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The melt‐freeze cycle of the Arctic Ocean ice cover and its dependence on ocean stratification
Author(s) -
Linders Johanna,
Björk Göran
Publication year - 2013
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
eISSN - 2169-9291
pISSN - 2169-9275
DOI - 10.1002/jgrc.20409
Subject(s) - halocline , sea ice , stratification (seeds) , arctic ice pack , drift ice , antarctic sea ice , arctic , climatology , geology , sea ice thickness , melt pond , cryosphere , canada basin , arctic sea ice decline , oceanography , thermohaline circulation , environmental science , salinity , seed dormancy , botany , germination , dormancy , biology
A time‐dependent, 1‐D coupled ice‐ocean model is used to quantify the impact of ocean stratification on the Arctic ice cover. The model results show that the ice growth during winter equals the ice melt in summer for areas with a well‐developed cold halocline layer (CHL), provided that the initial ice thickness is around 3 m, while thinner initial ice thickness results in net growth. Areas with weak salt stratification can have a negative annual thickness change irrespective of the initial ice thickness and are thus dependent on ice import in order to remain ice covered. The model results also show that ocean stratification is mostly important for ice‐thickness development during the growing season. Areas with weak stratification have an ocean heat flux up to 8 W m −2 reaching the ice during the growing season, while areas with a CHL have an average of about 0.7 W m −2 . In the extreme area, north of Svalbard, the ocean heat fluxes are typically around 25 W m −2 but can be up to 400 W m −2 during the initial adjustment, when the warm Atlantic water has direct contact with the ice. A general outcome of the study is that, depending on ocean stratification, the ice cover of Arctic Ocean can be divided into one part with net ice growth (the major part) and another part with net ice melt (mainly in the Nansen Basin).