Ocean heat uptake in transient climate change : mechanisms and uncertainty due to subgrid-scale Eddy mixing /
(Cont.) Experiments are carried out with values of the diffusivity of 500, 1000, and 2000 m2/sec. The total OHU is insensitive to these changes. The insensitivity is mainly due to the changes in the vertical heat flux by GMR mixing being compensated by changes in the other vertical heat flux compone...
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Format: | Book |
Language: | English |
Published: |
Cambridge, MA :
MIT Joint Program on the Science and Policy of Global Change,
[2003]
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Series: | Reprint series (Massachusetts Institute of Technology. Joint Program on the Science and Policy of Global Change) ;
no. JP 03-006 |
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QC981.8.C5.M585 no.JP 03-006 |
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