Does ocean coupling matter for the northern extratropical response to projected Arctic sea ice loss?
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Does ocean coupling matter for the northern extratropical response to projected Arctic sea ice loss?
  • Published Date:

    2016

  • Source:
    Geophysical Research Letters, 43(5), 2149-2157.
Filetype[PDF-5.79 MB]


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Does ocean coupling matter for the northern extratropical response to projected Arctic sea ice loss?
Details:
  • Personal Author:
  • Description:
    The question of whether ocean coupling matters for the extratropical Northern Hemisphere atmospheric response to projected late 21st century Arctic sea ice loss is addressed using a series of experiments with Community Climate System Model version 4 at 1 degrees spatial resolution under different configurations of the ocean model component: no interactive ocean, thermodynamic slab ocean, and full-depth (dynamic plus thermodynamic) ocean. Ocean-atmosphere coupling magnifies the response to Arctic sea ice loss but does not change its overall structure; however, a slab ocean is inadequate for inferring the role of oceanic feedbacks. The westerly winds along the poleward flank of the eddy-driven jet weaken in response to Arctic sea ice loss, accompanied by a smaller-magnitude strengthening on the equatorward side, with largest amplitudes in winter. Dynamical and thermodynamic oceanic feedbacks amplify this response by approximately 50%. Air temperature, precipitation, and sea level pressure responses also show sensitivity to the degree of ocean coupling.
  • DOI:
    https://doi.org/10.1002/2016GL067792
  • Document Type:
    Journal Article
  • Collection(s):
    NOAA Cooperative Institutes
    Office of Oceanic and Atmospheric Research (OAR)
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