The relative contribution of albedo and evapotranspiration to regional trends in surface temperature  remains unresolved, and may be determined by different mechanisms in different systems, depending on site-specific conditions such as snow coverage, vegetation and soil moisture . For example, the vegetation-albedo feedback mechanism may dominate in the Arctic , while the vegetation- evaporation feedback may drive change in other regions. Actions that increase forest cover across Africa could thus, theoretically, moderate projected future temperature increases , but with potentially negative effects on biodiversity . Soil drying exacerbates atmospheric aridity, which causes more soil drying in a self-reinforcing land-atmosphere feedback that could intensify under RCP8.5 .
IPCC
Climate Change 2022: Impacts, Adaptation and Vulnerability
IPCC Report