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Albedo evolution of seasonal Arctic sea ice
Author(s) -
Perovich Donald K.,
Polashenski Christopher
Publication year - 2012
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2012gl051432
Subject(s) - ice albedo feedback , sea ice , cryosphere , arctic ice pack , melt pond , antarctic sea ice , sea ice thickness , drift ice , environmental science , albedo (alchemy) , climatology , arctic sea ice decline , oceanography , geology , atmospheric sciences , art , performance art , art history
There is an ongoing shift in the Arctic sea ice cover from multiyear ice to seasonal ice. Here we examine the impact of this shift on sea ice albedo. Our analysis of observations from four years of field experiments indicates that seasonal ice undergoes an albedo evolution with seven phases; cold snow, melting snow, pond formation, pond drainage, pond evolution, open water, and freezeup. Once surface ice melt begins, seasonal ice albedos are consistently less than albedos for multiyear ice resulting in more solar heat absorbed in the ice and transmitted to the ocean. The shift from a multiyear to seasonal ice cover has significant implications for the heat and mass budget of the ice and for primary productivity in the upper ocean. There will be enhanced melting of the ice cover and an increase in the amount of sunlight available in the upper ocean.