中文摘要：

利用观测资料分析了亚洲季风区夏季海陆热力差异的变化特征。在此基础上,采用国际耦合模式比较计划第五阶段（Coupled Model Intercomparison Program 5,CMIP5）20个模式的输出结果,对其进行了模拟评估。结果表明,亚洲季风区夏季陆地上空温度呈下降趋势,海洋上空呈升高趋势,海陆热力差呈减弱趋势。虽然模式模拟的海陆热力差也呈减弱趋势,但陆地和海洋上空温度均呈上升趋势。模式对陆地上空温度趋势模拟较差的原因是对青藏高原上空的温度模拟偏低。进一步分析表明,对海陆热力差异模拟相对较好的模式对亚洲季风系统模拟较好,而较差的模式对亚洲季风系统模拟也较差。

英文摘要：

Monsoons are one of the most active members of the global climate system, and the land-sea thermal contrast is the main reason for the establishment and continuity of monsoons.At present,the CMIP5 climate coupling model, which has made significant improvements in the physical process, carbon cycle, etc., is an important tool by which to carry out research regarding climate variability and change.The characteristics of the land-sea thermal contrast in the 20th century and how the CMIP5 modes have simulated it are problems which are worthy of study. In this study,observations from NCEP/NCAR and ERA-40 are used to contrast and analyze the features of summer land-sea thermal contrast over the Asian monsoon region, and to define the land-sea thermal contrast index. The results indicate that the temperature over land decreased, while that over sea increased, and the contrast tended to decrease.On this basis ,the model simulations given by the 20 climate models of historical simulations from Phase 5 of the Coupled Model Inter-comparison Project（CMIP5） are used for comparison with observation analysis.Both the best and worst models in the RCP4.5 scenario are selected for forecasting.The main results of the study are as follows： （ 1 ） The observation data show that the average temperature of the upper-middle troposphere had a remarka- ble trend over the Asian monsoon region from 1955 to 2005 ,namely the temperature over land decreased and that over sea increased.According to the selected area,we define a land index, sea index and land-sea thermal contrast index.These present a large rate of inter-annual change;the land-sea thermal contrast index reduced;and the land- sea thermal contrast index was able to reflect the features of the difference between strong and weak monsoons. The NCEP is consistent with the ERA-40,yet the NCEP has an obvious linear trend. （2） The CMIP5 models have a better simulation performance regarding the climate condition of the zonalwind field and height field in 500 hPa and 200 hPa,y