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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Dynamical downscaling of historical climate over CORDEX East Asia domain: A comparison of regional ocean-atmosphere coupled model to stand-alone RCM simulations
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Dynamical downscaling of historical climate over CORDEX East Asia domain: A comparison of regional ocean-atmosphere coupled model to stand-alone RCM simulations

机译:CORDEX东亚地区历史气候的动态降尺度:区域海洋-大气耦合模型与独立RCM模拟的比较

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摘要

The FROALS (flexible regional ocean-atmosphere-land system) model, a regional ocean-atmosphere coupled model, has been applied to the Coordinated Regional Downscaling Experiment (CORDEX) East Asia domain. Driven by historical simulations from a global climate system model, dynamical downscaling for the period from1980 to 2005 has been conducted at a uniformhorizontal resolution of 50 km. The impacts of regional air-sea couplings on the simulations of East Asian summer monsoon rainfall have been investigated, and comparisons have been made to corresponding simulations performed using a stand-alone regional climate model (RCM). The added value of the FROALSmodel with respect to the driving global climatemodel was evident in terms of both climatology and the interannual variability of summer rainfall over East China by the contributions of both the high horizontal resolution and the reasonably simulated convergence of the moisture fluxes. Compared with the stand-alone RCM simulations, the spatial pattern of the simulated low-level monsoon flow over East Asia and the western North Pacific was improved in the FROALS model due to its inclusion of regional air-sea coupling. The results indicated that the simulated sea surface temperature (SSTs) resulting from the regional air-sea coupling were lower than those derived directly from the driving global model over the western North Pacific north of 15°N. These colder SSTs had both positive and negative effects. On the one hand, they strengthened the western Pacific subtropical high, which improved the simulation of the summer monsoon circulation over East Asia. On the other hand, the colder SSTs suppressed surface evaporation and favored weaker local interannual variability in the SST, which led to less summer rainfall and weaker interannual rainfall variability over the Korean Peninsula and Japan. Overall, the reference simulation performed using the FROALS model is reasonable in terms of rainfall over the land area of East Asia and will become the basis for the generation of climate change scenarios for the CORDEX East Asia domain that will be described in future reports.
机译:FROALS(灵活的区域性海洋-大气-陆地系统)模型(一种区域性海洋-大气耦合模型)已应用于协调的区域缩减规模试验(CORDEX)东亚领域。在全球气候系统模型的历史模拟的推动下,1980年至2005年期间的动态降尺度以50 km的水平水平分辨率进行。研究了区域海海耦合对东亚夏季风降水模拟的影响,并与使用独立区域气候模型(RCM)进行的相应模拟进行了比较。 FROALS模型相对于驱动全球气候模型的附加值在气候学和华东地区夏季降水的年际变化方面都很明显,这要归功于高水平分辨率和合理模拟的水汽通量的贡献。与独立的RCM模拟相比,FROALS模型改善了模拟的东亚和北太平洋西部低层季风流的空间格局,这是因为它包含了区域海海耦合。结果表明,由区域海气耦合产生的模拟海表温度(SST)低于直接驱动全球模型在北太平洋以北15°N以北的海温。这些较冷的SST既有正面影响,也有负面影响。一方面,他们加强了西太平洋副热带高压,改善了东亚夏季风环流的模拟。另一方面,较冷的SST抑制了表面蒸发,并有利于SST的局部年际变化,这导致了朝鲜半岛和日本夏季降水减少和年际降水变化较弱。总体而言,使用FROALS模型进行的参考模拟就东亚陆地上的降雨而言是合理的,并将成为产生CORDEX东亚地区气候变化情景的基础,这将在以后的报告中进行介绍。

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