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Ensemble Sensitivity Analysis-Based Ensemble Transform with 3D Rescaling Initialization Method for Storm-Scale Ensemble Forecast

机译:基于集合敏感度分析的集合变换与3D缩放初始化方法进行风暴规模集合预测

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In order to further investigate the influence of ensemble generation methods on the storm-scale ensemble forecast (SSEF) system, a new ensemble sensitivity analysis-based ensemble transform with 3D rescaling (ET_3DR_ESA) method was developed. The Weather Research and Forecasting (WRF) Model was used to numerically simulate a squall line that occurred in the Jianghuai region in China on 12 July 2014. In this study, initial perturbations were generated via ET_3DR_ESA, and the ensemble forecast performance was compared to that of the dynamical downscaling (Down) method and the ensemble transform with 3D rescaling (ET_3DR) method. Results from a set of experiments indicate that ET_3DR_ESA linked to multi-scale environmental fields generates initial perturbations that can not only capture analysis uncertainties, but also match the actual synoptic conditions. Such perturbations produce faster ensemble spread growth, lower root-mean-square error, and a lower percentage of outliers, especially during the peak period of the squall line. In addition, ET_3DR_ESA can effectively reduce the energy dissipation on different scales through the analysis of the power spectrum. Moreover, the intensity and distribution forecasts of heavy rainfall from the ET_3DR_ESA ensemble forecast system were demonstrated to better match the observation. Furthermore, according to results of the relative operating characteristic (ROC) test, Brier score (BS), and equitable threat score (ETS), ET_3DR_ESA significantly improved the forecast skills for heavy rain (15–30 mm/12 h) and extreme rain (30 mm/12 h), which are critical to the realization of accurate storm-scale system precipitation forecasts. In general, these results suggest that ET_3DR_ESA can be effectively applied to SSEF systems.
机译:为了进一步研究集合生成方法对风暴尺度集合预报(SSEF)系统的影响,开发了一种新的基于集合灵敏度分析的3D缩放尺度集合变换​​(ET_3DR_ESA)方法。使用天气研究和预报(WRF)模型对2014年7月12日发生在中国江淮地区的qua线进行了数值模拟。在这项研究中,通过ET_3DR_ESA产生了初始扰动,并将集合的预报性能与该值进行了比较。动态缩减(Down)方法和具有3D缩放的整体变换(ET_3DR)方法的概述。一组实验的结果表明,与多尺度环境场关联的ET_3DR_ESA会产生初始扰动,不仅可以捕获分析不确定性,而且可以匹配实际天气条件。这样的扰动会产生更快的整体传播增长,更低的均方根误差和更低的异常值百分比,尤其是在线的高峰期。此外,ET_3DR_ESA可以通过分析功率谱来有效地减少不同规模的能耗。此外,还证明了ET_3DR_ESA总体预报系统的强降雨强度和分布预报与观测值更好地吻合。此外,根据相对运行特征(ROC)测试,布莱尔得分(BS)和公平威胁得分(ETS)的结果,ET_3DR_ESA显着提高了大雨(15-30 mm / 12 h)和极端降雨的预报技能(> 30 mm / 12 h),这对于实现准确的风暴规模系统降水预报至关重要。通常,这些结果表明ET_3DR_ESA可以有效地应用于SSEF系统。

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