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Sensitivity of WRF precipitation simulation to the microphysics schemes: Results from the SoWMEX IOP-8 Case

机译:WRF降水模拟对微观物理方案的敏感性:SoWMEX IOP-8案例的结果

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The heavy rainfall event on 14-15 June 2008,also categorized as the IOP-8 case,during the SoWMEX/TiMREX field experiment is investigated in this study.The precipitation simulation results using the WRF (Weather Research and Forecasting)model nested down to 1.67 km are compared with the observations from NCAR S-POL and NCU TEAM-R radars during the Mei-Yu frontal system near Taiwan area.Four dimensional data assimilation (FDDA; nudging relaxation) is used on the coarse grids (with grid sizes of 5,15,and 45 km) to capture the large and synoptic-scale forcings.Four microphysics schemes (including the WSM6,WDM6,Thompson,and Morrison) are chosen to compare the simulated microphysics structures.
机译:本文研究了SoWMEX / TiMREX野外试验期间2008年6月14日至15日的强降雨事件,也被归类为IOP-8案例。使用WRF(天气研究和预报)模型的降水模拟结果可嵌套到与台湾地区附近的梅雨锋系统中的NCAR S-POL和NCU TEAM-R雷达观测到的1.67 km进行了比较。在粗糙网格(网格尺寸为)时使用了四维数据同化(FDDA;微动弛豫)。分别捕获5、15和45 km),以捕获较大的天气天气强迫。选择了四种微物理方案(包括WSM6,WDM6,Thompson和Morrison)比较模拟的微物理结构。

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