Influence of land evapotranspiration on climate variations

A coupled numerical model of the global atmosphere with a qualified biosphere(GOALS/LASG) has been used to assess the nature of the physical mechanisms for land-atmos-phere interactions, and the impacts of the Asian/North American land-surface evapotranspirationon the regional and global climate. This sensitivity study suggests that the simulated climate wouldbe relatively sensitive to land surface evapotranspiration, especially over the Asian regions. Theremoval of evapotranspiration in Asia would create a warmer and drier climate to a certain degree.Furthermore, the surface evapotranspiration anomalies would make a substantial contribution tothe formation and variation of subtropical anticyclones through the changes in monsoon precipita-tion and the β-effect, but also make a large contribution to the variations of the atmosphericcirculation in the Northern Hemisphere and even the globe. Therefore, besides the traditionalperception that we have generally emphasized on the influence of subtropical anticyclonesactivities on the boreal summer precipitation over the regions of eastern China, the surfaceevapotranspiration anomalies, however, also have substantial impacts on the subtropicalanticyclones through the changes in monsoon precipitation. For this reason, the variation in theinternal heating sources of the atmosphere caused by the land surface evapotranspiration and thevapor phase change during the boreal summer is an important external factor forcing the weatherand

A coupled numerical model of the global atmosphere with a qualified biosphere (GOALS/LASG) has been used to assess the nature of the physical mechanisms for land-atmosphere interactions, and the impacts of the Asian/North American land-surface evapotranspiration on the regional and global climate. This sensitivity study suggests that the simulated climate would be relatively sensitive to land surface evapotranspiration, especially over the Asian regions. The removal of evapotranspiration in Asia would create a warmer and drier climate to a certain degree. Furthermore, the surface evapotranspiration anomalies would make a substantial contribution to the formation and variation of subtropical anticyclones through the changes in monsoon precipitation and the β -effect, but also make a large contribution to the variations of the atmospheric circulation in the Northern Hemisphere and even the globe. Therefore, besides the traditional perception that we have generally emphasized on the influence of subtropical anticyclones activities on the boreal summer precipitation over the regions of eastern China, the surface evapotranspiration anomalies, however, also have substantial impacts on the subtropical anticyclones through the changes in monsoon precipitation. For this reason, the variation in the internal heating sources of the atmosphere caused by the land surface evapotranspiration and the vapor phase change during the boreal summer is an important external factor forcing the weather and climate.