Guest Post by Willis Eschenbach
I got to thinking again about the question of evaporation and rainfall. I wrote about it here a few years ago. Short version—when the earth’s surface gets warmer, we get more evaporation and thus more rainfall. Since what comes down must go up, we can use the Tropical Rainfall Measuring Mission (TRMM) satellite rainfall data to calculate the corresponding rainfall-related evaporation.
From that TRMM data, we can also calculate how much the evaporation changes with additional warming. Figure 1 shows the trends in evaporative cooling with respect to temperature, in units of W/m2 of additional evaporative cooling per degree of additional warming
Figure 1. Amount of additional evaporative cooling per additional degree of temperature. Red areas have the greatest rainfall and thus the greatest evaporative cooling. The area of greatest cooling is the Inter-Tropical Convergence Zone (ITCZ) just above the Equator. Note that this includes…
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