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Winter sea‐ice melt in the Canada Basin, Arctic Ocean
Author(s) -
Jackson Jennifer M.,
Williams William J.,
Carmack Eddy C.
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 - 10.1029/2011gl050219
Subject(s) - sea ice , environmental science , halocline , climatology , arctic ice pack , drift ice , antarctic sea ice , geology , atmospheric sciences , oceanography , salinity
Recent warming and freshening of the Canada Basin has led to the year‐round storage of solar radiation as the near‐surface temperature maximum (NSTM). Using year‐round ocean (from ice tethered profilers and autonomous ocean flux buoys), sea‐ice (from ice mass balance buoys), and atmosphere (from NCEP/NCAR reanalysis) data from 2005–2010, we find that heat from the NSTM is entrained into the surface mixed layer (SML) during winter. Entrainment can only occur when the base of the SML reaches the top of the NSTM. If this condition is met, the surface forcing and stratification together determine whether the SML deepens into the NSTM. Heat transfer occurs by diffusion or by the erosion of the summer halocline. The average temperature of the SML warmed by as much as 0.06°C during storm events. Solar radiation began warming the SML about 1 month early during the winter of 2007–2008 and this can be explained by thin sea ice.