Deriving Severe Hail Likelihood from Satellite Observations and Model Reanalysis Parameters using a Deep Neural Network

B. Scarino, K. Itterly, Kristopher Bedka, C. Homeyer, J. Allen, S. Bang, Daniel J. Cecil
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Abstract

Geostationary satellite imagers provide historical and near-real-time observations of cloud top patterns that are commonly associated with severe convection. Environmental conditions favorable for severe weather are thought to be represented well by reanalyses. Predicting exactly where convection and costly storm hazards like hail will occur using models or satellite imagery alone, however, is extremely challenging. The multivariate combination of satellite-observed cloud patterns with reanalysis environmental parameters, linked to Next Generation Weather Radar- (NEXRAD-) estimated Maximum Expected Size of Hail (MESH) using a deep neural network (DNN), enables estimation of potentially severe hail likelihood for any observed storm cell. These estimates are made where satellites observe cold clouds, indicative of convection, located in favorable storm environments. We seek an approach that can be used to estimate climatological hailstorm frequency and risk throughout the historical satellite data record. Statistical distributions of convective parameters from satellite and reanalysis show separation between non-severe/severe hailstorm classes for predictors including overshooting cloud top temperature and area characteristics, vertical wind shear, and convective inhibition. These complex, multivariate predictor relationships are exploited within a DNN to produce a likelihood estimate with a critical success index of 0.511 and Heidke skill score of 0.407, which is exceptional among analogous hail studies. Furthermore, applications of the DNN to case studies demonstrate good qualitative agreement between hail likelihood and MESH. These hail classifications are aggregated across an 11-year GOES-12/13 image database to derive a hail frequency and severity climatology, which denotes the Central Plains, the Midwest, and northwestern Mexico as being the most hail-prone regions within the domain studied.
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利用深度神经网络从卫星观测和模式再分析参数推导强冰雹可能性
地球同步卫星成像仪提供了通常与强对流有关的云顶模式的历史和近实时观测。人们认为重新分析很好地反映了有利于恶劣天气的环境条件。然而,仅使用模型或卫星图像准确预测对流和冰雹等代价高昂的风暴灾害将发生的地方是极具挑战性的。卫星观测到的云型与再分析环境参数的多元组合,与下一代天气雷达(NEXRAD)结合,使用深度神经网络(DNN)估计最大预期冰雹大小(MESH),可以估计任何观测到的风暴单体的潜在严重冰雹可能性。这些估计是在卫星观测到位于有利的风暴环境中指示对流的冷云时作出的。我们寻求一种方法,可用于估计整个历史卫星数据记录的气候冰雹频率和风险。来自卫星和再分析的对流参数的统计分布显示非严重/严重冰雹等级之间的分离,包括超调云顶温度和面积特征、垂直风切变和对流抑制。在DNN中利用这些复杂的多变量预测关系来产生具有0.511关键成功指数和0.407 Heidke技能分数的可能性估计,这在类似的冰雹研究中是例外的。此外,DNN在案例研究中的应用表明,冰雹可能性和MESH之间具有良好的定性一致性。这些冰雹分类是在一个11年的GOES-12/13图像数据库中汇总的,以得出冰雹频率和严重程度气候学,其中表明中部平原,中西部和墨西哥西北部是研究领域内最容易发生冰雹的地区。
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