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



During the <a href="https://www.earth.com/news/humans-were-likely-the-leading-cause-of-megafauna-extinctions/" target="_blank" rel="noreferrer noopener">Pleistocene</a> - the geologic chapter that began about 2.7 million years ago and ran through innumerable swings between cold and mild - the island’s ice waxed and waned in tune with global climate. 



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



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



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



That sliver of soil, shielded for ages by roughly 1.9 miles (3 km) of ice, now refocuses the conversation about future sea level and the stability of polar ice in a warming world.



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



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



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



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



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



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



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



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



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



High‑energy isotope ratios show that the summit last saw open air within the past 1.1 million years, while argon trapped in overlying clear ice indicates at least 250,000 years of continuous cover since then. Basal ice at another drilling site about 19 miles away is roughly 1 million years old. 



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



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



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



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



“It was amazing,” Mastro exclaimed. 



<figure class="wp-block-image aligncenter size-full"><a href="https://www.earth.com/wp-content/uploads/2025/04/greenland_soil-sample_fossils_recently-melted-ice_credit-UVermont_1m.jpg" target="_blank" rel="noreferrer noopener"><img src="https://www.earth.com/wp-content/uploads/2025/04/greenland_soil-sample_fossils_recently-melted-ice_credit-UVermont_1s.webp" alt="Willow bud scale, arctic poppy seed, fungal bodies, and rock spikemoss megaspores found in the GISP2 soil sample viewed under a microscope at the University of Vermont. Credit: Halley Mastro/University of Vermont" class="wp-image-1966471"/></a><figcaption class="wp-element-caption">Willow bud scale, arctic poppy seed, fungal bodies, and rock spikemoss megaspores found in the GISP2 soil sample viewed under a microscope at the University of Vermont. Click image to enlarge. Credit: Halley Mastro/University of Vermont</figcaption></figure>



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



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



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



Sea level today is rising more than an inch each decade. “And it's getting faster and faster,” said&nbsp;Bierman. The extra water comes from a warming ocean that expands as well as from melting glaciers worldwide.



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



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



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



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



Richard Alley, a leading climate scientist at Penn State, reviewed the new research.



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



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



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



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



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



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

Greenland’s ice-covered landscape looks like an immovable block on satellite maps. Yet the story locked beneath its center suggests a very different past, one that places future coastal cities in a tight spot. During the Pleistocene - the geologic chapter that began about 2.7 million years ago and ran through innumerable swings between cold and mild - the island’s ice waxed and waned in tune with global climate. New evidence hints that those swings were more dramatic than scientists once believed. In 1993, drillers hauled a two‑mile‑deep ice core up...

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The environmental impacts of crime. Recent research by the University of Surrey's <a href="http://www.surrey.ac.uk/ces/" target="_blank" rel="noopener">Centre for Environmental Strategy</a> has found that despite policy makers currently examining the economic and social impacts of crime, the environmental impacts have not, to date, been included.

The study, published in the Journal of Industrial Ecology, estimates the carbon footprint of crime. It was conducted by a UK-based research team led by an engineering doctorate student, Helen Skudder, in the Centre for Environmental Strategy at the University of Surrey. The environmental impacts of crime

The authors use a complex method of quantification--applying carbon emissions factors to the monetized costs of crime using environmentally-extended input-output analysis. This allowed them to estimate the carbon footprint of crime committed in <a href="https://www.earth.com/news/human-footprints-oldest-england/">England</a> and Wales in 2011. They found it to be over 4 million metric tonne s CO2e, equivalent to the carbon emissions of around 900,000 UK homes.

Of the offence types considered, burglary resulted in the largest proportion of the total footprint (30%) due to large volume of offences and the carbon associated with replacing stolen or damaged goods. Criminal justice system services (policing, prisons and courts) also accounted for a large proportion of the total footprint (21% of all crime and 49% of police recorded offences).

The limitations to the findings are particularly interesting and predominantly result from the footprinting methodology. Although it is tempting to conclude from the research that crime reduction will automatically result in a reduction of carbon emissions, this is not necessarily the case, due to the rebound effect. That is, the study considered how money currently spent addressing crime might be spent in the absence of crime. By comparing the carbon emissions associated with this re-spending of the money with the carbon footprint of crime, it was found that the most likely rebound effect would be an increase in emissions of around 2%.

Author Helen Skudder, of the University of Surrey, said "Although there are limitations to the methodology, we've highlighted some interesting findings, such as the large proportion of the footprint which arises due to burglaries. Looking at burglary in more detail, we find that emissions not only arise from policing and the criminal justice system response to crime, but also that the carbon arising due to replacement of stolen items is significant. The analysis illustrates the complex ways that institutions in society and the associated economic activity shape the impact we have on our climate. We have shown that it is possible to take into account the environmental implications of crime alongside the social and economic costs, as part of crime prevention policy appraisals".
###
The article, "Addressing the Carbon-Crime Blind Spot: A Carbon Footprint Approach" is freely downloadable <a href="http://onlinelibrary.wiley.com/doi/10.1111/jiec.12457/epdf" target="_blank" rel="noopener">here</a>.

Media enquiries: Ashley Lovell, Media Relations Office at the University of Surrey, Tel: 01483 686141 or E-mail: <a href="mailto:a.lovell@surrey.ac.uk">a.lovell@surrey.ac.uk</a>

Notes to Editors:

About the University of Surrey

The University of Surrey is one of the UK's leading professional, scientific and technological universities with a world-class research profile and a reputation for excellence in teaching. Ground-breaking research at the University is bringing direct benefit to all spheres of life - helping industry to maintain its competitive edge and creating improvements in the areas of health, medicine, space science, the environment, communications, defence and social policy. Programmes in science and technology have gained widespread recognition and it also boasts flourishing programmes in dance and music, social sciences, management and languages and law.

In addition to the campus on 150 hectares just outside Guildford, Surrey, the University also owns and runs the Surrey Research Park, which provides facilities for 110 companies employing 2,750 staff.

The University of Surrey was named University of the Year by the Times and Sunday Times, both overall and for 'Student Experience', and achieved a top-five ranking in the Guardian University Guide 2017.

For more information about the University and its work, visit <a href="http://www.surrey.ac.uk/" target="_blank" rel="noopener">http://www.surrey.ac.uk</a>

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The environmental impacts of crime

The environmental impacts of crime. Recent research by the University...

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Typhoon Nepartak dropped almost 20 inches of rain. Typhoon Nepartak was a powerful category four tropical typhoon when it hit Taiwan last week but weakened to a tropical storm as it moved into the Taiwan Strait. NASA calculated the heavy rainfall the typhoon brought to Taiwan and <a href="https://www.earth.com/image/historic-flooding-has-killed-hundreds-across-china/">China</a> before it dissipated over southeastern China.

Nepartak's winds and heavy rains caused severe problems when it moved ashore over southeastern China. Thousands of homes in China were destroyed by the storm. At least three deaths in Taiwan and six fatalities in China were attributed to Nepartak. Torrential rain caused flash flooding and mudslides in both Taiwan and China. Typhoon Nepartak dropped almost 20 inches of rain

<a href="https://www.bing.com/search?q=nasa&amp;cvid=7483842c389943f5b116a82e2e9bc57f&amp;FORM=ANAB01&amp;PC=HCTS">NASA's</a> Integrated Multi-satellitE Retrievals for the Global Precipitation Measurement or GPM mission (IMERG) were used to estimate the total amount of rain that Nepartak dropped over Taiwan and southeastern China. Totals were estimated during the period from July 3 through July 10, 2016 when the typhoon moved through the western Pacific. IMERG estimates indicated that the typhoon dropped over 500 mm (19.7 inches) in some areas. Even greater rainfall totals were calculated in areas of China and southern Japan that were not directly affected by typhoon Nepartak.


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Typhoon Nepartak dropped almost 20 inches of rain

Typhoon Nepartak dropped almost 20 inches of rain. Typhoon Nepartak...

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Gas causing ground to rise near Mount Vesuvius volcano. New work by <a href="http://www.earth.com/news/virus-killing-dolphins/">Italian</a> geochemists seems to indicate that the current ground movement around one of the world's most dangerous volcano systems may be due to gas pressure, and not because of a surge of volcanic magma. This work was recently presented at the Goldschmidt conference in Yokohama, Japan (30 June 2016).

The Campi Flegrei (Phlegraean Fields), just across the Bay of Naples from the famous Vesuvius volcano, is amongst the most dangerous volcanos on <a href="https://www.bing.com/search?q=earth+wiki&amp;form=EDGEAR&amp;qs=HS&amp;cvid=197419b1fd0e4faab09bac8a8c043c41&amp;cc=US&amp;setlang=en-US&amp;elv=AY3%21uAY7tbNNZGZ2yiGNjfNqIbOEKEZbuUqFXmqcpemEfleM0HF8bdm1Pd6C0xc49T3*BQd5YYqegbJpmu*JbdftEw98VI*hZAfiFFzcD9lI&amp;plvar=0&amp;PC=HCTS">Earth</a>. In the past it has been capable of a "VEI 7" eruption (Volcanic Explosivity Index of 7, meaning that it has produced an explosive eruption even bigger than the famous Krakatoa eruption of 1883). However, this was around 40,000 years ago. The last eruption, "VEI 2" occurred in 1538 AD.

Because of the geological instability in the area, the land in this area can rise and fall by several metres over just a few years, a phenomenon known as Bradyseism. The last few years have seen the ground in the area begin to rise again, with a 38 cm rise recorded since late 2005*. There have been worries that this may presage an eruption.

The last serious geological unrest in the area was in 1982-84, which saw ground levels rise by up to 1.8m. Most scientists think that the movement in this period was caused by mixed magmatic- hydrothermal activity (although some recent papers in the geochemical literature have suggested a major role for hydrothermal processes supported by deep magmatic gases, with pressurised water causing the land to rise). On the other hand, consensus exists that the current activity is caused by molten magma movement and accumulation under the Campi - which carries a greater risk of an eruption. Now however, a group of Geochemists from Second University of Naples and the Vesuvius Observatory think that the consensus has got it exactly the wrong way round.

Lead researcher, Professor Roberto Moretti (Seconda Università degli Studi di Napoli) commented:

"Everyone accepts the geochemical evidence that current activity has different causes to that of 1982-84. Most geochemists are now showing that the 1982-84 movement was caused by hydrothermal activity and the current activity is caused by magma, but we think that it's exactly the other way round. We have checked geochemical records going back over more than 30 years, and our ongoing interpretation - looking at released gases and physical signals - seem to be consistent with current activity being hydrothermal, with the support of deep magmatic gases, rather than due to magma migration or growth of a shallow (3-4 km deep) magma chamber. We believe that this magma dynamics characterized the 1982-84 episode.Gas causing ground to rise near Mount Vesuvius volcano

This is apparently better news, at least for now; activity in which magma moves upward and accumulates tends to be associated with an increased chance of an eruption. However the change from hydrothermal to magmatic activity can take place at any time, so we're not in a position to say that everything is well under the Campi Flegrei. The Campi Flegrei is still a very volatile place. What it does show is the difficulty in interpreting the data, even from one of the most-studied volcanic areas in the world. Reconciling all of the data is a major issue, despite our efforts.

Achieving such a unique and consistent interpretation would probably require direct access to underground geochemical, geophysical and geochemical information in the areas of interest. However, there is still a debate over the safety of drilling in such a volatile area".

Commenting, Professor Jon Blundy (University of Bristol) said:

"Interpreting the causes of ground movement at restless volcanoes is an enduring problem for volcanologists. Both hot gases (steam) and magma are candidate causes, but with quite different implications for future eruptive activity. Moretti and others make a compelling case for gas, rather than magma, as the cause of the latest bradyseisms at Campi Flegrei. Their methods could be used at other restless volcanoes where there is evidence of ground uplift"


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Gas causing ground to rise near Mount Vesuvius volcano

Gas causing ground to rise near Mount Vesuvius volcano. New...

Carbon Dioxide

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New method to store carbon dioxide deep underground. Scientists have found an inexpensive way to monitor the storage of the most common greenhouse gas - carbon dioxide - deep underground.

Successful trials of their method at a site in Australia will inform the development of <a href="http://www.earth.com/video/carbon-is-the-basis-for-all-life-on-our-planet/">Carbon</a> Capture and Storage (CCS) technology, in which CO2 from power stations and industrial sources is held deep underground, to prevent emissions from contributing to climate change.

In the first experiment of its kind, researchers studied the different forms of oxygen in waters sampled from rocks deep below ground at the storage site in the Otway Basin, in south eastern <a href="https://www.bing.com/search?q=australia&amp;form=EDGEAR&amp;qs=PF&amp;cvid=fb6c1e791558406ca3ef6d925796e2a3&amp;cc=US&amp;setlang=en-US&amp;elv=AY3%21uAY7tbNNZGZ2yiGNjfNqIbOEKEZbuUqFXmqcpemE8HmDlKQIjBSv1FYbv4LOfm2z499WfxHyqGGAQRik9r%21EcBfh9YuFwS39zsw5PYAF&amp;plvar=0&amp;PC=HCTS">Australia</a>.

They found that the reservoir's waters changed their oxygen composition when in contact with bubbles of trapped CO2. Testing samples of water for this altered form of oxygen provides a simple way to measure the amount of CO2 stored within the rock.

The study shows that injected CO2 is very quickly retained in the underground rocks, with CO2 being locked away like air being trapped within a foam sponge. The research was carried out by the Universities of Edinburgh and Australian research organisation CO2CRC.

Researchers say their technique provides an inexpensive monitoring solution, as they need only measure only CO2 injected into a site and water samples from before and after injection to find out how much CO2 is trapped.

The study, published in the International Journal of Greenhouse Gas Control, was supported by the UK Carbon Capture and Storage Research Centre and CO2CRC.

Dr Sascha Serno, of the University of Edinburgh's School of GeoSciences, who led the study, said: "Our results highlight the promising potential of using oxygen compositions to monitor the fate of CO2 injected underground. This method is simple and cheap, and can be easily combined with other monitoring techniques for CCS projects in the UK and beyond."

Dr Stuart Gilfillan, also of the School of GeoSciences, the study co-ordinator, said: "Understanding the fate of CO2 injected into the underground for storage is essential for engineering secure CO2 stores. Our work with our Australian partners paves the way for better understanding of the fate of CO2 when we inject it underground."


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New method to store carbon dioxide deep underground

New method to store carbon dioxide deep underground. Scientists have...

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Hurricane Celia is seen headed for the Central Pacific Ocean. The Suomi NPP and Aqua satellites captured visible and infrared data on Hurricane Celia as it continues to head west toward the Central <a href="http://www.earth.com/news/dust-asia-fertilizes-north-pacific/">Pacific Ocean</a>.

Hurricane Celia is currently in the Eastern Pacific Ocean, but once it passes west of 140 degrees west longitude, warnings on the system will be issued by NOAA's Central Pacific Hurricane Center.

On July 11 at 22:05 UTC (6:05 p.m. EDT) the Visible Infrared Imaging Radiometer Suite (VIIRS) instrument aboard NASA-NOAA-DOD's Suomi NPP satellite captured a visible light image of Hurricane Celia that showed a cloud-filled eye with powerful bands of thunderstorms wrapping around the low level center. The VIIRS image also showed a large band of thunderstorms that extended to the south, wrapping into the storms' eastern quadrant.Hurricane Celia is seen headed for the Central Pacific Ocean

On July 11 at 21:29 UTC (5:29 p.m. EDT) the Atmospheric Infrared Sounder or AIRS instrument aboard NASA's Aqua satellite captured infrared data of Celia's cloud top temperatures. The data was made into a false-colored image that showed the coldest, strongest, highest thunderstorm cloud tops in purple wrapping around the center. The color indicated that those thunderstorm tops were as cold as minus 63 Fahrenheit (minus 53 Celsius). <a href="https://en.wikipedia.org/wiki/NASA">NASA</a> research has shown that storms that high in the atmosphere have the ability to generate heavy rain.

At 5 a.m. EDT (0900 UTC) on July 12 the center of Hurricane Celia was located near 16.2 north latitude and 127.9 west longitude. That's about 1,260 miles (2,025 km) west-southwest of the southern tip of Baja California, Mexico. It was moving to the west-northwest at 10 mph (17 kph) and NOAA's National Hurricane Center (NHC) expects Celia to turn toward the northwest later today, with this motion continuing Tuesday night and Wednesday. Maximum sustained winds were near 100 mph (155 kph).

NHC forecasts weakening over the next two days and Celia could weaken to a tropical storm on Wednesday.


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Hurricane Celia is seen headed for the Central Pacific Ocean

Hurricane Celia is seen headed for the Central Pacific Ocean....

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Ice algae: The engine of life in the central Arctic Ocean. Ice algae play a much greater role for the Arctic food web than previously assumed. In a new study, biologists of the Alfred Wegener Institute, Helmholtz Centre for Polar and <a href="http://www.earth.com/news/marine-species-are-moving-away-from-the-equator/">Marine</a> Research (AWI) showed that not only animals that live directly under the ice thrive on carbon produced by so-called ice algae. Even species that mostly live at greater depth depend to a large extent on carbon from these algae. This also means that the decline of the Arctic sea ice may have far-reaching consequences for the entire food web of the <a href="https://www.bing.com/search?q=arctic+ocean&amp;FORM=EDGENA&amp;PC=HCTS&amp;refig=e67e02a78cb6408faaccf7ab66a410e8">Arctic Ocean</a>. Their results have been published online now in the journal Limnology &amp; Oceanography.

The summer sea ice in the Arctic is diminishing at a rapid pace and with it the habitat of ice algae. The consequences of this decline for the Arctic ecosystem are difficult to predict. Scientists of the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research showed the significance of ice algae for the Arctic food web in this context. "A number of studies have already speculated that ice algae are an important energy source for the polar ecosystems. We have now been able to show that not only animals associated with ice meet the majority of their carbon needs from ice algae, but that, surprisingly, so do species that mostly live at greater depths," says lead author Doreen Kohlbach.Ice algae: The engine of life in the central Arctic Ocean

In a new study, she and her colleagues examined copepods, amphipods, crustaceans and sea angels from the central Arctic Ocean and their dependence on ice algae. A number of these species use the underside of the sea ice as their habitat. Many other species of zooplankton, however, spend their entire lives floating in water depths up to 1000 metres and more.

"We now know that ice algae play a much more important role for the pelagic food web than previously assumed. This finding also means, however, that the decline of the ice could have a more profound impact on Arctic marine animals, including fish, seals and ultimately also polar bears, than hitherto suspected," says Doreen Kohlbach.

The AWI researcher was able to establish the close relationship between zooplankton and ice algae using fatty acids as biomarkers, which are passed on unchanged in the food chain. The typical fatty acids in ice algae are thus indicators of whether an animal has ingested carbon from ice algae via food. In order to precisely determine the proportion of ice algae carbon in the diet, Doreen Kohlbach also performed an isotope analysis of these biomarkers. The scientist took advantage of the fact that ice algae inherently have a higher proportion of heavy carbon isotopes incorporated in their cells than algae that float freely in the water. On the basis of the ratio of heavy to light carbon isotopes in the biomarkers it is possible to determine the exact proportion of carbon derived from ice algae in the organisms along the food web.

The result showed that ice-associated animals derive between 60 and 90 percent of their carbon from the ice. For animals living at greater depths, the percentages were between 20 and 50 - significantly higher than expected. "Personally, I was most surprised by the percentage in the predatory amphipod Themisto libellula, which lives in the open waters and is not known to hunt under the surface of the ice. We now know that it obtains up to 45 percent of its carbon from ice algae, which had been eaten by its prey," says AWI sea ice ecologist and co-author Dr Hauke Flores. "We found that pelagic copepods also obtain up to 50 percent from these algae, even though we had assumed that they mainly feed on algae from the water column," Hauke Flores continues.

These figures were also surprising in view of the fact that ice algae mainly grow in spring when little light penetrates the ice, which is still thick at that time of the year. The samples, however, were taken in the summer - and the percentage of ice algae carbon in the food chain was still relatively high. The AWI scientists now wonder what the figures look like at other times of the year. They are also interested in whether a greater distinction can be made between the various ice algae and whether perhaps there is a key alga.

Based on the new study, it is now possible to back up the flow of ice algae carbon through the summer food web in the central Arctic using specific figures. AWI biologists can use these figures in model calculations to assess the consequences of the sea ice decline for the Arctic ecosystem.


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Ice algae: The engine of life in the central Arctic Ocean

Ice algae: The engine of life in the central Arctic...

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El Niño climate patterns contributed to the warm blob that began dominating the Gulf of Alaska in late 2013, and later gripped the West Coast of North America in what became the Northeast Pacific's largest marine heatwave, according to a <a href="http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate3082.html" target="_blank" rel="noopener">new study</a> published in Nature Climate Change today.

While the warm blob started in the Gulf of Alaska in 2013, its persistence and evolution into a much larger pattern of ocean warming in 2014 and 2015 involved long-distance "teleconnections" between the North and tropical <a href="https://www.bing.com/search?q=pacific&amp;cvid=5c70472f6b5b487babad9c9d087a10ed&amp;FORM=ANAB01&amp;PC=HCTS">Pacific.</a> El Nino climate patterns contributed to the warm blob

"The bottom line is that El Niño had a hand in this even though we're talking about very long-distance influences," said Nate Mantua, a research scientist at NOAA Fisheries' Southwest Fisheries Science Center and a coauthor of the new study. "It's been known for decades that El Niño causes changes in wind, weather, and ocean temperatures across the North Pacific through an 'atmospheric bridge,' where massive shifts in tropical rainfall influence storm tracks over the North Pacific and North America."

The new research found that the known climate patterns linked the tropical and temperate latitudes of the North Pacific Ocean, helping to fuel the extreme marine heatwave.El Nino climate patterns contributed to the warm blob

Climate models suggest that the extreme atmospheric conditions that gave rise to the warm blob could become more pronounced as greenhouse gases accumulate in the atmosphere, the study found. The study was authored by Emanuele Di Lorenzo of the Georgia Institute of Technology and Mantua.

"Climate models predict that these kind of multi-year extremes become stronger in a warming climate," Mantua said. "But while the models show that they should get stronger as the earth's climate warms, it's not clear to us yet if that is now detectable in nature."

The heat wave emerged in the fall of 2013, when a ridge of high pressure dampened winds over the Gulf of Alaska, allowing a large section of the North Pacific to warm by up to 3 degrees C (about 5 degrees F) above average. It represented the highest temperature anomaly in the North Pacific in more than 100 years of records. The ridge came with weak winds in the subtropical Pacific near Hawaii, which is a known precursor of El Niño conditions that develop up to one year later.

The warm patch spread to fill the northeast Pacific between Hawaii and the West Coast of North America by the fall of 2014, shaking up the marine food chain and leading to sightings of warm-water species far outside of their normal range. The conditions led to die-offs of seabirds, mass strandings for California sea lion pups, and likely contributed in 2015 to the largest-ever harmful algal bloom recorded on the West Coast, closing fisheries for clams and Dungeness crab.

"While the socio-economic consequences of this climate event need to be further evaluated, it is possible that the northeast Pacific warm anomaly of 2014-15 is the most ecologically and economically significant marine heatwave on record," the researchers wrote.

A weak El Niño pattern that stalled out during the winter of 2014-15 contributed to the North Pacific's heatwave, according to a combination of climate observations and model simulations. That was followed by a second and much stronger El Niño pattern that emerged the following winter, with an "atmospheric bridge" concentrating the extended warmth of the Northeast Pacific Ocean in an arc-pattern along the West Coast from Alaska to Mexico.

The latest observations in July 2016 show that ocean temperatures near the coast of Southern and Baja California, around Alaska and in a wide offshore band between Hawaii and Alaska remain about 3 degrees C warmer than average. In contrast, there are colder than normal surface temperatures along coast of Northern California and Southern <a href="https://www.earth.com/news/unequal-treatment-protestors/">Oregon,</a> and in patches along the equator.

The latest seasonal forecasts from NOAA's Climate Prediction Center show that the cool waters in the tropical Pacific are likely to expand and that a La Niña pattern is likely to develop during the Northern Hemisphere summer of 2016, with about a 75% chance of La Niña during the fall and winter of 2016-17. La Niña would favor changes in wind, weather, and ocean currents that tend to cool the Northeast Pacific Ocean between Hawaii and North America.


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El Nino climate patterns contributed to the warm blob

El Niño climate patterns contributed to the warm blob that...

<a href="http://www.earth.com/image/shasta-lake-northern-california/">California</a> Gov. Jerry Brown has launched a campaign to extend some of the most ambitious climate change efforts in the country and ensure his environmental legacy when he leaves office in two years. California governor hopes to extend climate change efforts
The centerpiece of the push is a cap-and-trade program that aims to reduce the use of fossil fuels by forcing manufacturers and other companies to meet tougher emissions limits or pay up to exceed them. The program has been one of the most-watched efforts in the world aimed at the climate-changing fuels.
The four-year-old program, however, is only authorized to operate until 2020 and faces a litany of challenges, including a lawsuit questioning its legality, poor sales of credits, and lukewarm support among Democratic legislators to extend it.
On Tuesday, the California Air Resources Board will release a proposed blueprint for continuing the cap-and-trade program until 2030, with a vote expected next year.
Supporters credit the strategy - born under previous Gov. <a href="https://www.bing.com/search?q=arnold+schwarzenegger&amp;form=EDGEAR&amp;qs=PF&amp;cvid=4ca4fc39e5fa4619909f511b2551a47b&amp;cc=US&amp;setlang=en-US&amp;elv=AY3%21uAY7tbNNZGZ2yiGNjfNqIbOEKEZbuUqFXmqcpemEo%215PM2sBYostJSqdPaPMpYwp5HQYTif6LdEJ0QJv%216ceJ3TQdi9DwJYaonw*7aQ4&amp;plvar=0&amp;PC=HCTS">Arnold Schwarzenegger</a>, a Republican, and stemming from other climate change programs initiated under Brown - with helping to cut California's overall output of emissions by 1.5 percent in its first two years, despite the massive energy demands of the state's thriving economy.California governor hopes to extend climate change efforts
With Brown set to leave office in 2018, a state appeals court is considering a challenge from the California Chamber of Commerce contending the pollution-credit program is an illegal tax, not a fee.
Environmental groups say the lawsuit and overall uncertainty about the survival of the program are undermining the market for pollution credits. A May auction saw companies buy only one-tenth of the available credits, leaving the state billions of dollars short in projected revenue from the sales.
Meanwhile, groups representing oil interests confirmed last week that they are in direct talks with the Brown administration over cap-and-trade.
California oil companies have long sought to alter or repeal the state's low-carbon fuel standard. By 2020, those companies would be required to reduce the carbon content of gasoline and other fuels by 10 percent, a significant jump from the current 2 percent.
Any deal-making on climate change would reflect a pragmatic approach to the oil industry by Brown, who took office encouraging immediate boosts in oil and gas drilling to spur California's economy, even as he promoted incentives that would reduce long-term reliance on fossil fuels.
"What you're seeing now is an all-hands-on-deck effort to formulate the most responsible way forward." said Derek Walker, an associate vice president of the Environmental Defense Fund. "They're talking to the oil industry, talking to environmental groups, to organized labor - they're talking to everybody."
Brown has leveraged his position as governor to help draw attention to the battle against climate change. He has set non-binding mandates for increased use of solar, wind and other renewable energy sources in California in the decades to come while signing accords and global support statements aimed at easing climate change.
At home, though, Brown has encountered trouble from moderate Democrats in the state Assembly who last year blocked his plan to slash statewide petroleum use in half within 15 years.
The same lawmakers refused to endorse legislation by Sen. Fran Pavley, D-Agoura Hills, seeking to dramatically cut greenhouse gas emissions through 2050. Pavley was forced to scale back her proposal that now would extend only to 2030. She has since compromised even further, agreeing last month to merge parts of her plan with legislation mandating that revenues from such programs be spent in low-income communities affected by pollution.
Winning legislative support could be key for Brown in ensuring the survival of the cap-and-trade program, said Jessica Levinson, a political science professor at Loyola Law School.
"His ability to solidify cap and trade is a big part of being able to say to other governors, to other countries, 'We're doing something big and specific and real and it works,'" Levinson said.
Should the program succumb to legal challenges, market weakness or legislative ambivalence: "Jerry Brown's fingerprints will be on whatever we ultimately decide to do," Levinson said.
---
Knickmeyer reported from San Francisco.
© 2016 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.

California governor hopes to extend climate change efforts

California Gov. Jerry Brown has launched a campaign to extend...

Greenland ice melt is rapidly increasing sea level rise. In the most detailed picture to date, information from ESA’s CryoSat satellite reveals how melting ice in Greenland has recently contributed twice as much to sea level rise as the prior two decades.

Between 2011 and 2014, Greenland lost around one trillion tonnes of ice. This corresponds to a 0.75 mm contribution to global sea-level rise each year – about twice the average of the preceding two decades.

The study, published in Geophysical Research Letters today, combines data from the <a href="https://www.earth.com/video/understanding-earths-climate-system-through-the-cryosphere/">CryoSat</a> mission with a regional climate model to map changes in Greenland ice-sheet mass. It is the most detailed recent picture of ice loss from Greenland.

CryoSat carries a radar altimeter that can measure the surface height variation of ice in fine detail, allowing scientists to record changes in its volume with unprecedented accuracy.

The study demonstrates how the satellite has allowed researchers to map the complex regional pattern of imbalance.

“CryoSat’s radar really brings into focus our view of the ice sheet, revealing which glaciers are exhibiting the greatest signs of change,” explained lead author Dr Mal McMillan from the UK Centre for Polar Observation and Modelling at the University of Leeds.

“This helps us to study Greenland’s individual outlet glaciers, which in turn allows us to better understand the contribution they have made to global sea-level rise.”

The study also shows large variations in the amount of ice loss from year to year, with the highest losses occurring in 2012 when summer temperatures hit record highs. This demonstrates Greenland’s sensitivity to sudden changes in the surrounding environment.

“These significant results clearly demonstrate CryoSat’s unique capability of recording cryospheric changes, and it is essential that it is maintained in future,” said CryoSat Mission Manager Tommaso Parrinello.

CryoSat’s measurement of Greenland ice losses are in close agreement with those computed from NASA’s GRACE mission, which carries sensors that are specially designed to weigh changes at the scale of the entire ice sheet.

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<a href="http://www.esa.int" target="_blank" rel="noopener">European Space Agency</a>

Greenland ice melt is rapidly increasing sea level rise

Greenland ice melt is rapidly increasing sea level rise. In...

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<a href="https://www.bing.com/search?q=nasa&amp;cvid=d5a17ea28cd6420aa1e75f7a83f33081&amp;FORM=ANAB01&amp;PC=HCTS">NASA</a> studies a strengthening Tropical Storm Darby. Tropical Storm Darby has been increasing in intensity since yesterday and is expected to become a hurricane. NASA provided a visible look at the structure of the storm and peered through it to determine surface wind speed.

On July 12 at 21:45 UTC (5:45 p.m. EDT) the Visible Infrared Imaging Radiometer Suite (VIIRS) instrument aboard NASA-NOAA-DOD's Suomi NPP satellite captured a visible light image of Hurricane Celia and Tropical Storm Darby in the Eastern Pacific Ocean. Celia is located to the northwest of Darby. As of today, July 13, Celia has weakened to a tropical storm. NASA studies a strengthening Tropical Storm Darby

VIIRS collects visible and infrared imagery and global observations of land, atmosphere, cryosphere and oceans.

On July 12, RapidScat saw Darby's strongest winds (red) southwest of the center at 27 meters per second (60.4 mph/97.2 kph). Since that time, the National Hurricane Center noticed that Darby had been rapidly intensifying with a 30 knot wind increase over 24 hours. RapidScat is a scatterometer instrument that flies aboard the International Space Station. It measures surface wind speeds and direction over open waters of oceans.

On July 13 at t 5 a.m. EDT (0900 UTC), the center of Tropical Storm Darby was located near latitude 15.3 North, longitude 111.5 West. That's about 540 miles (870 km) west-southwest of Manzanillo, Mexico. Darby was moving toward the west near 12 mph (19 kph) and the National Hurricane Center (NHC) said this general motion is expected for the next couple of days.

Maximum sustained winds have increased to near 70 mph (110 kph) with higher gusts. RapidScat imagery shows tropical-storm-force winds extend outward up to 70 miles (110 km) from the center. The estimated minimum central pressure is 998 millibars.

The NHC expects Darby to become a hurricane later today.


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NASA studies a strengthening Tropical Storm Darby

NASA studies a strengthening Tropical Storm Darby. Tropical Storm Darby...

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El Nino and climate change played a key role in Pacific Marine Heatwave. The largest <a href="https://www.earth.com/image/noumea-in-the-south-pacific-archipelago-of-new-caledonia/">pacific</a> marine heatwave on record was at least in part caused by El Niño climate patterns. And unusually warm water events in that ocean could potentially become more frequent with rising levels of greenhouse gases.

That's the findings of a new study by researchers from Georgia Institute of Technology and the National Oceanic and Atmospheric Administration. They linked the 2014-2015 marine heatwave - often referred to as the "warm blob" - to weather patterns that started in late 2013. The heatwave caused marine animals to stray far outside of their normal habitats, disrupting ecosystems and leading to massive die-offs of seabirds, whales and sea lions.

The study, which was published July 11 in journal Nature <a href="https://www.bing.com/search?q=climate+change&amp;cvid=c17b564cd2624539abe70705b32ab9a9&amp;FORM=ANAB01&amp;PC=HCTS">Climate Change</a>, was sponsored by the National Science Foundation.El Nino and climate change played a key role in Pacific Marine Heatwave

"We had two and a half years of consistent warming, which translated to a record harmful algal bloom in 2015 and prolonged stress on the ecosystem," said Emanuele Di Lorenzo, a professor in Georgia Tech's School of Earth and Atmospheric Sciences. "What we do in the study is ask whether this type of activity is going to become more frequent with greenhouse gases rising."

The researchers traced the origin of the marine heat wave to a few months during late 2013 and early 2014, when a ridge of high pressure led to much weaker winds that normally bring cold Artic air over the North Pacific. That allowed ocean temperatures to rise a few degrees above average.

Then, in mid-2014 the tropical weather pattern El Niño intensified the warming throughout the Pacific. The warm temperatures lingered through the end of the year, and by 2015 the region of warm water had expanded to the West Coast, where algal blooms closed fisheries for clams and Dungeness crab.

"The bottom line is that El Niño had a hand in this even though we're talking about very long-distance influences," said Nate Mantua, a research scientist at NOAA Fisheries' Southwest Fisheries Science Center and a coauthor of the study.

The researchers used climate model simulations to show the connection between increasing greenhouse gas concentrations and the impact on the ocean water temperatures. The study found that these extreme weather events could become more frequent and pronounced as the climate warms.

"This multi-year event caused extensive impacts on marine life," Di Lorenzo said. "For example, some salmon populations have life cycles of three years, so the marine heatwave has brought a poor feeding, growth and survival environment in the ocean for multiple generations. Events like this contribute to reducing species diversity."

And the effects of the "warm blob" could linger.

"Some of these effects are still ongoing and not fully understood because of the prolonged character of the ocean heatwave," Di Lorenzo said. "Whether these multi-year climate extremes will become more frequent under greenhouse forcing is a key question for scientists, resource managers and society."
###
This material is based upon work supported by the National Science Foundation under Grant Nos. OCE 1356924 and OCE 1419292. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the authors and do not necessarily reflect the views of the National Science Foundation.

CITATION: Emanuele Di Lorenzo and Nathan Mantua, "Multi-year persistence of the 2014/15 North Pacific marine heatwave," (Nature Climate Change, July 2016).

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El Nino and climate change played a key role in Pacific Marine Heatwave

El Nino and climate change played a key role in...

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NASA studies Tropical Cyclone Celia's winds and rainfall rates. Tropical Cyclone Celia continued to generate heavy rains as it moved through the Eastern Pacific Ocean. NASA's RapidScat analyzed surface wind speeds while the GPM core satellite measured rainfall rates occurring within the storm.

RapidScat is a scatterometer instrument that flies aboard the International Space Station. It measures surface wind speeds and direction over open waters of <a href="https://www.earth.com/news/the-worlds-oceans-have-become-less-resilient-to-climate-change/">oceans</a> On July 12 RapidScat saw strongest sustained surface winds (red) occurring east of the center of Hurricane Celia. Those winds were in excess of 30 meters per second (67.1 mph/108 kph). Images from RapidScat data are made into images at NASA's Jet Propulsion Laboratory in Pasadena, California where the mission is managed.NASA studies Tropical Cyclone Celia's winds and rainfall rates

The Global Precipitation Measurement (GPM) core observatory satellite twice flew almost directly above hurricane Celia in the eastern<a href="https://www.bing.com/search?q=pacific&amp;cvid=408abefede5b40c781c499b048a29805&amp;FORM=ANAB01&amp;PC=HCTS"> Pacific Ocean</a> on July 12, 2016. The first time was on July 12, 2016 at 0011 UTC (July 11 at 8:11 p.m. EDT) and the second view was on July 12, 2016 at 1326 UTC (9:26 a.m. EDT). With both passes GPM's Microwave Imager (GMI) clearly showed the location of rainfall around hurricane Celia's well defined eye. The hurricane had maintained intensity during this period with sustained maximum wind speeds estimated at 80 knots (92.8 mph). With the first pass GMI measured rain in the southwestern side of Celia's eye wall falling at a rate of close to 33 mm (1.3 inches) per hour. GPM is a joint mission between NASA and the Japanese space agency JAXA.

On July 13 at 5 a.m. EDT (0900 UTC) Celia weakened to a tropical storm. It was centered about 1,410 miles (2,270 km) west of the southern tip of Baja California. Celia was located near latitude 18.3 north and longitude 131.2 west. Celia was moving toward the west-northwest near 12 mph (19 kph) and this general motion is expected to continue for the next couple of days. Maximum sustained winds have decreased to near 70 mph (110 kph) with higher gusts. Additional weakening is forecast during the next 48 hours. The estimated minimum central pressure is 987 millibars.

Celia is moving in the general direction of the Hawaiian Islands but is predicted to weaken to tropical depression intensity in a few days as it moves into the central Pacific.


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NASA studies Tropical Cyclone Celia's winds and rainfall rates

NASA studies Tropical Cyclone Celia's winds and rainfall rates. Tropical...

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



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



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



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



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



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



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



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



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



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

Is chocolate the next nutritional powerhouse?

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

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



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



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



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



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



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



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



Video Credit: Amanda Nguyen/University of Illinois



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



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



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



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



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



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



Video Credit: ESA&nbsp;&nbsp;



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



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.

Lesotho: Africa's "Kingdom in the Sky"

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



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



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



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



Video Credit: NASA Goddard



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



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 <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

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



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



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



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



Video Credit: NASA Goddard&nbsp;



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



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Satellites reveal how Earth's systems are interconnected

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



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



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



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



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



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



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



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Tiger sharks are shifting poleward as temperatures rise

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

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



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



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



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



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



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



Video Credit: ESA&nbsp;



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



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

Melt ponds on the Greenland Ice Sheet

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



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



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



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



Video Credit: ESA



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



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Tracking changes in Earth's water cycle

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



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



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



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



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



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



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



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



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



Video Credit: NASA Goddard&nbsp;



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



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

Mysterious "spoke season" captured on Saturn

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

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



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



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



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



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



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



Video Credit: NTU Singapore



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



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

Plants help remove heavy metals from contaminated soil

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



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



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



Video Credit: American Chemical Society&nbsp;



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



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

Weeds are becoming increasingly resistant to herbicides

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



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



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



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



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



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



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



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NASA monitors giant dust storms on Mars

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



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



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



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



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



Video Credit: ESA&nbsp;



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



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Qeshm Island in the Strait of Hormuz

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



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



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



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



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



Video/ Image Credit: ESA



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



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Inhambane Bay in southeast Mozambique

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



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



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



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



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



Video Credit: ESA



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



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Kangerlussuaq Glacier on the Greenland ice sheet

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



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



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



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



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



Video Credit: ESA



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



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Ocean heat influences regional climate

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



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



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



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



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



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



Image/ Video Credit: ESA



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

Monitoring the dynamic shape of the sea surface

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