Abstract: hanges in moisture as represented by P ? E (precipitation ? evapotranspiration) and the possible causes over the Tibetan Plateau (TP) during 1979?2011 are examined based on the Global Land Data Assimilation Systems (GLDAS) ...

Abstract: thorough understanding of the peak flows under urbanization and climate change?with the associated uncertainties?is indispensable for mitigating the negative social, economic, and environmental impacts from flooding. In ...

Abstract: he performance of 24 GCMs available in the fifth phase of the Coupled Model Intercomparison Project (CMIP5) is evaluated over the eastern Tibetan Plateau (TP) by comparing the model outputs with ground observations for the ...

Abstract: nknown future precipitation is the dominant source of uncertainty for many streamflow forecasts. Numerical weather prediction (NWP) models can be used to generate quantitative precipitation forecasts (QPF) to reduce this ...

Abstract: et precipitation [precipitation minus evapotranspiration (P ? E)] changes between 1979 and 2011 from a high-resolution regional climate simulation and its reanalysis forcing are analyzed over the Tibetan Plateau (TP) and ...

Abstract: ridded daily precipitation, temperature minima and maxima, and wind speed are generated for the northern Tibetan Plateau (NTP) for 1957?2009 using observations from 81 surface stations. Evaluation reveals reasonable quality ...