资源环境科技发展态势分析平台

The impact of convection on the humidity and clouds in the tropical tropopause layer (TTL) during boreal summer 2007 is investigated in simulations of detailed cloud microphysical processes and their effects on the water vapor (H2O) profile along backward trajectories from the 379 K potential temperature (100-hPa pressure) surface. Convective influence is determined by tracing the trajectories through time-dependent fields of satellite-based convective cloud top height. The simulated H2O mixing ratios at the 100-hPa level and cloud occurrence fractions in the middle to upper (16-18 km) TTL exhibit a pronounced maximum over the Asian monsoon region as in observations; these local enhancements are virtually absent in the simulation without convection, indicating that convection is the dominant driver of the localized H2O and cloud maxima in the Asian summer monsoon region. Convection moistens the 100-hPa level by 0.6 ppmv (similar to 15%) averaged over the 10 degrees S-50 degrees N domain and increases tropical (10 degrees S-30 degrees N) mean cloud occurrence in the middle to upper TTL by similar to 170%. Nearly all of the convective enhancements in H2O and clouds are due to the effect of convective saturation; convectively detrained ice crystals have negligible impact. Parcels are most frequently hydrated by deep convection in the southern sector of the Asian monsoon anticyclone and subsequently dehydrated downstream of convection to the west, shifting the locations of final dehydration northwest of the cold temperature region in the northern Tropics. Infrequent, extreme deep convective systems (cloud tops exceeding 380 K) have a disproportionately large effect on TTL humidity and clouds.