What if we’ve been looking at the climate, well, incompletely? What if there’s another side to climate change, one less concerned with what we put in the atmosphere than what we do to the land, a side which, despite four decades of climate education, has yet to be explained to us?

Scientifically speaking, there is. Scientists call it “land change,” a characteristically neutral term for the not-so-neutral ways humans alter landscapes, through things like logging, agriculture, road building and urban/suburban sprawl. By disturbing land this way, we disturb the land’s ability to hold and cycle water, and that affects climate, particularly on a local and regional level.

Though we tend to think of climate in terms of carbon, water is in fact the primary medium of Earth’s heat dynamics, perhaps not surprising on this 71% water planet. Water not only has the highest heat capacity around, it’s also a shapeshifter, continuously phase-changing between water, vapor and ice, absorbing and releasing heat at each juncture, elegantly distributing heat along the way.

Evaporation, the phase-change from water to vapor, is a cooling process. We’ve all felt it when we sweat. Plants essentially do the same thing when they respire, cooling themselves and their surroundings by releasing water vapor from under their leaves. Trees are the power lifters here, drawing upwards of 150 gallons per day through their roots and out through their leaves, giving an average tree the cooling power of two air conditioning units running all day.1

The vapor, with the heat held latent inside it as a chemical potential, rises until it is high and cold enough to condense back into clouds and rain, at which point the heat is released into the air again, only higher, some of which continues its journey out to space, the rest reentering the system elsewhere…

…click on the above link to read the rest…