Measurements of precipitation isotopic composition have been conducted on a daily basis for one year at Bomi, southeast Tibetan Plateau, an area affected by the interaction of southwest monsoon, the westerlies and Tibetan high pressure systems, and at Lhasa, situated West of Bomi. The measured isotope signals are analyzed both on an event basis and on a seasonal scale using available meteorological information and air mass trajectories. The processes driving daily and seasonal isotopic variability are investigated using multi-decadal climate simulations forced by 20th century boundary conditions and conducted with two different isotopic atmospheric general circulation models (LMDZiso and ECHAM4iso). Both models use specific nudging techniques to mimic observed atmospheric circulation fields. The models simulate a wet and cold bias on the Tibetan Plateau together with a dry bias in its southern part. A zoomed LMDZ simulation conducted with ~50 km local spatial resolution dramatically improves the results. Simulated water isotope fields are compared with our new data and with previous observations. Here we focus in particular on relationships between the water isotopes and climate variables on an event and seasonal scale and in terms of spatial and altitudinal isotopic gradients. Enhancing the spatial resolution is crucial for improving the simulation of the precipitation isotopic composition. Simulated back trajectories from LMDZ demonstrate the difference of precipitation δ18O between Bomi and Lhasa results from the different moisture origin.
AGU Fall Meeting Abstracts
- Pub Date:
- December 2010
- 1620 GLOBAL CHANGE / Climate dynamics;
- 1626 GLOBAL CHANGE / Global climate models