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Glaciers - National Snow and Ice Data Center
WEBglaciers begin to form when snow remains in the same area year round, where enough snow accumulates to transform into ice. Each year, new layers of snow bury and compress the previous layers. This compression forces the snow to recrystallize, initially forming grains similar to the size and shape of sugar grains.
Nsidc.orgLearn - National Snow and Ice Data Center
WEBTwo categories of glaciers exist: ice sheets and alpine glaciers. Ice sheets cover vast areas of land in broad domes. Alpine glaciers, are smaller, and found not only at the poles, but in high mountain regions across the globe.
Nsidc.orgWhy Glaciers Matter - National Snow and Ice Data Center
WEBWhy they matter. glaciers, slow-moving rivers of ice, have sculpted mountains and carved valleys throughout Earth's history. They continue to flow and shape the landscape in many places today. But glaciers affect much more than the landscape. Glacier melt delivers nutrients into lakes, rivers, and oceans. Those nutrients can drive blooms of
Nsidc.orgGlacier Quick Facts - National Snow and Ice Data Center
WEBA glacier is an accumulation of ice and snow that slowly flows over land. Alpine glaciers are frozen rivers of ice, slowly flowing under their own weight down mountainsides and into valleys. Ice sheets exist only on Greenland and Antarctica, and they spread out in broad domes in multiple directions. A group of people explore the Perito Moreno
Nsidc.orgScience of Glaciers - National Snow and Ice Data Center
WEBglaciers move by internal deformation of the ice, and by sliding over the rocks and sediments at the base. The weight of overlying snow, firn, and ice, and the pressure exerted by upstream and downstream ice deforms glacier ice, in a phenomenon known as creep. A glacier may slide on a thin layer of water at its base.
Nsidc.orgHomepage | National Snow and Ice Data Center
WEBArctic sea ice has likely reached its minimum extent for the year, at 4.28 million square kilometers (1.65 million square miles) on September 11, 2024, according to scientists at the National Snow and Ice Data Center (NSIDC) at the University of Colorado Boulder. The 2024 minimum is ranked seventh lowest in the 46-year satellite record. Read More.
Nsidc.orgGLIMS - National Snow and Ice Data Center
WEBGLIMS is an international project to inventory the world’s glaciers and to create a comprehensive, global database of land ice through repeat surveys. This data collection’s primary data product is the GLIMS Glacier Database. The glacier database includes measurements of glacier geometry, glacier area, snowlines, supraglacial lakes and rock
Nsidc.orgWhat are glacial lakes? | National Snow and Ice Data Center
WEBFeb 15, 2022 — A glacial lake is a body of water that originates from a glacier. It typically forms at the foot of a glacier, but may form on, in, or under it. As Earth’s climate warms, the world’s glaciers are shrinking, increasing freshwater outputs to all kinds of glacial lakes. Some communities depend on glacial meltwater for seasonal irrigation or
Nsidc.orgWorldwide retreat of glaciers confirmed in unprecedented detail
WEBThe IPCC report concluded that most of the world’s glaciers have been losing ice at an increasing rate in recent decades. More than 60 institutions across the globe are involved in GLIMS, with more than 150 scientists from all over the world contributing to this compilation. Jeffrey S. Kargel of the Department of Hydrology and Water Resources
Nsidc.orgThe story is in the ice: Documenting climate change through the …
WEBAug 12, 2024 — They were programmed to snap continuous shots of glaciers during every hour of daylight for months or years on end. These were the photos that would eventually end up at NSIDC. In addition to the time-lapse photography, the project also captured beauty shots, which focused on the character of ice, and repeat photographic sequences …
Nsidc.org