A major goal of this proposal will be to improve the net surface mass balance estimate of Antarctica by incorporating the mass loss due to wind-drifted sublimation over wind-scour zones.
The Antarctic and Southern Ocean Data Portal provides access to geoscience data, primarily marine, from the Antarctic region.
The ring of deep water around Antarctica not only links the major ocean [Atlantic/Pacific/Indian] , but also produces dense waters along the continental margins of the frozen continent, which sinks
| Name | Title | Fields of interest | |
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Laura Stevens | Postdoctoral Research Fellow | Glaciology, Geophysics, Physical processes driving ice-sheet flow. |
| Elizabeth Case | Graduate Student | ||
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Hugh Ducklow | Professor | Ecosystems ecology, marine and global biogeochemistry, microbial ecology |
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Indrani Das | Lamont Associate Research Professor | Mass balance of Antarctica and Greenland ice sheets, and mountain glaciers deep ice processes, ice-ocean interaction, basal melt of ice shelves, grounding line processes, Climate change and sea level rise. Airborne laser altimetry and ice penetrating radar, satellite remote sensing, surface energy and mass balance models, ice surface hydrology, dust and aerosols. |
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Bruce A. Huber | Senior Staff Associate |
An engineer at Lamont-Doherty, Frearson builds instruments that help scientists collect vital data in Antarctica, the deep sea, and at the top of volcanoes.
The warmer it gets, the faster Antarctica will lose ice, and at some point the losses will become irreversible. That is what researchers say in a new cover story in the leading journal Nature, in which they calculate how much warming the Antarctic Ice Sheet can survive.
Newly discovered deep seabed channels beneath the Thwaites Glacier in West Antarctica may be pathways for warm ocean water to melt the undersides of the ice, and contribute to sea-level rise say scientists.
A new study says that many of the ice shelves ringing Antarctica could be vulnerable to quick destruction if rising temperatures drive meltwater into the numerous fractures that currently penetrate their surfaces.
Research by Center for Climate and Life Fellow Pierre Dutrieux will lead to greater understanding of the West Antarctic Ice Sheet’s future stability and associated sea level rise.
Researchers long ago predicted that the 1987 Montreal Protocol, banning ozone-depleting gases, would reverse a worrisome trend in Southern Hemisphere winds. A new study shows they were right.
Earth Institute researchers are in the field studying the dynamics of the planet on every continent and every ocean. Here is a list of projects.
Long-lived compounds implicated in a third of overall global warming from 1955 to 2005.
A bay in Antarctica has been named after biological oceanographer Hugh Ducklow to celebrate his contributions to Antarctic research.
Pierre Dutrieux, a Lamont oceanographer and 2019 Climate and Life Fellow, discusses his Antarctic research and what the new IPCC report says about sea-level rise.
A new study shows, for the first time, evidence of a link between human-caused global warming and melting of the West Antarctic Ice Sheet.
The Antarctic field team returns to humanity, showers, and hot breakfasts.
A team of scientists working in Antarctica faces a host of new challenges.
Moving a team from a science base into a deep field camp comes with a mix of high energy and optimism. Yes there is always a bit of concern that the necessary plans are in place for the operation to be successful, but time is always a factor pushing to move things along.
From cooking to going to the bathroom, here’s what daily life is like in a remote Antarctic camp.
Fieldwork in Antarctica adds a whole new layer to the meaning of planning. When heavily field based projects are planned, it is common for preliminary fieldwork to precede the larger project.
On every continent and every ocean, Earth Institute researchers are studying climate, geology, natural hazards and other dynamics of the planet. Here is a list of projects in rough chronological order for the coming year and beyond.
A concerted, multidisciplinary, and international effort is needed to tackle this complexity, scientists argue in a paper released today.
Thousands of years ago, the West Antarctic ice sheet shrank dramatically—then grew back in an unexpected way.
An international collaboration will study the wasting of the Thwaites glacier, which already accounts for around 4 percent of current global sea-level rise, and could collapse within decades or centuries.
Lamont’s Robin Bell is one of the world’s leading polar investigators and has been tracking ice for thirty years. She has coordinated ten expeditions to Antarctica and Greenland. And although she took her first expedition to Antarctica back in the 1980s, there is nothing routine about her approach.
Working as an Antarctic field scientist, I witnessed the destruction provoked by a rapidly warming planet. But I also found inspiration.
The coasts of Antarctica are ringed with ice shelves – large expanses of ice that float on the surrounding ocean and form the outermost extensions of the glaciers that cover the land behind them. A new study shows that even minor deterioration of ice shelves can instantaneously hasten the motion and loss of ice hundreds of miles landward.
One of the largest icebergs ever, roughly the size of Delaware just broke off Antarctica according to scientists who have been observing the area for years. While it’s not unusual for ice shelves to calve, many in the climate community fear that the breaking of Larsen C may be a signal of other events to come
In recent years, scientists have discovered hundreds of lakes lying hidden deep beneath the Antarctic ice sheet. Now a team of researchers has found the remains of at least one sub-ice lake that existed when the ice was far more extensive, in sediments on the Antarctic continental shelf. The discovery is significant because it is thought that such lakes may have accelerated the retreat of glaciers in the past, and could do so again. Their study appears this week in the journal Nature Communications.
Antarctica’s ice locks up enough fresh water to inundate coastal regions around the globe. And the ice is on the move: The continent’s vast glaciers are sliding toward the coast and out over the ocean, forming huge ice shelves that in some places are collapsing. Researchers from the Lamont-Doherty Earth Observatory have spent the last two Antarctic summers flying over the massive Ross Ice Shelf, deploying a custom-made package of instruments to probe the ice. Their goal: to untangle the interactions between ice, ocean and land, to try and gauge the effects of warming climate.
In the first such continent-wide survey, scientists have found extensive drainages of meltwater flowing over parts of Antarctica’s ice during the brief summer. Researchers already knew such features existed, but assumed they were confined mainly to Antarctica’s fastest-warming, most northerly reaches. Many of the newly mapped drainages are not new, but the fact they exist at all is significant; they appear to proliferate with small upswings in temperature, so warming projected for this century could quickly magnify their influence on sea level. An accompanying study looks at how such systems might influence the great ice shelves ringing the continent, which some researchers fear could collapse, bringing catastrophic sea-level rises. Both studies appear this week in the leading scientific journal Nature.
Many giant shelves of ice hanging off Antarctica into the Southern Ocean are now melting rapidly. But up to now, it has been a mystery why much of the resulting fresh water ends up in the depths instead of floating above saltier, denser ocean waters. Scientists working along one major ice shelf believe they have found the answer: earth’s rotation is pushing meltwater sideways as it bleed off the ice, preventing it from reaching the surface. The finding has implications for how ocean circulation may affect the planet’s future climate. The research was published this week in the journal Nature.
A metal tube packed with scientific instruments parachuted into the ice-cold waters of Antarctica’s Ross Sea on Tuesday, marking a new frontier in polar research. This ALAMO float and five others being deployed over the coming weeks are the first explorers of their kind to begin profiling the water adjacent to Antarctica’s Ross Ice Shelf and sending back data in real time. Their mission: find vulnerabilities where warmer (but still near freezing) water from the deep ocean may be seeping in under the ice shelf and melting it from below. That information, paired with aerial surveys currently mapping the ice shelf and the sea floor beneath it, will help scientists assess the stability of the Ross Ice Shelf as they seek to understand how quickly Antarctica will lose ice in a warming world and what that will mean for sea level rise globally.
A special section in the October issue of BioScience examines the effects of a single season of intense melting on two Antarctic ecosystems, tracking impacts all the way from microbial food webs to shifting penguin populations.
Twenty-three million years ago, the Antarctic Ice Sheet began to shrink, going from an expanse larger than today’s to one about half its modern size. Computer models suggested a spike in carbon dioxide levels as the cause, but the evidence was elusive – until now. Ancient fossilized leaves retrieved from a lake bed in New Zealand now show for the first time that carbon dioxide levels increased dramatically over a relatively short period of time as the ice sheet began to deteriorate. The findings raise new questions about the stability of the Antarctic Ice Sheet today as atmospheric CO2 concentrations rise to levels never before experienced by humans.
In a new study, Lamont's Michael Previdi and Lorenzo Polvani found that the effect of rising temperatures on snowfall in Antarctica has so far been overshadowed by the frozen continent's large natural climate variability. By mid-century, however, as temperatures continue to rise, the effect of human-induced warming on Antarctica's net snow accumulation should emerge above the noise, and the increase in snowfall could begin to help partially offset sea level rise.
The fate of the ice sheets has a direct impact on populations worldwide: as the land-based ice melts, it raises sea level, and that can threaten coastal communities and economies.
Readers can follow a New York Times blog from the arctic as the U.S. flagship vessel for charting geology under the seabed sails the Chukchi Sea, north of Alaska and Siberia. By sending sound pulses to the seabed and reading the echoes, scientists conducting the Chukchi Edges project aboard the Marcus G. Langseth hope to understand the structure and history of the continental shelves running underwater off Asia and North America, and the Chukchi Borderland, an adjoing region of dramatic deep-sea plateaus and ridges some 800 miles from the North Pole.
The frigid seabottom off Antarctica holds a surprising riot of life: colorful carpets of sponges, starfish, sea cucumbers and many other soft, bottom-dwelling animals,shown on images from robotic submarines. Now, it appears that many such communities could fast disappear, due to warming climate.
Stronger ocean currents beneath West Antarctica’s Pine Island Glacier Ice Shelf are eroding the ice from below, speeding the melting of the glacier as a whole, according to a new study in Nature Geoscience. A growing cavity beneath the ice shelf has allowed more warm water to melt the ice, the researchers say—a process that feeds back into the ongoing rise in global sea levels. The glacier is currently sliding into the sea at a clip of four kilometers (2.5 miles) a year, while its ice shelf is melting at about 80 cubic kilometers a year - 50 percent faster than it was in the early 1990s - the paper estimates.
Warming Climate Drives Plankton and Penguins Poleward
Adélie penguins are flocking closer to the South Pole. A new study in the leading journal Science explains why: they’re following the food supply, which is moving southward with changing climate.
Under Miles of Ice, Range May Hold Secrets of Geology and Climate
Scientists from six nations will combine efforts over the next three months to try and penetrate one of earth’s last unexplored places: Antarctica’s vast Gamburtsev Mountains, never seen by humans...
Each year nearly 40,000 tons of cosmic dust fall to Earth from outer space. Now, the first successful chronological study of extraterrestrial dust in Antarctic ice has shown that this amount has remained largely constant over the past 30,000 years, a finding that could help refine efforts to understand the timing and effects of changes in the Earth's past climate.
Seismologists at Columbia University and Harvard University have found a new indicator that the Earth is warming: "glacial earthquakes" caused when the rivers of ice lurch unexpectedly and produce temblors as strong as magnitude 5.1 on the moment-magnitude scale, which is similar to the Richter scale. Glacial earthquakes in Greenland, the researchers found, are most common in July and August, and have more than doubled in number since 2002.
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Kirsty Tinto: Mapping on and under Antarctica's Ice | |
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Western Antarctic Peninsula: Rapid Climate Change and an Ecosystem Near a Tipping Point | |
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Basal Plumbing for the Changing (ice) Masses | Earth Science Colloquium |
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A Delicate Balance: Antarctica and its Surrounding Oceans | Part of the 2011 Public Lecture Series |
