An analysis is provided to explain the sensitivity of regional climate
to tropical deforestation based on an intermediate-level mechanistic
model for land-atmosphere interaction. The analytical framework is mad
e possible by the fact that feedback to local thermodynamics from larg
e-scale dynamics is negligible, so the determining processes take plac
e in situ. The analytical method accurately reproduces the intermediat
e-level numerical model results for an albedo change scenario and furt
her provides insight into the mechanisms, A three-way balance among la
rge-scale adiabatic cooling, moist convective heating, and radiative h
eating allows two positive feedback mechanisms, moisture convergence f
eedback and evaporation feedback, that give rise to the high sensitivi
ty. The analysis also highlights a deficiency in column energy balance
commonly used in tropical simple models, which results in a sensitivi
ty that is likely too high. In light of these findings, some immediate
needs for further advancing understanding of the problem are discusse
d.