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Ice formation normally starts in late November in the north and east, and the maximum ice coverage occurs in late February to early March.
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Around 150,000 years ago the extent of ice coverage reached a maximum, followed around 130,000 years before the present (YBP) by a rapid deglaciation.
Sea level reductions and extended ice coverage likely eliminated most shelf habitats during the past glacial maximum about 20 000 years ago (Anderson et al. 2002).
A climate-dependent model of ice dynamics is employed to determine ice coverage and ice flux.
Sea ice coverage is massively reduced (up to 90%).
The loss of ice coverage has created additional ice-free habitat for Adélie penguins.
The maximum ice thickness can reach 7.7 cm.
Ice conductivity, the ice ocean drag parameter, maximum ice salinity and ridging parameters significantly affect the simulation year-round.
The study was designed to test a widely held hypothesis that population sizes of "ice-loving" top predators declined with decreasing ice coverage, whereas "ice-avoiding" species increased in population size as ice coverage diminished.
In any vitrification solution, the temperature of maximum ice growth rate is above the temperature of maximum ice nucleation rate.
Nonetheless, the total ice coverage was still 2.2percentt below the long-term average.
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