Observational Studies on the Land-air Exchange Processes over the Tibetan Mountain

The Tibetan Plateau (TP) greatly affects climate and environment systems over Asian through the lower atmospheric mass/energy transfer processes. However, the lower atmospheric processes were not clearly understood due to the limitation of observational data, especially over the TP mountain regions. Observations and model simulations suggested a distinguished land-air transfer and vertical structure over the TP mountain regions, which largely differ from those over plateau flat regions. An inhomogeneous distributions are also found in the land-air exchange processes over the whole TP regions, and a new high-resolution dataset are consequently constructed and developed, under the consideration of different TP climate classification.