) toward the moon as it passes overhead. Similarly, Earth has an instant initial response to glaciers and ice sheets melting, called the elastic response.

Since NASA launched the Gravity Recovery and Climate Experiment twin satellites in 2002, scientists have had an extremely precise measurement of the contribution that ice sheets' loss of mass contributes to changes in gravity and what it is adding to sea level rise. "Because of GRACE, we've had a pretty good idea of what's happening since 2002," said Steve Nerem of the University of Colorado, head of NASA's Sea Level Change Team. "We know how much [of sea level rise] is from Greenland, how much is from Antarctica, how much is from glaciers."

Because every ice sheet and glacier has a unique location and size, each one creates a pattern of response in the ocean as individual as a fingerprint. "The physics behind understanding these fingerprints is very well understood," Tamisiea said. "It's like the tides." He and Jerry Mitrovica of Harvard University have calculated the fingerprints of East and West Antarctica and Greenland around the globe. "We do each ice sheet individually so we can use the latest GRACE analysis," Tamisiea explained. "You can sort of add the effects up and see what the result is for any given location."

As any ice sheet melts, sea levels along coastlines as much as 1,500 miles (2,000 kilometers) away will fall as seawater escapes from the reduced gravitational pull and the crust lifts. The escaping seawater flows clear across the equator: the melting of Antarctica affects the U.S. East and West coasts, and Greenland's disappearance impacts the coastline of Brazil. These regional differences are significant – such as in the case of the East Coast of the United States.

The East Coast is also on the losing end of another important solid-Earth process that affects regional sea levels: post-glacial rebound. After the elastic response to a crustal weight loss, uplift continues more slowly for many millennia. North America is still responding to the massive melt-off at the end of the last ice age 6,000 years ago. The North American tectonic plate wasn't evenly loaded during that ice age: ice sheets were sitting on what is now Canada and Greenland, while most of today's United States remained ice free. This ice load pushed the mantle out from under Canada and buoyed up the United States. Today, the U.S. side of the North American plate is sinking like the downhill end of a seesaw as the northern side continues to lift.

Greenland's uplift from postglacial rebound means the island is gaining mass from below and its bedrock is continuously rising. At the same time, it is losing mass from above as its ice melts. GRACE measures the net result of these opposing processes, not just the result of melting ice alone. A National Science Foundation- and NASA-funded program called the Greenland GPS Network is working to overcome this problem. Led by Michael Bevis of Ohio State University, the program is using more than 50 GPS stations in Greenland to measure Greenland's rise and fall. The network is dense enough, and the instruments record elevation precisely enough, to distinguish the steady, long-term rise caused by postglacial rebound from shorter-term changes in elevation caused by the weight of the winter snows and loss of weight in summer. The goal of the project is to provide a "correction factor" for postglacial rebound that can be applied to measurements by GRACE and succeeding missions so that the remainder is an accurate measurement of the loss of mass from melting.

Scientists currently believe that ice sheet fingerprints will be the major driver of future regional variations in sea levels. They are working on questions of how these solid-Earth processes interact with other global and local drivers of sea level rise. "We have to understand global and larger-scale regional changes to do localized impact studies," Tamisiea explained. "In some places, it may very well be that regional processes will be the most important signal. There has to be a continuum of understanding of the global average, regional changes, and more localized processes. We'll need all of those layers to make viable predictions."

---

<a href="http://www.nasa.gov" target="_blank" rel="noopener noreferrer">NASA</a>

Study: Climate Change Can Alter Genetic Diversity Of Plants. A study by the University of Liverpool has found that the genetic diversity of wild plant species could be altered rapidly by anthropogenic climate change.

Scientists studied the genetic responses of different wild plant species, located in a natural grassland ecosystem near Buxton, to a variety of simulated climate change treatments--including drought, watering, and warming--over a 15-year period.

Analysis of DNA markers in the plants revealed that the climate change treatments had altered the genetic composition of the plant populations. The results also indicated a process of evolutionary change in one of the study species, suggesting that genetic diversity may be able to buffer plants against the harmful effects of climate change, allowing an "evolutionary rescue" Study: Climate Change Can Alter Genetic Diversity Of Plants

Dr Raj Whitlock, from the University's Institute of Integrative Biology, said:

"Climate change is expected to present a significant challenge to the persistence of many populations of wild plant species.

"Our understanding of the potential for such responses to climate change is still limited, and there have been very few experimental tests carried out within intact ecosystems.

"We found that experimental climate change treatments can modify the genetic structure of plant populations within 15 years, which is very fast, in evolutionary terms.

"Evolutionary flexibility within the plant populations at Buxton may help to explain why the grassland there has proven resistant to simulated environmental change."

The experiment took place at the Buxton Climate Change Impacts Laboratory (BCCIL) in Derbyshire, where intact species-rich limestone grassland has been subjected to experimentally manipulated climate treatments since 1993 (involving summer drought, increased temperature, and enhanced rainfall). BCCIL was set up by Prof Phil Grime (University of Sheffield), and is currently run by Dr Jason Fridley (Syracuse University) and Prof Grime, with support from the USA's National Science Foundation. Climate treatments at the site are amongst the longest-running multi-factor climate manipulations anywhere in the world.

---

<a href="http://www.liv.ac.uk/" target="_blank" rel="noopener">University of Liverpool</a>

Study: Climate Change Can Alter Genetic Diversity Of Plants

Study: Climate Change Can Alter Genetic Diversity Of Plants. A...

Regional Differences In Sea Level Rise Becoming More Apparent. These regional differences in sea level rise will become even more apparent in the future, as ice sheets melt. When you fill a sink, the water rises at the same rate to the same height in every corner. That's not the way it works with our rising seas.

According to the 23-year record of satellite data from NASA and its partners, the sea level is rising a few millimeters a year -- a fraction of an inch. If you live on the U.S. <a href="http://www.earth.com/news/shellfish-harvests-declining-warming/">East Coast</a>, though, your sea level is rising two or three times faster than average. If you live in Scandinavia, it's falling. Residents of China's Yellow River delta are swamped by sea level rise of more than nine inches (25 centimeters) a year.Regional Differences In Sea Level Rise Becoming More Apparent

These regional differences in sea level change will become even more apparent in the future, as ice sheets melt. For instance, when the Amundsen Sea sector of the West <a href="https://www.bing.com/search?q=arctic+ocean&amp;FORM=EDGENA&amp;PC=HCTS&amp;refig=06f30f4e602a4654d276cea6f9598ffb">Antarctic</a> Ice Sheet is totally gone, the average global sea level will rise four feet. But the East Coast of the United States will see an additional 14 to 15 inches above that average.

Tides, winds and ocean currents play a role in these regional differences, but an increasingly important mover and shaker is the solid Earth itself. Global warming is not just affecting the surface of our world; it's making the Earth move under our feet.

Unless a volcano or earthquake are in the news, we tend to think of our home planet as solid rock. But 50 miles below our feet, there's a layer thousands of miles thick that can flow like a liquid over thousands of years. The tectonic plates of Earth's crust float on this viscous layer, called the mantle, like a vanilla wafer on a very thick pudding.

[caption id="attachment_2384134" align="alignleft" width="150"]<a href="http://cff1.greenatom.net/uploads/2015/08/27091856/greenland-bedrock-rise_1big_nasa.jpg"><img class="size-thumbnail wp-image-2384134" src="http://cff1.greenatom.net/uploads/2015/08/27091856/greenland-bedrock-rise_1big_nasa-150x150.jpg" alt="Greenland's rising bedrock interacts with its ice loss from global climate change." width="150" height="150" /></a> Greenland's rising bedrock interacts with its ice loss from global climate change.[/caption]

If you were to put a strawberry on top of that vanilla wafer, the added weight would make the cookie sink into the pudding. In the same way, heavy weights on Earth's crust push it down into the mantle, which flows away and bulges out elsewhere. The miles-thick ice sheets of Greenland and Antarctica have been depressing the crust beneath them for millennia. That weight has a second effect that you won't see in your dessert: its gravitational pull on the surrounding ocean makes seawater pile up around the coastlines.

These weight-filled dents in the mantle don't make a permanent scar. When the extra weight lifts, the mantle rebounds. This doesn't just happen at the majestic pace of mountain ranges crumbling. It happens every day.

"The solid earth can respond very quickly -- nearly instantaneously," said Mark Tamisiea, a scientist at the National Oceanography Centre, Liverpool, England, who studies the connection between sea levels and Earth processes. Tamisiea cited the example of solid-Earth tides, which pull the crust outward as much as a foot (30 centimeters) toward the moon as it passes overhead. Similarly, Earth has an instant initial response to glaciers and ice sheets melting, called the elastic response.

Since NASA launched the Gravity Recovery and Climate Experiment twin satellites in 2002, scientists have had an extremely precise measurement of the contribution that ice sheets' loss of mass contributes to changes in gravity and what it is adding to sea level rise. "Because of GRACE, we've had a pretty good idea of what's happening since 2002," said Steve Nerem of the University of Colorado, head of NASA's Sea Level Change Team. "We know how much [of sea level rise] is from Greenland, how much is from Antarctica, how much is from glaciers."

Because every ice sheet and glacier has a unique location and size, each one creates a pattern of response in the ocean as individual as a fingerprint. "The physics behind understanding these fingerprints is very well understood," Tamisiea said. "It's like the tides." He and Jerry Mitrovica of Harvard University have calculated the fingerprints of East and West Antarctica and Greenland around the globe. "We do each ice sheet individually so we can use the latest GRACE analysis," Tamisiea explained. "You can sort of add the effects up and see what the result is for any given location."

As any ice sheet melts, sea levels along coastlines as much as 1,500 miles (2,000 kilometers) away will fall as seawater escapes from the reduced gravitational pull and the crust lifts. The escaping seawater flows clear across the equator: the melting of Antarctica affects the U.S. East and West coasts, and Greenland's disappearance impacts the coastline of Brazil. These regional differences are significant – such as in the case of the East Coast of the United States.

The East Coast is also on the losing end of another important solid-Earth process that affects regional sea levels: post-glacial rebound. After the elastic response to a crustal weight loss, uplift continues more slowly for many millennia. North America is still responding to the massive melt-off at the end of the last ice age 6,000 years ago. The North American tectonic plate wasn't evenly loaded during that ice age: ice sheets were sitting on what is now Canada and Greenland, while most of today's United States remained ice free. This ice load pushed the mantle out from under Canada and buoyed up the United States. Today, the U.S. side of the North American plate is sinking like the downhill end of a seesaw as the northern side continues to lift.

Greenland's uplift from postglacial rebound means the island is gaining mass from below and its bedrock is continuously rising. At the same time, it is losing mass from above as its ice melts. GRACE measures the net result of these opposing processes, not just the result of melting ice alone. A National Science Foundation- and NASA-funded program called the Greenland GPS Network is working to overcome this problem. Led by Michael Bevis of Ohio State University, the program is using more than 50 GPS stations in Greenland to measure Greenland's rise and fall. The network is dense enough, and the instruments record elevation precisely enough, to distinguish the steady, long-term rise caused by postglacial rebound from shorter-term changes in elevation caused by the weight of the winter snows and loss of weight in summer. The goal of the project is to provide a "correction factor" for postglacial rebound that can be applied to measurements by GRACE and succeeding missions so that the remainder is an accurate measurement of the loss of mass from melting.

Scientists currently believe that ice sheet fingerprints will be the major driver of future regional variations in sea levels. They are working on questions of how these solid-Earth processes interact with other global and local drivers of sea level rise. "We have to understand global and larger-scale regional changes to do localized impact studies," Tamisiea explained. "In some places, it may very well be that regional processes will be the most important signal. There has to be a continuum of understanding of the global average, regional changes, and more localized processes. We'll need all of those layers to make viable predictions."

---

<a href="http://www.nasa.gov" target="_blank" rel="noopener noreferrer">NASA</a>

Regional Differences In Sea Level Rise Becoming More Apparent. These...

Scientists Issue More Warnings Over Thawing Permafrost. As President Obama and high-level representatives of other nations converge in Anchorage, Alaska on August 30-31 for the Conference on Global Leadership in the <a href="https://www.bing.com/search?q=arctic+ocean&amp;FORM=EDGENA&amp;PC=HCTS&amp;refig=06f30f4e602a4654d276cea6f9598ffb">Arctic</a>: Cooperation, Innovation, Engagement and Resilience (GLACIER), hosted by the U.S. Department of State, top U.S. climate scientists urge policymakers to address the critical problem of the thawing permafrost in the Arctic region.

Arctic permafrost - ground that has been frozen for many thousands of years - is now thawing because of global climate change, and the results could be disastrous and irreversible.

"The release of greenhouse gases resulting from thawing Arctic permafrost could have catastrophic global consequences," said Dr. Max Holmes, a Senior Scientist at the Woods Hole Research Center (WHRC) who has been advising State Department officials on the problem.

Thawing permafrost releases greenhouse gases (carbon dioxide and methane) into the atmosphere, which accelerates climate change, which in turn causes more thawing of the permafrost. This potentially unstoppable and self-reinforcing cycle could constitute a calamitous "tipping point."

WHRC scientists have counseled the State Department on policies that could control this problem, including reducing global carbon emissions from fossil fuel use and deforestation, and limiting emissions of "black carbon," sooty particles that darken snow and ice and hasten Arctic warming.

"Despite the importance and urgency of this problem, until now it has received little attention from policymakers," said Dr. Sue Natali, another WHRC <a href="http://www.earth.com/news/scientists-explore-the-basis-of-animal-decision-making/">scientist</a>. A study published earlier this year by Dr. Natali and WHRC scientists estimated that greenhouse gases released from thawing permafrost could make it much more difficult to meet the widely held goal of limiting global warming to 2 degrees Celsius.

"The United States must lead a large-scale effort to find the tipping point - at what level of warming will the cycle of warming and permafrost thawing become impossible to stop," said Dr. Holmes. "The real and imminent threat posed by permafrost thawing must be communicated clearly and broadly to the general public and the policy community."

The key science points, implications and recommendations can be found in the WHRC Policy Brief, "<a href="http://whrc.org/wp-content/uploads/2015/06/PB_Permafrost.pdf" target="_blank" rel="noopener noreferrer">Permafrost and Global Climate Change</a>."

---

<a href="http://www.whrc.org/" target="_blank" rel="noopener noreferrer">Woods Hole Research Institute</a>

Scientists Issue More Warnings Over Thawing Permafrost

Scientists Issue More Warnings Over Thawing Permafrost. As President Obama...

Sea Fog Over Coastal California Contains Mercury. What do the roof of a building in a West Coast redwood forest, a bluff in California chaparral, and a research vessel in <a href="http://www.earth.com/news/microplastics-monterey-bay/">Monterey Bay</a> have in common?

They're often draped in tendrils of fog. That makes them prime sites for collecting fog water samples. And there's something else that can be found at those sites: mercury, according to atmospheric chemist Peter Weiss-Penzias of the University of California at <a href="https://www.bing.com/search?q=santa+cruz&amp;form=EDGEAR&amp;qs=PF&amp;cvid=9e06ae999a9d4741906a9ed384dfcd66&amp;cc=US&amp;setlang=en-US&amp;elv=AY3%21uAY7tbNNZGZ2yiGNjfOBcxbQRbvDfQi*Dv3Rctz2DIOGgIwIpR5QFAJIUQDftMhwSnHcA8KYpL1%21flsp5Xqzo16kmZxqc2mlF0xkWjLS&amp;plvar=0&amp;PC=HCTS">Santa Cruz</a> (UCSC).

Mercury: rolling in with fog

Sea fog is a significant, but previously overlooked, source of toxic monomethyl mercury deposited in coastal environments, Weiss-Penzias and colleagues reported at the December 2014, American Geophysical Union (AGU) Fall Meeting in San Francisco.Sea Fog Over Coastal California Contains Mercury

Their research is funded by the National Science Foundation (NSF)'s Chemical Oceanography Program in its Division of Ocean Sciences.

"'Fog drip' could deliver unsafe levels of monomethyl mercury to upland and near-shore ecosystems along the Pacific Coast," Weiss-Penzias says.

Other scientists had previously found high levels of mercury in Monterey Bay during coastal upwelling events--occasions when winds drive surface water offshore and colder water from the deep moves in to replace it. That gave Weiss-Penzias and colleagues the idea to find out whether mercury was somehow stealing ashore in fog.

Mercury is a heavy metal neurotoxin that bioaccumulates and bioconcentrates--primarily as monomethyl mercury--in aquatic food webs. It often reaches high levels in fish and other animals, making them unsafe for human consumption.

The source of monomethyl mercury in aquatic organisms has been debated, says Weiss, "but atmospheric deposition has been implicated as a pathway. Emissions such as coal combustion likely make a significant contribution."

That deposition affects all forms of precipitation: rain, snow and fog.

Weiss-Penzias and other researchers started their search by collecting fog samples by dark of night from June through August 2011.

They worked only in blackness so there would be no decomposition of mercury from sunlight, moving a single fog water collector among four locations near Santa Cruz: the roof of a UCSC building located in a redwood forest; a bluff at UCSC's Long Marine Laboratory; the Moss Landing Marine Labs' research vessel John H. Martin in Moss Landing Harbor; and on offshore spot in Monterey Bay where the John H. Martin was temporarily moored.

FogNet: a dragnet for mercury

The scientists then expanded their goals. Their NSF-funded project, called FogNet, involves sampling fog from seven locations along the California coast, from Eureka to Monterey.

FogNet is a collaborative effort among researchers at UCSC, Moss Landing Marine Labs, California State University-Monterey Bay, Humboldt State University Marine Laboratory, University of California-Davis Bodega Bay Marine Laboratory, San Francisco State University, Pepperwood Preserve and the U.S. Geological Survey.

The project will collect fog water during the summers of 2014 through 2016 for chemical characterization and quantification of fog deposition volume, Weiss-Penzias says.

The new data show elevated monomethyl mercury concentrations, similar to those the team revealed at the December AGU conference, as well as in a paper published in 2012 in the AGU journal Geophysical Research Letters.

"The hypothesis we're now testing," Weiss-Penzias says, "is whether a form of mercury called dimethyl mercury produced in the coastal ocean can be incorporated into cloud droplets, then be deposited in ecosystems on land and become an important, or even dominant, contributor to monomethyl mercury there."

Fog samples are being collected at Marina Airport, Long Marine Laboratory, UCSC, Montara Lighthouse, Bodega Bay, Pepperwood Preserve, and Humboldt State University Marine Laboratory.

Hidden in the mist

The average monomethyl mercury concentration in the fog water samples taken in 2011 was five-fold greater than the previously reported highest monomethyl mercury levels in rain water.

"There haven't been reports of monomethyl mercury measurements in fog water in the scientific literature," says Weiss. "But these elevated concentrations suggest that fog could be a significant source in coastal environments."

Could fog be a vector for not only mercury, but other toxic elements?

"We really don't know," says Weiss. "The potentially far-reaching consequences of these results, however, underscore the need to collect fog water in various locations along the coast."

Weiss-Penzias has teamed with UCSC biologist Chris Wilmers for one of the next steps in the research. Wilmers is providing hair and whisker samples from mountain lions that roam the oft-foggy Santa Cruz Mountains and Sierra Nevada foothills, where mercury was used in the Gold Rush era due to its ability to extract the precious metal from other materials.

Early results show that whiskers from coastal mountain lions contain mercury levels that are, on average, 10 times higher than those of their inland counterparts.

"We're looking at whether the mercury is linked with plants eaten by the mountain lions' main prey--deer," says Weiss-Penzias.

The scientist says he's constantly looking for mercury. When walks down his driveway to pick up the morning paper, he wonders what's in the dew.

"If my feet are wet when I get back in," he says, "I'm thinking: 'it was foggy enough last night to get a good sample.'"

---

<a href="http://www.nsf.gov" target="_blank" rel="noopener noreferrer">National Science Foundation</a>

Sea Fog Over Coastal California Contains Mercury

Sea Fog Over Coastal California Contains Mercury. What do the...

Sea Fog Over Coastal California Contains Mercury. What do the roof of a building in a West Coast redwood forest, a bluff in California chaparral, and a research vessel in Monterey Bay have in common?

They're often draped in tendrils of fog. That makes them prime sites for collecting fog water samples. And there's something else that can be found at those sites: mercury, according to atmospheric chemist Peter Weiss-Penzias of the University of<a href="https://www.bing.com/search?q=santa+cruz&amp;form=EDGEAR&amp;qs=PF&amp;cvid=9e06ae999a9d4741906a9ed384dfcd66&amp;cc=US&amp;setlang=en-US&amp;elv=AY3%21uAY7tbNNZGZ2yiGNjfOBcxbQRbvDfQi*Dv3Rctz2DIOGgIwIpR5QFAJIUQDftMhwSnHcA8KYpL1%21flsp5Xqzo16kmZxqc2mlF0xkWjLS&amp;plvar=0&amp;PC=HCTS"> California</a> at Santa Cruz (UCSC).

Mercury: rolling in with fog

Sea fog is a significant, but previously overlooked, source of toxic monomethyl mercury deposited in coastal environments, Weiss-Penzias and colleagues reported at the December 2014, <a href="http://www.earth.com/news/most-americans-plan-to-improve-self-care-after-pandemic/">American</a> Geophysical Union (AGU) Fall Meeting in San Francisco.

Their research is funded by the National Science Foundation (NSF)'s Chemical Oceanography Program in its Division of Ocean Sciences.Sea Fog Over Coastal California Contains Mercury

"'Fog drip' could deliver unsafe levels of monomethyl mercury to upland and near-shore ecosystems along the Pacific Coast," Weiss-Penzias says.

Other scientists had previously found high levels of mercury in Monterey Bay during coastal upwelling events--occasions when winds drive surface water offshore and colder water from the deep moves in to replace it. That gave Weiss-Penzias and colleagues the idea to find out whether mercury was somehow stealing ashore in fog.

Mercury is a heavy metal neurotoxin that bioaccumulates and bioconcentrates--primarily as monomethyl mercury--in aquatic food webs. It often reaches high levels in fish and other animals, making them unsafe for human consumption.

The source of monomethyl mercury in aquatic organisms has been debated, says Weiss, "but atmospheric deposition has been implicated as a pathway. Emissions such as coal combustion likely make a significant contribution."

That deposition affects all forms of precipitation: rain, snow and fog.

Weiss-Penzias and other researchers started their search by collecting fog samples by dark of night from June through August 2011.

They worked only in blackness so there would be no decomposition of mercury from sunlight, moving a single fog water collector among four locations near Santa Cruz: the roof of a UCSC building located in a redwood forest; a bluff at UCSC's Long Marine Laboratory; the Moss Landing Marine Labs' research vessel John H. Martin in Moss Landing Harbor; and on offshore spot in Monterey Bay where the John H. Martin was temporarily moored.

FogNet: a dragnet for mercury

The scientists then expanded their goals. Their NSF-funded project, called FogNet, involves sampling fog from seven locations along the California coast, from Eureka to Monterey.

FogNet is a collaborative effort among researchers at UCSC, Moss Landing Marine Labs, California State University-Monterey Bay, Humboldt State University Marine Laboratory, University of California-Davis Bodega Bay Marine Laboratory, San Francisco State University, Pepperwood Preserve and the U.S. Geological Survey.

The project will collect fog water during the summers of 2014 through 2016 for chemical characterization and quantification of fog deposition volume, Weiss-Penzias says.

The new data show elevated monomethyl mercury concentrations, similar to those the team revealed at the December AGU conference, as well as in a paper published in 2012 in the AGU journal Geophysical Research Letters.

"The hypothesis we're now testing," Weiss-Penzias says, "is whether a form of mercury called dimethyl mercury produced in the coastal ocean can be incorporated into cloud droplets, then be deposited in ecosystems on land and become an important, or even dominant, contributor to monomethyl mercury there."

Fog samples are being collected at Marina Airport, Long Marine Laboratory, UCSC, Montara Lighthouse, Bodega Bay, Pepperwood Preserve, and Humboldt State University Marine Laboratory.

Hidden in the mist

The average monomethyl mercury concentration in the fog water samples taken in 2011 was five-fold greater than the previously reported highest monomethyl mercury levels in rain water.

"There haven't been reports of monomethyl mercury measurements in fog water in the scientific literature," says Weiss. "But these elevated concentrations suggest that fog could be a significant source in coastal environments."

Could fog be a vector for not only mercury, but other toxic elements?

"We really don't know," says Weiss. "The potentially far-reaching consequences of these results, however, underscore the need to collect fog water in various locations along the coast."

Weiss-Penzias has teamed with UCSC biologist Chris Wilmers for one of the next steps in the research. Wilmers is providing hair and whisker samples from mountain lions that roam the oft-foggy Santa Cruz Mountains and Sierra Nevada foothills, where mercury was used in the Gold Rush era due to its ability to extract the precious metal from other materials.

Early results show that whiskers from coastal mountain lions contain mercury levels that are, on average, 10 times higher than those of their inland counterparts.

"We're looking at whether the mercury is linked with plants eaten by the mountain lions' main prey--deer," says Weiss-Penzias.

The scientist says he's constantly looking for mercury. When walks down his driveway to pick up the morning paper, he wonders what's in the dew.

"If my feet are wet when I get back in," he says, "I'm thinking: 'it was foggy enough last night to get a good sample.'"

---

<a href="http://www.nsf.gov" target="_blank" rel="noopener noreferrer">National Science Foundation</a>

Scientists Issue More Warnings Over Thawing Permafrost. As President Obama and high-level representatives of other nations converge in Anchorage, Alaska on August 30-31 for the Conference on Global Leadership in the Arctic: Cooperation, Innovation, Engagement and Resilience (GLACIER), hosted by the U.S. Department of State, top <a href="https://en.wikipedia.org/wiki/NASA">U.S</a>. climate scientists urge policymakers to address the critical problem of the thawing permafrost in the Arctic region.

Arctic permafrost - ground that has been frozen for many thousands of years - is now thawing because of global climate change, and the results could be disastrous and irreversible.

"The release of greenhouse gases resulting from thawing <a href="http://www.earth.com/image/arctic-ice-arch-remains-intact/">Arctic</a> permafrost could have catastrophic global consequences," said Dr. Max Holmes, a Senior Scientist at the Woods Hole Research Center (WHRC) who has been advising State Department officials on the problem.

Thawing permafrost releases greenhouse gases (carbon dioxide and methane) into the atmosphere, which accelerates climate change, which in turn causes more thawing of the permafrost. This potentially unstoppable and self-reinforcing cycle could constitute a calamitous "tipping point."

WHRC scientists have counseled the State Department on policies that could control this problem, including reducing global carbon emissions from fossil fuel use and deforestation, and limiting emissions of "black carbon," sooty particles that darken snow and ice and hasten Arctic warming.

"Despite the importance and urgency of this problem, until now it has received little attention from policymakers," said Dr. Sue Natali, another WHRC scientist. A study published earlier this year by Dr. Natali and WHRC scientists estimated that greenhouse gases released from thawing permafrost could make it much more difficult to meet the widely held goal of limiting global warming to 2 degrees Celsius.

"The United States must lead a large-scale effort to find the tipping point - at what level of warming will the cycle of warming and permafrost thawing become impossible to stop," said Dr. Holmes. "The real and imminent threat posed by permafrost thawing must be communicated clearly and broadly to the general public and the policy community."

The key science points, implications and recommendations can be found in the WHRC Policy Brief, "<a href="http://whrc.org/wp-content/uploads/2015/06/PB_Permafrost.pdf" target="_blank" rel="noopener noreferrer">Permafrost and Global Climate Change</a>."

---

<a href="http://www.whrc.org/" target="_blank" rel="noopener noreferrer">Woods Hole Research Institute</a>

New Zealand Stream

EPA Water Rules Take Effect Today New federal EPA water rules to protect smaller streams, tributaries and wetlands took effect on Friday - but only in some states.
A federal court ruling Thursday, hours before the rules were to go into effect, blocked the regulations in 13 states. Those states had sued the Environmental Protection Agency and the U.S. <a href="http://www.earth.com/news/armyworms-attack-crops/">Army</a> Corps of Engineers, arguing that the rules are federal overreach and could be costly and confusing for landowners. EPA Water Rules Take Effect Today
The government says the new rules will help protect the nation's waters from pollution and development, and safeguard drinking water for 117 million Americans.
Things to know about the new rules and court action blocking them:
---
EPA SAYS RULES ARE NEEDED
The regulations issued by the Environmental Protection Agency and the U.S. Army Corps of Engineers in May aim to clarify which smaller waterways fall under federal protection after two Supreme Court rulings left the reach of the Clean Water Act uncertain. Those decisions in 2001 and 2006 left 60 percent of the nation's streams and millions of acres of wetlands without clear federal protection, according to EPA, causing confusion for landowners and government officials.
The new rules would force a permitting process only if a business or landowner took steps that would pollute or destroy the affected waters - those with a "direct and significant" connection to larger bodies of water downstream that are already protected. For example, that could include tributaries that show evidence of flowing water.
---
STATES, FARMERS SAY THEY AREN'T
Despite the EPA's assurances, opponents fear a steady uptick in federal regulation of every stream and ditch on rural lands.
More than half of states have sued the EPA in hopes of delaying or blocking the rule. State officials from Georgia to New Mexico to Wisconsin have suggested the regulations could be harmful to farmers and landowners who might have to pay for extra permits or redesign their property to manage small bodies of water on their private land.
The federal ruling Thursday was in North Dakota, where officials from that state and 12 others argued the new guidelines are overly broad and infringe on their sovereignty. U.S. District Judge Ralph Erickson in Fargo agreed that they might have a case, issuing a temporary injunction.
The EPA said after the ruling that it would not implement the new rules in those 13 states - Alaska, Arizona, Arkansas, Colorado, Idaho, Missouri, Montana, Nebraska, Nevada, New Mexico, North Dakota, South Dakota and Wyoming.
Several other lawsuits remain, from other states and also from farm and business groups.
---
CONGRESS ALSO PUSHING BACK
In Congress, House Speaker John Boehner, R-Ohio, has called the rules "a raw and tyrannical power grab." The House has passed a bill that would block them - legislation the White House threatened to veto.
A Senate committee has passed a similar bill that would force the EPA to withdraw and rewrite the rules, and opponents are pushing the full Senate to act this fall.
The Senate bill has some bipartisan support. North Dakota Sen. Heidi Heitkamp and Indiana Sen. Joe Donnelly, both Democrats, have backed the legislation, saying the waters rule is a top issue they hear about from their agricultural constituents.
"It's the perfect example of the disconnect between Washington and rural areas," Donnelly said earlier this year.
---
EPA SAYS CRITICISM IS OVERBLOWN
Defending the rule in North Dakota, the government argued in court that the new rule clarifies some of the ambiguity in the law and actually makes it easier for the states to manage some waterways.
Government lawyers said during a hearing in Fargo last week that North Dakota's objection wrongly assumes some bodies of water will be affected. They also argued that the state is already going through some of the permitting procedures they're complaining about.
Since the rules were originally proposed last year, the EPA has been working to clear up some misconceptions, like some critics' assertions that average backyard puddles would be regulated. Farming practices currently exempted from the Clean Water Act - plowing, seeding and the movement of livestock, among other things - will continue to be exempted.
"We believe we have largely retained the status quo in terms of what a farmer would have to do under the current rule and the new rule," said Ken Kopocis, deputy assistant administrator of the EPA's Office of Water.
--
Associated Press writers James MacPherson in Bismarck, North Dakota and Dave Kolpack in Fargo, North Dakota contributed to this report.
---
Find Mary Clare Jalonick on Twitter: <a href="http://twitter.com/mcjalonick" target="_blank" rel="noopener noreferrer">http://twitter.com/mcjalonick</a> .
© 2015 The Associated Press. All rights reserved. This material may not be published, broadcast, rewritten or redistributed. Learn more about our Privacy Policy and Terms of Use.

EPA Water Rules Take Effect Today

EPA Water Rules Take Effect Today New federal EPA water...

Hawaii Waikiki Closure

Another Hawaii Beach Closed After Massive Sewage Spill. For the second time in a week a popular Hawaii beach closed Thursday after sewage from a treatment plant was discharged into the ocean.
A million gallons of treated but not yet disinfected wastewater was discharged from the East Honolulu Wastewater Treatment plant, closing Sandy Beach and its surroundings. The closure comes a day after beaches near Waikiki were reopened following a similar issue.
Hawaii American Water, the private company that runs the treatment plant, said the incident happened Tuesday after an underground electrical cable that feeds power to their chlorination system shorted out as heavy rains fell in the area. Another Hawaii Beach Closed After Massive Sewage Spill


[caption id="attachment_2384161" align="alignleft" width="150"]<a href="http://cff1.greenatom.net/uploads/2015/08/28101600/beach-closing-hawaii-wastewater_2big_ap.jpg"><img class="size-thumbnail wp-image-2384161" src="http://cff1.greenatom.net/uploads/2015/08/28101600/beach-closing-hawaii-wastewater_2big_ap-150x150.jpg" alt="Scott Muranka, of the Hawaii Department of Health" width="150" height="150" /></a> Scott Muranka, of the Hawaii Department of Health[/caption]
Lee Mansfield, manager of American Water, said in a telephone interview Thursday that there was un-disinfected water flowing into the ocean from their system for about five hours, resulting in about a million gallons of wastewater being discharged.
He said the water that flowed into the ocean had been treated through the plant, removing heavy debris and contaminants, but the water was not chlorinated before being discharged.
"We receive wastewater and we'll remove grit and large material, then we go through the primary sedimentation process, and that removes material that will readily settle out of the wastewater," Mansfield said. The water then goes through a biological treatment before being chlorinated, he said.
The state Department of Health released a statement advising the public to stay out of the waters from Halona Blow Hole to Erma's Beach on Oahu's southeast shore until further notice. Water samples were being taken for testing.
Another spill from Monday near Hickam Beach on Joint Base Pearl Harbor-Hickam was announced Thursday, prompting officials to tell the public to avoid those waters as well.
Officials said about 24,000 gallons spilled there, 12,000 of which went into a storm drain that leads into a canal near Hickam Beach. Water samples are being taken and the beach has posted with signs warning visitors of the potential dangers.
On Monday about 400,000 gallons of wastewater spilled in Ala Moana Beach Park after heavy rains associated with <a href="http://www.earth.com/image/tropical-storm-cristobal-over-the-yucatan-peninsula/">Tropical Storm</a> Kilo inundated the system. Officials opened the waters Wednesday afternoon after testing showed the water was safe.
Lori Kahikina, Honolulu's director of environmental services, said less sewage spilled than the half-million gallons the city initially reported.
She said Wednesday 129,000 gallons of wastewater flowed into the ocean. Another 264,000 spilled on land but never reached the ocean.
Officials said the Honolulu Zoo, which is in Waikiki, also flooded Monday, raising concern that untreated material from the zoo had entered the ocean.
A week of heavy rain had left the ground saturated, inundating the sewer systems with rain water. More rain was forecast for Thursday with flash flood watches in effect.
Meanwhile in the Pacific, Ignacio strengthened into a hurricane. The storm's maximum sustained winds increased Thursday morning to 90 mph (150 kph).
Hurricane Ignacio was centered about 1,135 miles (1,825 kilometers) east-southeast of Hilo, Hawaii, and was moving toward the state near 13 mph (20 kph). The storm could reach the islands by early next week.
---
Follow Caleb Jones on Twitter: <a href="https://twitter.com/CalebAP" target="_blank" rel="noopener noreferrer">https://twitter.com/CalebAP</a>
© 2015 The Associated Press. All rights reserved. This material may not be published, broadcast, rewritten or redistributed. Learn more about our Privacy Policy and Terms of Use.

Another Hawaii Beach Closed After Massive Sewage Spill

Another Hawaii Beach Closed After Massive Sewage Spill. For the...

Mauri Pelto digs his crampons into the steep icy slope on Mount Baker in Washington state and watches as streams of water cascade off the thick mass of bare, bluish ice. Every 20 yards, the water carves vertical channels in the face of the glacier as it rushes downstream.
What little snow from last winter is already gone, so ice is melting off the glacier at a rate of nearly three inches a day this summer, he said.
"At the rate it's losing mass, it won't make it 50 years," said Pelto, a glaciologist who returned this month for the 32nd year to study glaciers in the North Cascades range. "This is a dying glacier," he said.
Glaciers on Mount Baker and other mountains in the North Cascades are thinning and retreating. Seven have disappeared over the past three decades, and the overall volume of glaciers in the range have lost about one-fifth of their volume.
The shrinking glaciers here mirror what is happening around the U.S. and worldwide: As the planet warms, glaciers are losing volume, some faster than others.
Two of the largest glaciers in Yosemite National Park in California have retreated over the past century, losing about two-thirds of their surface areas. In Alaska, a recent study of 116 glaciers estimated they have lost about 75 billion metric tons of ice every year from 1994 to 2013. In Montana, scientists are already seeing the impacts in increased stream temperature and changes to high-elevation ecosystems. In 1850, there were 150 glaciers at Glacier National Park; now there are 25.
"These glaciers are, from a geological standpoint, rapidly disappearing from the landscape," said Dan Fagre, a research ecologist with U.S. Geological Survey stationed in Glacier National Park. "They're so small and vulnerable that they could be gone in a matter of decades."
Glaciers -thick masses of accumulated snow that compress into ice and move - are important indicators of climate change because they are driven by precipitation and temperature.
The glaciers on Mount Baker, a volcanic peak about 125 miles northwest of Seattle, provide a critical water source for agriculture, cities and tribes during the late summer. The icy glacial melt keeps streams cool for fish and replenishes rivers during a time of year when they typically run low.
For the Nooksack Indian Tribe, which has relied for hundreds of years on salmon runs in the glacier-fed Nooksack River, a way of life is at risk. Without that glacial runoff, rivers will dry up more quickly and warm up faster, making it harder for salmon to spawn or migrate to the ocean.
"Climate change will impact the ability of tribal members to harvest fish in the future," said Oliver Grah, water resources manager for the tribe, which has teamed up with Pelto. They want to know how glacier runoff will affect the river's hydrology and ultimately fish habitat and restoration planning.
On a recent day in August, Grah and colleague Jezra Beaulieu hiked 5 miles into the Sholes Glacier to study how climate change will influence the timing and magnitude of stream flow in the river. It's their fifth field trip to the glacier this summer, and each time they're amazed at how rapidly the snow and ice are melting.
Grah strings a measuring tape across the stream, wades in shin-deep in the fast-moving, brownish water and measures the depth of the water streaming from the toe of the glacier. He calls out numbers that Beaulieu records in a yellow notebook. They're trying to calculate how much flow and sediment is coming from the glacier.
"This is a frozen reservoir that yields water all summer long," said Pelto, a professor of environmental sciences at Nichols College in Dudley, Massachusetts. "So you take this away and what are you going to replace it with?"
The tribe also is collaborating with Western Washington University, which is using data collected in the field to model what the streamflow will be like in the future.
"The late summer flows controlled by melting glaciers are predicted to decrease as the glaciers get smaller and smaller," said Robert Mitchell, a geology professor at Western Washington University.
This year, a record low snowpack in Washington state and warmer temperatures have made it one of the worst Pelto has seen in over three decades.
"They're losing volume at a faster rate than ever before," Pelto said. "If you can't sustain a glacier at a place like this in the Lower 48 states, there's no hope."
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Scientists Voice Concerns Over Rapidly Shrinking Glaciers On Mount Baker

Mauri Pelto digs his crampons into the steep icy slope...

Arctic OffShore Drilling

Shell Pauses Arctic Ocean Oil Drilling Strong winds and high waves that pounded the northern coast of Alaska have led Royal Dutch Shell PLC to temporarily stop exploratory <a href="https://www.bing.com/search?q=arctic+ocean&amp;FORM=EDGENA&amp;PC=HCTS&amp;refig=06f30f4e602a4654d276cea6f9598ffb">Arctic</a> Ocean oil drilling.
"Due to high wind and sea states, we have paused all critical operations in the Chukchi Sea," said spokesman Curtis Smith in an email response to questions.
The eastern Chukchi Sea this week experienced gale-force winds in the range of 39 to 54 p.m., said Ed Townsend, lead forecaster for the National Weather Service in Fairbanks. Winds at Point Lay on Alaska's northwest coast about 9 a.m. Friday blew steadily at 29 mph with gusts to 37 mph.Shell Pauses Arctic Ocean Oil Drilling
Smith said he isn't sure when drilling might resume. "We hope to resume normal operations as soon as it's safe to do so," he said.
The Polar Pioneer, a semi-submersible drilling unit that Shell leases from Transocean Ltd., began top-hole and drilling work July 30 and remains safely anchored at the drill site, Smith said.
Bad weather has postponed previous drilling operations, Smith said, and Shell plans for it. Bad weather affected drilling in both the Chukchi and Beaufort seas in 2012.
"It's why we use a combination of satellite images, sonar and on-site reconnaissance to inform our operations," he said. "With safety the first priority, we take a conservative approach to these weather events and make plans to curtail operations well in advance."
Arctic offshore drilling is strongly opposed by environmental groups that say oil companies have not demonstrated the ability to respond effectively to a spill in harsh conditions where floating ice could hamper cleanup operations.
"Imagine trying to respond to a spill in that kind of weather," said Pam Miller, a longtime Arctic researcher and environmental advocate in Fairbanks.
Halting drilling for severe weather or moving ice was a common occurrence for Shell drilling in 1989 and 1990, she said. Global warming's effect on sea ice, which formerly acted like a blanket over waves, adds to the risk.
"The waves may be even greater. We know they are along shore, where coastal erosion is a problem," she said.
Every time a drill rigs disconnects from a well for weather or ice moving in, she said, it adds to the risk of a spill.
The weather is also affecting operations on shore. Shell is temporarily relocating staff at its housing camp in Barrow, the northernmost city in the United States. "A road used to transport people to the camp is down to one lane due to high water and could become impassable," Smith said.
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Shell Pauses Arctic Ocean Oil Drilling

Shell Pauses Arctic Ocean Oil Drilling Strong winds and high...

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 the <a href="https://www.esa.int/">European Space Agency</a> features Nushagak Bay, a large estuary in southwest Alaska. Nushagak runs mainly north to south and exits in Bristol Bay, a large body of water in the Bering Sea.



"The bay is primarily fed by the Nushagak River, which begins in the Alaska Range and flows southwest approximately 450 km. The bay is also fed by several additional rivers including the Wood, Igushik, Snake and Weary rivers," says ESA.



"The dark colors of the Nushagak River are most likely due to tannins or lignins (chemical substances found in plants). Tannins and lignins from roots, leaves, seeds, bark and soil can leach into the water and give it a brown or even black colour. The sediments then flow southwards where it is mixed with the bluer waters of the bay."



Video/ Image 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

Nushagak Bay in southwest Alaska

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Today's Video of the Day from the <a href="https://www.acs.org/">American Chemical Society</a> (ACS) reveals that proteins on flu viruses are actually flexible, tilting and waving in a “breath-like” motion. According to the experts, these proteins could be used to better defend against the flu.



"The main antigenic targets of influenza virus are two surface glycoproteins, hemagglutinin (HA) and neuraminidase (NA). Whereas the structural and dynamical properties of both glycoproteins have been studied previously, the understanding of their plasticity in the whole-virion context is fragmented," wrote the researchers.



To investigate, the team conducted detailed simulations of the influenza A H1N1 virion, or the swine flu. The experts concluded that the visualizations show many new vulnerable states of flu viruses, which could improve future vaccines and antiviral drugs.



Video/ Image 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



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Flu viruses are more flexible than expected

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Today’s Video of the Day from the <a href="https://www.esa.int/">European Space Agency</a> features Lake Trasimeno, which is located west of Perugia in central Italy. It is the fourth largest lake in the country. While Trasimeno’s water level varies, it has a maximum depth of approximately six meters.&nbsp;



"In this Copernicus Sentinel-2 image, captured on 6 August 2022, the lake’s emerald green colour is likely due to the presence of phytoplankton. Streaks in the water, particularly visible in the west, indicate the presence of soil and sediments which have been stirred up by winds. Dark colored waters in the southern part of the lake indicate a presence of submerged and floating macrophytes (aquatic plants) as well as algae," says ESA.



"Surrounded by hills on three sides, Trasimeno is subject to heavy storms created by winds, especially from the north and west. There are three islets in the lake: Maggiore, Minore and Polvese (the largest). The lake’s shores are sparsely inhabited with only two popular villages: Castiglione del Lago and Passignano sul Trasimeno."



"Italy is experiencing its worst drought in 70 years which has affected drinking water supplies, hydroelectric power and agricultural production. High temperatures, hot winds and lack of rainfall are the main causes of drought in the Umbrian region which saw Lake Trasimeno’s drop 1.3 m, reaching the limit of the hydrometric zero in July 2022."



Video/Image Credit: ESA&nbsp;



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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

Lake Trasimeno in Central Italy

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Today's Video of the Day from the <a href="https://www.acs.org/">American Chemical Society</a> describes a new self-powered nanosensor that can instantly detect mercury contamination with the tap of a finger.&nbsp;



The oxidized form of mercury can be harmful when it is ingested through contaminated water or food. This makes it necessary for experts to develop sensors that can quickly and accurately detect the presence of mercury.&nbsp;



Zong-Hong Lin and colleagues have now created a triboelectric nanosensor (TENS) that can detect mercury by simply by touching a sample. According to the researchers, their TENS could serve as the basis for similar devices to safely and remotely monitor other pollutants.



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



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Detecting mercury contamination with the tap of a finger

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Today’s Video of the Day from the <a href="https://www.esa.int/">European Space Agency</a> features Kainji Lake, a reservoir on the Niger River.



In 1968, Kainji Lake was created by the construction of the Kainji Dam. The Niger River, the third longest in Africa, enters the lake in the north.&nbsp;



According to <a href="https://www.earth.com/news/rivers-in-the-american-west-are-a-lifesaving-resource-for-birds/">ESA</a>, the creation of the lake submerged Foge Island and the town of Bussa and permanently flooded other riverine settlements, leaving around 50,000 people displaced.&nbsp;



Large parts of Foge Island are temporarily exposed during low water tides, and the land is often used by migrating fishermen. Kainji Dam is a dam across the Niger River in Niger State of Central Nigeria. 



Wild mammals occur at relatively low densities due to illegal hunting. Lake Kainji has suffered a dramatic decline as a fishery due to the high numbers of artisanal and subsistence fisherfolk using the lake. It has been suggested that a period of closure, together with controlled fishing rights may help improve fish stocks.



Kainji Lake National Park is the oldest of its kind in Nigeria. The park contains three distinct areas: a part of the Kainji Lake, the Borgu Game Reserve to the west of the lake, and the Zugurma Game Reserve to the southeast. The park is home to around 65 mammal species, 350 bird species, and 30 species of reptiles and amphibians. 



Video/ Image Credit: European Space Agency&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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Kainji Lake in north central Nigeria

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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



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.

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 the <a href="https://www.acs.org/">American Chemical Society</a> explores the ability of salt to transform the way that foods and beverages taste. Salt is known to cover up undesirable flavors, such as bitterness in coffee or beer, but how exactly does sodium chloride change the taste of other compounds?



One previous study showed that, not only does salt suppress bitterness, but also enhances sweetness and sourness. Another study revealed that bitterness reduction by salt seems to be happening at the tongue receptor level as well as in the brain.&nbsp;



While it is known that salt taste is mediated by the presence of sodium channels in the form of taste buds, experts believe that there is also an unknown receptor responsible for how we taste salt that has not yet been identified.&nbsp;



Video Credit: ACS Reactions



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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.

How does salt makes things taste better?

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Today’s Video of the Day from the <a href="https://www.esa.int/">European Space Agency</a> features Santiago, the capital city of Chile. The city is located in the center of the Santiago Metropolitan Region, which has a population of about eight million people.&nbsp;



'The weather of Santiago resembles the Mediterranean climate with dry and warm summers with temperatures reaching up to 35°C (from October to March) and cool and humid winters that can drop to 0°C (from April to September)."



"The city lies in the centre of the country’s central valley around 80 km from the Pacific Ocean to the west and borders Argentina to the east. A tiny part of Argentina is visible in the top-right corner of the image where the mountain crest of the Andes Mountains acts as a divider between the two countries," says ESA.



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



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Santiago, Chile in South America

[sendtonews key="JRaP49ISmm-2357509-12187" type="single"] Today’s Video of the Day from the...

Spiral,Galaxy,,Illustration,Of,Milky,Way

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Astronomers at <a href="https://www.jhu.edu/">Johns Hopkins University</a> have created an interactive map of the universe, including the actual position and real colors of 200,000 galaxies. The map allows the public to access data that was previously only available to scientists.



The map was developed using data collected by the Sloan Digital Sky Survey. For over two decades, a telescope in New Mexico was aimed at slightly different locations to capture the night sky.&nbsp;



"Growing up I was very inspired by astronomy pictures, stars, nebulae and galaxies, and now it's our time to create a new type of picture to inspire people," said map creator Brice Ménard, a professor at Johns Hopkins. "Astrophysicists around the world have been analyzing this data for years, leading to thousands of scientific papers and discoveries. But nobody took the time to create a map that is beautiful, scientifically accurate, and accessible to people who are not scientists. Our goal here is to show everybody what the universe really looks like."



"In this map, we are just a speck at the very bottom, just one pixel. And when I say we, I mean our galaxy, the Milky Way which has billions of stars and planets. We are used to seeing astronomical pictures showing one galaxy here, one galaxy there or perhaps a group of galaxies. But what this map shows is a very, very different scale."



"From this speck at the bottom, we are able to map out galaxies across the entire universe, and that says something about the power of science."



The <a href="https://mapoftheuniverse.net/">interactive map</a> is available online, where it can be downloaded for free.



Video Credit: Johns Hopkins&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.

Interactive map of the universe includes 200,000 galaxies

[sendtonews key="e4ZG0Jawp3-2374785-12187" type="single"] Astronomers at Johns Hopkins University have created...

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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



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.

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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Today's Video of the Day from the <a href="https://www.esa.int/">European Space Agency</a> features Dublin, the capital and largest city of Ireland. Beyond its pub culture, Dublin is known as a modern culinary destination and a UNESCO City of Literature.



"Dublin is located near the midpoint of Ireland’s east coast in the province of Leinster. The city, which covers an area of around 115 square kilometers, is bordered by the Dublin Mountains, a low mountain range to the south, and is surrounded by flat farmland to the north and west," says ESA.



"The city straddles the River Liffey, which rises in the Wicklow Mountains and flows around 80 kilometers eastwards through the city of Dublin, in which it is canalised and bordered with quays. It then empties into Dublin Bay, an arm of the Irish Sea."



Dublin has an abundance of green spaces, including one of the largest enclosed public parks in any European capital city. Phoenix Park, which was originally formed as a royal hunting park in the 1660s, includes 707 hectares of green space.



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.

The city of Dublin on Ireland's east coast

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Today's Video of the Day from the <a href="https://www.esa.int/">European Space Agency</a> features the province of Zaragoza in northeast Spain. The image was captured by the Copernicus Sentinel-2 mission.



"Together with the provinces of Huesca and Teruel, Zaragoza formed the old kingdom of Aragon. Its capital, also called Zaragoza (not visible in this image) is home to around half of Aragon’s population," says ESA.



"The Ebro River can be seen winding its way through the province from west to east in this image. Between its source in the Cantabrian Mountains in the northwest and its delta on the Mediterranean coast, the Ebro River is fed by more than 200 tributaries as it flows 910 km across much of northern Spain."



Since rainfall is very scarce in this region, irrigation in the Ebro basin is critically important. In the valleys surrounding the Ebro River, many fields are used for growing crops such as corn, wheat, and barley.



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.

The province of Zaragoza in northeast Spain

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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



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.

Wetlands are a major source of methane emissions

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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



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.

The rapid retreat of the Columbia Glacier

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Today’s Video of the Day from the <a href="https://www.esa.int/">European Space Agency</a> features the Pyrenees Mountains, which form a natural boundary between France and Spain in southwest Europe.



The mountain range is 430 kilometers in length. It stretches from the Mediterranean Sea on the east to the Atlantic Ocean on the west.



At an elevation of 3404 meters, Pico de Aneto is the highest mountain peak in the Pyrenees, and the third-highest peak in Spain. Pico de Aneto is located in the Posets-Maladeta Natural Park, which spans more than 82,000 acres.&nbsp;



"Geological studies have revealed that the Pyrenees Mountains have been around for longer than the Alps, with their sediments first deposited in coastal basins during the Paleozoic and Mesozoic eras," reports ESA.



"The entire mountain range formed due to the upwelling of large sedimentary rocks by the collision of the Iberian and the Eurasian plate around 100 to 150 million years ago, followed by intense erosion from ice and water."



The western Pyrenees receive more precipitation due to moisture blowing in from the Atlantic Ocean. The mountain range contains many lakes, several small glaciers, and some of the highest waterfalls in Europe.



Video &amp; 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.

The Pyrenees Mountains in southwest Europe

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Today’s Video of the Day from <a href="https://www.stowers.org/">Stowers Institute for Medical Research</a> describes why experts are studying zebrafish to gain a better understanding of how the immune system responds to injury. Zebrafish have the ability to repair and regenerate organs.



“Organ regeneration offers an exciting opportunity for studying the immune system and to inquire why some species can regenerate organs like the heart or missing limbs while others like humans cannot,” explained Dr. Tatjana Piotrowski.



Zebrafish sensory organ hair cells are an ideal system to investigate the pathways and cell types involved in regeneration since they are easily destroyed with antibiotics and begin regenerating within five hours. This enabled the researchers to identify the exact timing and genetic programs for each anti-inflammatory macrophage activation state.&nbsp;



“Our hypothesis is that human macrophages do not receive the proper chemical activation 'cocktail' to instruct pro-regenerative processes,” said Dr. Nicolas Denans. “Identifying the molecular recipe of macrophage activation in zebrafish may one day enable us to design regenerative immunotherapies in humans.”&nbsp;&nbsp;&nbsp;



“The new evidence is a valuable resource for comparative studies on the genetic programs involved in macrophage-mediated repair and regeneration. In other words, different types of injuries may induce different kinds of inflammatory responses. We want to decipher whether this 'language' is universal or if there are a variety of dialects."



Video Credit: Stowers Institute for Medical Research&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.

How the immune system responds to injury

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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



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.

2022 illustrated the consequences of a warming climate

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

Earth,Like,Exoplanet,3d,Render

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Today's Video of the Day from <a href="https://www.nasa.gov/goddard">NASA Goddard</a> describes two exoplanets that are orbiting a star 218 light-years away. A team of researchers led by the University of Montreal has found evidence that these planets are "water worlds."



The experts used data from NASA’s Hubble and Spitzer Space Telescopes. They discovered that exoplanets Kepler-138 c and Kepler-138 could be composed largely of water.



"We previously thought that planets that were a bit larger than Earth were big balls of metal and rock, like scaled-up versions of Earth, and that's why we called them super-Earths," explained study co-author Björn Benneke.&nbsp;



"However, we have now shown that these two planets, Kepler-138 c and d, are quite different in nature and that a big fraction of their entire volume is likely composed of water. It is the best evidence yet for water worlds, a type of planet that was theorized by astronomers to exist for a long time."



Video Credit: NASA Goddard



Image Credit: NASA, ESA, and Leah Hustak (STScI)



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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.

Two distant planets may be "water worlds"

[sendtonews key="QIoVYJqRBi-2434608-12187" 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



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.

Satellites reveal how Earth's systems are interconnected

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

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