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The Simulation of East Asian Summer Monsoon Precipitation With a Regional Ocean-Atmosphere Coupled Model

机译:利用区域海洋气氛耦合模型仿真东亚夏季季风降水

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A fully coupled regional ocean-atmosphere model was used to simulate the East Asian summer monsoon (EASM) precipitation. This coupled regional climate modeling system consists of the Regional Spectral Model (RSM) for the atmosphere and the Regional Ocean Modeling System for the ocean. The ocean and atmosphere share the same horizontal grid resolution. The coupled model is forced by the National Centers for Environmental Prediction-Department of Energy (R-2) global atmospheric reanalysis and Simplified Ocean Data Assimilation global oceanic reanalysis through the lateral boundary. This study examines EASM surface oceanic state and precipitation variability from a 22-year (1984-2005) integration with a horizontal resolution of 40 km. The coupled model captures the features of observed sea surface temperature (SST), sea surface height, and ocean surface currents. Compared with the control run of the uncoupled RSM forced with observed SSTs, the coupled model shows more realistic simulation of the EASM precipitation climatology. The coupled model also improves the simulation of precipitation variability at both interannual and intraseasonal scales. It is the coupled model, not the uncoupled RSM, represents the observed SST-precipitation and SST-evaporation relationships. This study indicates that the ocean-atmosphere coupling is essential for model simulations of the EASM precipitation.
机译:采用完全耦合的区域海洋气氛模型来模拟东亚夏季季风(EASM)降水。这种耦合的区域气候建模系统包括大气的区域光谱模型(RSM)和海洋区域海洋建模系统。海洋和大气层分享相同的水平网格分辨率。耦合模型由国家环境预测 - 能源部(R-2)全球大气再分析和通过横向边界的简化海洋数据同化全球海洋再分析的耦合模型。本研究审查了22年(1984-2005)集成的EASM表面海洋状态和降水可变性,水平分辨率为40公里。耦合模型捕获观察海面温度(SST),海面高度和海洋表面电流的特征。与观察到的SST的未耦合RSM的控制运行相比,耦合模型表明了EASM降水气流的更现实的模拟。耦合模型还提高了持续耕作和季节性尺度的降水变异性的模拟。它是耦合模型,而不是未耦合的RSM,表示观察到的SST-沉淀和SST蒸发关系。本研究表明海洋气氛耦合对于EASM降水的模型模拟至关重要。

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