Impact of CO2 doubling on the Asian summer monsoon: Robust versus model-dependent responses

The possible impact of anthropogenic climate change on the Asian summer mon soon is investigated in several time-slice experiments using prescribed sea -surface temperature (SST) and sea-ice anomalies. The study is carried out with four different atmospheric general circulation models (GCMs), each bei ng involved in two pairs of experiments differing only by the treatment of the land surface hydrology. The objective is to assess the robustness of th e simulated climate change, and its possible sensitivity to the land surfac e scheme. Despite the use of identical SST anomalies, the four GCMs do not predict similar monsoon responses on the regional scale. All models produce a stronger warming over the Asian continent than over the Indian Ocean, bu t this warming is not a good predictor of the monsoon response to increased CO2 level. There is a significant spread in the summer precipitation anoma lies despite a general weakening of the monsoon circulation, showing that t he response of the monsoon rainfall is not solely related to the changes in the large-scale dynamics. In a warmer climate, the monsoon precipitation c an increase despite a weakening of the monsoon flow, due to an increase in the atmospheric water content. For decades to come, the increase in the atm ospheric water content could be more important than the increase in the lan d-sea thermal gradient for understanding the evolution of the monsoon preci pitation. Though it does not represent a major source of uncertainty, the t reatment of the surface hydrology is liable to affect significantly the reg ional response of the monsoon to CO2 doubling. A slight change in evapotran spiration is enough to induce a significant change in precipitation. A simp le analysis of the regional water budget indicates that this sensitivity is not only related to changes in the horizontal transport of water vapor, bu t also to changes in the precipitation efficiency, which depends on the tre atement of the land surface hydrology.