摘要:Land use and land cover changes affect the partitioning of latent and sensible heat, which
impacts the broader climate system. Increased latent heat flux to the atmosphere has a
local cooling influence known as 'evaporative cooling', but this energy will be released back
to the atmosphere wherever the water condenses. However, the extent to which local
evaporative cooling provides a global cooling influence has not been well characterized.
Here, we perform a highly idealized set of climate model simulations aimed at
understanding the effects that changes in the balance between surface sensible and latent
heating have on the global climate system. We find that globally adding a uniform 1 W m − 2 source of latent heat flux along with a uniform 1 W m − 2 sink of sensible heat leads to a decrease in global mean surface air temperature of
0.54 ± 0.04 K. This occurs largely as a consequence of planetary albedo increases associated
with an increase in low elevation cloudiness caused by increased evaporation.
Thus, our model results indicate that, on average, when latent heating replaces
sensible heating, global, and not merely local, surface temperatures decrease.