1000 500 0 GW/degree


Fig. 3.11 Distribution of wind stress work on surface waves (right panel) (mW/m2), and its latitudinal distribution (leftpanel) (Wang and Huang, 2004b).

Fig. 3.16 Conversion rate of mean GPE to eddy GPE through baroclinic instability based on the empirical eddy parameterization of Gent and McWilliams (1990) (mW/m2) (Huang and Wang, 2003).
0 0

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