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Unusually, there is melting at the bottom of the NGRIP core – believed to be due to a high geothermal heat flux locally. This has the advantage that the bottom layers are less compressed by thinning than they would otherwise be: NGRIP annual layers at 10.5 kyr age are 1.1 cm thick, twice the GRIP thicknesses at equal age.
Dye 3 circa early 1980s. Dye 3 is an ice core site and previously part of the DYE section of the Distant Early Warning (DEW) line, located at (, 2480 masl) [1] in GreenlandAs a DEW line base, it was disbanded in years 1990/1991.
View of the GRIP site at Summit Camp. The Greenland Ice Core Project (GRIP) was a research project organized through the European Science Foundation (ESF). [1] The project ran from 1989 to 1995, with drilling seasons from 1990 to 1992. [2]
Schools were shuttered in North Dakota, South Dakota, Minnesota and Wisconsin while public officials warned people to keep off the roads due to dangerous whiteout conditions and snow squalls.
Changes in the elevation of Lake Superior due to glaciation and post-glacial rebound. During the last glacial period, much of northern Europe, Asia, North America, Greenland and Antarctica were covered by ice sheets, which reached up to three kilometres thick during the glacial maximum about 20,000 years ago.
A yellow warning for ice was in place until 10:00 GMT on Thursday [Getty Images] Motorists have been urged to take care on the roads as cold conditions cause ice across Northern Ireland.
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