climate warming

Nonlocal effects dominate the global mean surface temperature response to the biogeophysical effects of deforestation

Nonlocal effects dominate the global mean surface temperature response to the biogeophysical effects of deforestation

Nonlocal effects: Deforestation influences surface temperature at the location of deforestation (local effects) and elsewhere (nonlocal effects). […] Using simulations in a climate model, we show that deforestation-induced changes in the brightness of the surface influence surface temperature mainly nonlocally and thus may be largely overlooked in observation-based data sets. The simulations show that the nonlocal effects have a larger impact on global average surface temperature than the local effects, independent of how much area is deforested and at which latitude the deforestation takes place.

Posted by Stefan in Allgemein, 0 comments