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Effect of sea ice morphology during Arctic summer on atmospheric drag coefficients used in climate models
Author(s) -
Lüpkes C.,
Gryanik V. M.,
Rösel A.,
Birnbaum G.,
Kaleschke L.
Publication year - 2013
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 - 10.1002/grl.50081
Subject(s) - parametrization (atmospheric modeling) , drag , sea ice , arctic ice pack , atmospheric sciences , arctic , drag coefficient , environmental science , geology , climatology , physics , oceanography , mechanics , radiative transfer , quantum mechanics
Realistic modeling of polar sea ice dynamics and atmospheric processes over sea ice needs a detailed representation of the near‐surface atmospheric fluxes of momentum. In this study, parametrizations of neutral drag coefficients mostly used in different general circulation models are compared with a recently developed parametrization including the impact of sea ice morphology. The new parametrization, using the sea ice and melt pond fraction as governing parameters, accounts for the effect of form drag caused by edges at leads, melt ponds, and floes. Based on remote sensing data of ice and melt pond fraction, it is shown that during Arctic summer the traditionally used drag coefficients differ from the new ones by a factor 0.5–1.2. The geographic distribution of drag coefficients obtained from both parametrizations is very different. Differences are due to a nonlinear and non‐monotonic dependence of drag coefficients on sea ice concentration in the new parametrization.