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WRF simulation for a heavy rainfall event over the huaihe river basin, China — An evaluation using remote sensing and ground observations

机译:淮河流域中国强降雨事件的WRF模拟—基于遥感和地面观测的评估

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Aiming to simulate a heavy rainfall process with higher spatiotemporal resolution over the Huaihe River Basin (HRB), the Weather Research and Forecasting (WRF) Model was adopted with a nested domain setting the spatial resolutions as 15km and 5km, respectively. TRMM 3B42 estimates and meteorological station observations were collected to evaluate the WRF simulation performance on precipitation in daily and weekly time scale. The WRF predicted rainfall with a spatial resolution of 5km was tested to be slightly higher than that with 15km. Compared to the ground observations, the correlation coefficient scores of WRF daily accumulated precipitations reached up to 0.70. Contrasting with TRMM estimates, the threat scores of the heavy rainfall with a threshold exceeded 50 mm reached up to 0.215 and 0.434, respectively in the daily and weekly time scales which demonstrated the feasibility of the TRMM 3B42 precipitation for evaluating the WRF performance for heavy precipitation simulations.
机译:为了模拟具有较高时空分辨率的淮河流域(HRB)的强降雨过程,采用了嵌套域将天气分辨率分别设置为15km和5km的天气研究和预报(WRF)模型。收集了TRMM 3B42估计值和气象站观测值,以评估WRF在每日和每周时间尺度上对降水的模拟性能。 WRF预测的空间分辨率为5 km的降雨量要略高于15 km的降雨量。与地面观测相比,WRF日累积降水量的相关系数得分达到0.70。与TRMM估计相反,阈值超过50 mm的强降雨的威胁评分在每日和每周的时间尺度上分别达到0.215和0.434,这证明了TRMM 3B42降水评估强降水WRF性能的可行性。模拟。

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