Regional and global climate response to aerosol and GHG forcings
We employ the state-of-the-art Earth system models and regional climate models (e.g. MPAS, CESM, MMF, WRF-Chem) as well as long-term climate records (satellite products, reanalysis data) to understand the physical pathways for aerosol and GHG effects on regional and global climate and project their future responses. Foci are put on the climate extremes and large-scale and mesoscale interactions.
Air Cleaning Suppressed Winter Extremes
Anthropogenic aerosol emissions decreased over North America and Europe but increased over Asia since the 1970s. We revealed that this aerosol forcing caused jet stream winds to shift poleward over the Atlantic, decreasing planetary wave activity and partially inhibiting extreme winter weather over northern Eurasia. It stresses the importance of anthropogenic aerosols and their spatiotemporal variability in assessing the drivers of extreme weather in historical and future climate.
Attribution of Extreme Precipitation in China
To reconcile the influence of aerosols and greenhouse gases on precipitation extremes, we implemented an in-situ diagnostics of precipitation probability distribution function in CAM5. A series of model simulations suggested aerosols primarily account for the light precipitation suppression in Eastern China. In contrast, greenhouse gas effects mainly enhance tropical precipitation extremes via dynamical pathways.