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Linear relation between convective cloud base height and updrafts and application to satellite retrievals

机译:对流云底高度与上升气流之间的线性关系及其在卫星反演中的应用

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Measurements done by the Department of Energy/Atmospheric Radiation Measurement program, at the Southern Great Plains, the central Amazon, and on board an oceangoing ship between Honolulu and Los Angeles, show that updraft speeds measured by Doppler lidar and 95GHz cloud radar are tightly linearly correlated with cloud base height (H-b). Based on these relationships, a method of satellite retrieval of maximum (W-max) and cloud base (W-b) updraft speeds in cloud topped planetary boundary layer is proposed. H-b, as an input for updraft estimation, is obtained from satellite-retrieved cloud base temperature in combination with 2m air temperature derived from European Centre for Medium-Range Weather Forecasts reanalysis. Validation by the lidar and radar measurements shows good agreements for the satellite retrieval of W-max with RMSE (root-mean-square error)=0.38m/s and MAPE (mean absolute percentage error)=19% and W-b with RMSE=0.34m/s and MAPE=21%.
机译:由能源/大气辐射测量计划部在南部大平原,亚马逊中部以及檀香山和洛杉矶之间的一艘远洋船上进行的测量表明,多普勒激光雷达和95GHz云雷达测得的上升气流速度呈线性紧密关系与云底高度(Hb)相关。基于这些关系,提出了一种在卫星云顶行星边界层中获取卫星最大(W-max)和云基(W-b)上升速度的卫星的方法。 H-b,作为上升气流估算的输入,是从卫星ret回的云底温度与2m气温的组合中得出的,该气温是从欧洲中距离天气预报中心重新分析得出的。激光雷达和雷达测量结果的验证表明,对于卫星最大的W-max卫星检索,RMSE(均方根误差)= 0.38m / s,MAPE(平均绝对百分比误差)= 19%,Wb的RMSE = 0.34 m / s和MAPE = 21%。

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