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Table 1.

Components of the heat flux difference (W m−2) from 1°S to 2.5°N: ocean forcing of the evaporation Eocean, total atmospheric forcing of the evaporation Eatm, sensible heat flux Hatm, and net downwelling radiation at the surface R.

Components of the heat flux difference (W m−2) from 1°S to 2.5°N: ocean forcing of the evaporation Eocean, total atmospheric forcing of the evaporation Eatm, sensible heat flux Hatm, and net downwelling radiation at the surface R.
Components of the heat flux difference (W m−2) from 1°S to 2.5°N: ocean forcing of the evaporation Eocean, total atmospheric forcing of the evaporation Eatm, sensible heat flux Hatm, and net downwelling radiation at the surface R.
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