Improving seasonal predictions of German Bight storm activity

Daniel Krieger, S. Brune, J. Baehr, Ralf Weisse
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Abstract

Abstract. Extratropical storms are one of the major coastal hazards along the coastline of the German Bight, the southeastern part of the North Sea, and a major driver of coastal protection efforts. However, the predictability of these regional extreme events on a seasonal scale is still limited. We therefore improve the seasonal prediction skill of the Max Planck Institute Earth System Model (MPI-ESM) large-ensemble decadal hindcast system for German Bight storm activity (GBSA) in winter. We define GBSA as the 95th percentiles of three-hourly geostrophic wind speeds in winter, which we derive from mean sea-level pressure (MSLP) data. The hindcast system consists of an ensemble of 64 members, which are initialized annually in November and cover the winters of 1960/61–2017/18. We consider both deterministic and probabilistic predictions of GBSA, for both of which the full ensemble produces poor predictions in the first winter. To improve the skill, we observe the state of two physical predictors of GBSA, namely 70 hPa temperature anomalies in September, as well as 500 hPa geopotential height anomalies in November, in areas where these two predictors are correlated with winter GBSA. We translate the state of these predictors into a first guess of GBSA and remove ensemble members with a GBSA prediction too far away from this first guess. The resulting subselected ensemble exhibits a significantly improved skill in both deterministic and probabilistic predictions of winter GBSA. We also show how this skill increase is associated with better predictability of large-scale atmospheric patterns.
改进对德国湾风暴活动的季节性预测
摘要外热带风暴是北海东南部德国湾沿岸的主要海岸灾害之一,也是海岸保护工作的主要驱动力。然而,这些区域性极端事件的季节预测能力仍然有限。因此,我们改进了马克斯-普朗克研究所地球系统模式(MPI-ESM)大集合十年期后报系统对冬季德国港湾风暴活动(GBSA)的季节预测能力。我们将 GBSA 定义为冬季三小时地转风速的第 95 百分位数,该数据来自平均海平面气压(MSLP)数据。后报系统由 64 个成员组成,每年 11 月初始化,涵盖 1960/61-2017/18 年冬季。我们同时考虑了确定性和概率性的 GBSA 预测,对于这两种预测,完整的集合在第一个冬季都会产生较差的预测结果。为了提高预测的准确性,我们观测了两个全球平均降水量的物理预测因子的状态,即 9 月的 70 hPa 温度异常和 11 月的 500 hPa 位势高度异常,这两个预测因子与冬季全球平均降水量相关。我们将这些预测因子的状态转化为对全球平均海平面上升率的初步猜测,并删除全球平均海平面上升率预测值与这一初步猜测相差太远的集合成员。由此产生的子选择集合在冬季全球平均降水量的确定性和概率预测方面都表现出明显的技能提高。我们还展示了这种技能的提高是如何与更好地预测大尺度大气模式相关联的。
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