Heat Exchange: Q total = Q s -(Q b + Q e + Q h )
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Transcript of Heat Exchange: Q total = Q s -(Q b + Q e + Q h )
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Heat Exchange: Qtotal = Qs -(Qb + Qe + Qh)
Qh 24 watts/m2
Qb, 66 watts/m2
long wave terrestial radiation
Qs, 168 watts/m2
Short wave solar radiation
Qe, 78 watts/m2
evaporation
Freshwater Exchange = Precipitation - Evaporation
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Heat Flux between the ocean and atmosphere
Heat Exchange: Qtotal = Qs -(Qb + Qe + Qh)
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Net CONet CO22 Flux from Takahashi et al., 2002 Flux from Takahashi et al., 2002
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northward
northward
southward
southward
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SurfaceDeepBottom
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conv
ecti
on
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There is a lot of subsurface heat,separated from the surface mixed layer by a weak pycnocline.Slight changes in stratificationwould induce big changes in vertical heat flux and of the wintersea ice cover
Stratification under a full sea ice cover, Weddell sea
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Ope
n oc
ean
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