利用加性逻辑回归模型和 ECMWF 再预报预报大型冰雹和闪电

Francesco Battaglioli, P. Groenemeijer, I. Tsonevsky, T. Púčik
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摘要

摘要。利用ERA5再分析的对流参数、欧洲恶劣天气数据库(ESWD)的冰雹报告以及英国气象局到达时间差网络(ATDnet)的闪电观测数据,建立了闪电(ARlig)和大冰雹(ARhail)的加法逻辑回归模型。这些模型得出了特定网格点在特定时间范围内发生闪电和大冰雹的概率。为了探索这种方法在中期预报中的价值,这些模型被应用于欧洲中期天气预报中心(ECMWF)的再预报,为 11 个集合成员重建了概率闪电和大冰雹预报,预报时间从 2008 年到 2019 年,最长可达 228 小时。闪电和大冰雹模式基于不同的预测参数:最不稳定对流可用势能(CAPE)、925-500 hPa 体积切变、混合层混合比、湿球零高度(针对大冰雹)、最不稳定抬升指数、850 和 500 hPa 之间的平均相对湿度、1 小时累积对流降水和 925 hPa 比湿(针对闪电)。首先,我们将不同提前期的闪电和冰雹集合预报与观测到的闪电和冰雹进行了比较,重点是最近的一次冰雹爆发。其次,我们使用 ROC 曲线下面积(AUC)作为验证得分,评估了模型的预测技能与预测提前期的函数关系。该分析表明,ARhail 在最长 60 小时的预报时间内具有很高的预测能力(AUC > 0.95),即使在延长预报时间的情况下,ARhail 也能保持很高的预测能力(在 180 小时的预报时间内,AUC = 0.86)。虽然 ARlig 的预测能力低于 ARhail,但闪电预报在短期(60 h 时的 AUC = 0.92)和中期(180 h 时的 AUC = 0.82)也很娴熟。最后,我们比较了四维冰雹模型与综合参数的性能,如重要冰雹参数(SHP)或 CAPE 与 925-500 hPa 体积切变的乘积(CAPESHEAR)。结果表明,ARhail 在所有提前期均优于 CAPESHEAR,在中短提前期优于 SHP。这些研究结果表明,将加性逻辑回归模型和 ECMWF 集合预报结合起来,可以为欧洲提供高精度的中程冰雹和闪电预报。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Forecasting large hail and lightning using additive logistic regression models and the ECMWF reforecasts
Abstract. Additive logistic regression models for lightning (ARlig) and large hail (ARhail) were developed using convective parameters from the ERA5 reanalysis, hail reports from the European Severe Weather Database (ESWD), and lightning observations from the Met Office Arrival Time Difference network (ATDnet). The models yield the probability of lightning and large hail in a given timeframe over a particular grid point. To explore the value of this approach to medium-range forecasting, the models were applied to the European Centre for Medium Range Weather Forecasts (ECMWF) reforecasts to reconstruct probabilistic lightning and large hail forecasts for 11 ensemble members, from 2008 to 2019 and for lead times up to 228 h. The lightning and large hail models were based on different predictor parameters: most unstable convective available potential energy (CAPE), 925–500 hPa bulk shear, mixed layer mixing ratio, wet bulb zero height (for large hail), most unstable lifted index, mean relative humidity between 850 and 500 hPa, 1 hourly accumulated convective precipitation and specific humidity at 925 hPa (for lightning). First, we compared the lightning and hail ensemble forecasts for different lead times with observed lightning and hail focusing on a recent hail outbreak. Second, we evaluated the predictive skill of the model as a function of forecast lead time using the area under the ROC curve (AUC) as a validation score. This analysis showed that ARhail has a very high predictive skill (AUC > 0.95) for a lead time up to 60 h. ARhail retains a high predictive skill even for extended forecasts (AUC = 0.86 at 180 h lead time). Although ARlig exhibits a lower predictive skill than ARhail, lightning forecasts are also skilful both in the short term (AUC = 0.92 at 60 h) and in the medium range (AUC = 0.82 at 180 h). Finally, we compared the performance of the 4-dimensional hail model with that of composite parameters such as the significant hail parameter (SHP) or the product of CAPE and the 925–500 hPa bulk shear (CAPESHEAR). Results show that ARhail outperforms CAPESHEAR at all lead times and SHP at short-to-medium lead times. These findings suggests that the combination of additive logistic regression models and ECMWF ensemble forecasts can create highly skilful medium-range hail and lightning forecasts for Europe.
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