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Influences of convective parameterization schemes on the Simulation of air-sea phase relationship in East Asian summer monsoon region

机译:对流参数化方案对东亚夏季风区域海气相位关系模拟的影响

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In this study, the sensitivities of convective parameterization schemes(CPS) to the air-sea phase relationship in the east Asian summer monsoon region are investigated using a coupled regional climate model RegCM-POM. The east Asian summer monsoon climate from May to October in 1998 are simulated with two different CPSs, namely, the Grell scheme and the MIT-Emanuel scheme(EMU). Then the simulated precipitation-SST phase relationship and the sea surface heat flux(SSHF)-SST phase relationship derived by the Grell simulation and EMU simulation are compared, finding that the EMU simulation shows a superiority to the Grell simulation, especially in the south China sea(SCS) and the East China sea(ECS), indicating a more reasonable amplitude and phase of the lead lag precipitation-SST and SSHF-SST correlation coefficients. The reason for this phenomenon lies in that the convective precipitation(CP) produced by EMU scheme is more realistic, and the simulated SST is more coherent with the observation which benefits from the EMU through the interaction of the convective process and the oceanic process.
机译:在这项研究中,对流参数化方案(CPS)对东亚夏季风区域的海-气相位关系的敏感性使用耦合的区域气候模型RegCM-POM进行了研究。利用两种不同的CPS模拟了1998年5月至10月的东亚夏季风气候,即Grell方案和MIT-Emanuel方案(EMU)。然后比较了由Grell模拟和EMU模拟得到的模拟降水-SST相位关系和海表热通量(SSHF)-SST相位关系,发现EMU模拟显示出优于Grell模拟的优势,特别是在中国南方海(SCS)和东海(ECS),表明铅滞后降水-SST和SSHF-SST相关系数的幅度和相位更加合理。产生这种现象的原因在于,EMU方案产生的对流降水(CP)更为真实,而模拟的海温与通过对流过程和海洋过程相互作用而得益于EMU的观测更加一致。

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