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Are CMIP5 Models Better than CMIP3 Models in Simulating Precipitation over East Asia?

机译:在模拟东亚的降水方面,CMIP5模型是否优于CMIP3模型?

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The performance of climate models participating in phases 5 and 3 of the Coupled Model Intercomparison Project (CMIP5 and CMIP3, respectively) is evaluated and compared with respect to precipitation over East Asia (20 degrees-50 degrees N, 110 degrees-150 degrees E). The target period covers the 20 years from 1981 through 2000. The CMIP5 and CMIP3 models underestimate precipitation amounts over East Asia in the warmer season (May-September), while they overestimate precipitation amounts in the colder season (October-April). Both sets of models have some difficulty in simulating the seasonal march of the rainy season over China, the Korean Peninsula, and Japan, and they also underestimate the precipitation intensity over East Asia. Nevertheless, the CMIP5 models show a higher reproducibility of precipitation over East Asia than the CMIP3 models with respect to the geographical distribution of precipitation throughout the year, seasonal march of the rainy season, and extreme precipitation events. Models with a higher reproducibility of annual precipitation tend to show a higher reproducibility of precipitation intensity for both the CMIP5 and CMIP3 models. Correlation analysis using all of the CMIP5 and CMIP3 models reveals that models with higher horizontal resolution tend to perform better than those with a lower resolution. The advantage of the CMIP5 models over the CMIP3 models in the simulation of the East Asian climate can be partly attributed to the improved representation of the west Pacific subtropical high in the CMIP5 models, especially during the summer.
机译:评估并比较了耦合模型比较项目的第5和第3阶段(分别为CMIP5和CMIP3)的气候模型的性能,并比较了东亚地区(北纬20度至50度,东经110度至150度)的降水量。目标期涵盖从1981年到2000年的20年。CMIP5和CMIP3模型低估了暖季(5月至9月)中东亚的降水量,而高估了冷季(10月至4月)的降水量。这两套模型都难以模拟中国,朝鲜半岛和日本的雨季的季节性行进,并且它们也低估了东亚的降水强度。然而,就全年降水的地理分布,雨季的季节性进行和极端降水事件而言,CMIP5模型显示出的东亚地区降水重现性高于CMIP3模型。对于CMIP5和CMIP3模型,年降水重现性较高的模型往往表现出较高的降水强度重现性。使用所有CMIP5和CMIP3模型的相关性分析表明,水平分辨率较高的模型往往比分辨率较低的模型表现更好。在东亚气候模拟中,CMIP5模型相对于CMIP3模型的优势可以部分归因于CMIP5模型中西太平洋副热带高压代表的改进,尤其是在夏季。

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