supraglacial lake oor Italiaans
supraglacial lake
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Lago supraglaciale
en
pond of liquid water on the top of a glacier
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Supraglacial lakes can occur in all glaciated areas.
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A supraglacial lake is any pond of liquid water on the top of a glacier.
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Details of supraglacial lake research from Sarah Das, a specialist.
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Sedimentary particles often accumulate in supraglacial lakes; they are washed in by the meltwater or rainwater that supplies the lakes.
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A proliferation of supraglacial lakes preceded the collapse of the Antarctic Larsen B ice shelf in 2001, and may have been connected.
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Supraglacial lakes represent another possible supply of liquid water to the base of glaciers, so they can play an important role in accelerating glacial motion.
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Meltwater may come from a number of sources, including supraglacial lakes, geothermal heating of the bed, conduction of heat into the glacier and latent heat transfers.
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Supraglacial lakes also have a warming effect on the glaciers; having a lower albedo than ice, the water absorbs more of the sun's energy, causing warming and (potentially) further melting.
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A supraglacial lake on the surface of the Bering Glacier in 1995.
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It was once unclear whether global warming is increasing the abundance of supraglacial lakes on the Greenland Ice Sheet.
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A proliferation of supraglacial lakes preceded the collapse of the Antarctic Larsen B ice shelf in 2001,[citation needed] and may have been connected.
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Increasing global air temperatures take around 10,000 years to directly propagate through the ice before they influence bed temperatures, but may have an effect through increased surfacal melting, producing more supraglacial lakes, which may feed warm water to glacial bases and facilitate glacial motion.
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Some of these theories proposed that Rogen moraines had an origin as a series of end moraines, that they formed in association with calving ice termini in glacial lakes, or that Rogen moraines formed in dead-ice, where supraglacial material fell down into crevasses in the ice.
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