Inter-division Event for International Polar Year.
How can you make glacier goo?
How can you make a snow shelter?
Look for fossils in your own yard!
| Name | Title | Fields of interest | |
|---|---|---|---|
| Elizabeth Case | Graduate Student |
A small team of scientists ventures out onto the Greenland ice sheet to study the forces large and small that are accelerating the melting of the world’s second-largest ice mass.
For this early part of the season the goal is to tease apart a record of historic precipitation and temperature for this region using isotopes from leaf waxes collected in the lake sediments.
Snow on Ice is launching into the field with two teams of scientists this summer. The first group, an ‘advance team’ of six women, will focus on lakes where meltwater has collected on the southwestern flank of Greenland bedrock.
A new algorithm quickly sifts through hours of field recordings to learn how climate change influences bird migration. The A.I. could help track other wildlife as well.
As the Arctic warms, the unfreezing of permafrost poses a threat to the planet.
Iron particles catching a ride on glacial meltwater washed out to sea are likely fueling a recently discovered summer algal bloom off the southern coast of Greenland, according to a new study.
Microalgae, also known as phytoplankton, are plant-like marine microorganisms that form the base of the food web in many parts of the ocean. “Phytoplankton serve as food for all of the fish and animals that live there. Everything that eats is eating them ultimately,” said Kevin Arrigo, a biological oceanographer at Stanford University and lead author of the study.
The Arctic is warming twice as fast as the rest of the planet, and scientists are seeing the effects across ice and ecosystems. The average annual air temperature over Arctic land is now 3.5°C (6.5°F) warmer than it was 1900, Greenland is experiencing longer melting seasons, and this year’s spring snow cover extent set a record low in the North American Arctic, according to the National Oceanic and Atmospheric Administration’s newly released 2016 Arctic Report Card.
The Gordon and Betty Moore Foundation announced a $3.7 million grant to Columbia University's Lamont-Doherty Earth Observatory to support research that couples state-of-the-art geophysical observations from unmanned aerial systems with a community-engaged research approach to bridge scientific and indigenous understanding of sea ice change in the Alaskan Arctic.
The Arctic’s frozen ground contains large stores of organic carbon that have been locked in the permafrost for thousands of years. As global temperatures rise, that permafrost is starting to melt, raising concerns about the impact on the climate as organic carbon becomes exposed. A new study is shedding light on what that could mean for the future by providing the first direct physical evidence of a massive release of carbon from permafrost during a warming spike at the end of the last glacial period.
Kenneth Hunkins, an oceanographer who made many key 20th-century observations about the Arctic Ocean, often while camping for months on its frozen surface, died in his sleep at his home in Tappan, N.Y., on Sept. 2. He was 86. Columbia University’s Lamont-Doherty Earth Observatory, where he had spent his entire career, confirmed his death.
Tiny one-celled organisms called radiolaria are ubiquitous in the oceans, but various species prefer distinct habitats. Thus it aroused considerable intrigue in 2012 when protozoa specialist O. Roger Anderson and colleagues published a study showing that radiolaria normally found near the equator were suddenly floating around in arctic waters above Norway. Was this a sign that global climate change was bringing an invasion of warm-weather plankton?
The small town of Barrow, Alaska is perched on a point of land 320 miles above the Arctic Circle, where stark, flat tundra stretches in one direction and a vast expanse of Arctic Ocean extends to the horizon in the other. For most of the year a thick layer of sea ice covers this entire ocean. Even during the height of summer, a partial covering of ice remains, and the ocean temperature doesn’t rise above 35 degrees Fahrenheit. Despite these seemingly inhospitable conditions, tiny marine organisms thrive in this frigid environment.
Summers on the Norwegian archipelago of Svalbard are now warmer than at any other time in the last 1,800 years, including during medieval times when parts of the northern hemisphere were as hot as, or hotter, than today, according to a new study in the journal Geology.
A team led by Kevin Anchukaitis of the Lamont-Doherty Earth Observatory Tree Ring Lab is currently in Alaska’s Arctic National Wildlife Refuge, studying the effects of changing climate on trees. Ferried in by a bush pilot who landed on the tundra to drop them off, they are practically at treeline–the place where it is too far north for trees to grow. But there are still some spindly white spruces here, and they are taking cores from these, which can be used to measure weather of the past.
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Rapid Change in the Arctic and the Tropics: Vulnerabilities and Opportunities | |
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Researchers crack the ice to study the Arctic marine food web - Science Nation | |
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Ken Hunkins Memorial | |
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Life in and under Arctic Sea Ice | Featuring LDEO scientist Andrew Juhl |
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NOVA | Secrets Beneath the Ice | Featuring LDEO Scientist Robin Bell |
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Changes in the Arctic and Antarctic | Featuring LDEO scientist Robin Bell |
