Seasonal and Regional Biases in CMIP5 Precipitation Simulations
This study provides insight into how CMIP5 climate models perform in simulating summer and winter precipitation at different geographical locations and climate conditions. Precipitation biases in the CMIP5 historical (1951-2005) simulations relative to the Climatic Research Unit (CRU) observations are evaluated over 8 regions exhibiting distinct seasonal hydro-climates: moist tropical (Amazonia and central Africa); monsoonal (southern China); moist continental (central Europe); semi-arid (western United States and eastern Australia); and polar (Siberia and Canada). While the bias and mean quantile bias (MQB, defined herein) reflect no substantial differences in CMIP5 summer and winter precipitation simulations at the global scale, strong seasonality and high inter-model variability are found over the selected moist tropical regions. In the semi-arid regions, high inter-model precipitation variability is also displayed, especially in summer. In Siberia and central Europe, most CMIP5 models underestimate summer precipitation, and overestimate it in winter. Also, the MQB values decrease as the choice of quantile thresholds increase. While the CMIP5 models exhibit similar behaviors in simulating high latitude winter precipitation, they differ substantially in summer simulations for the selected Canadian and Siberian regions. In the monsoonal southern China region, CMIP5 models exhibit large overall precipitation biases in both summer and winter, as well as at higher quantiles. Finally, the CMIP5 precipitation simulations are also tested with the University of Delaware observation data and trend of the results are found to be the same.