Precipitation extremes in Ukraine from 1979 to 2019: climatology, large-scale flow conditions, and moisture sources

E. Agayar, F. Aemisegger, Moshe Armon, Alexander Scherrmann, H. Wernli
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Abstract

Abstract. Understanding extreme precipitation events (EPEs) and their underlying dynamical processes and moisture transport patterns is essential to mitigating EPE-related risks. In this study, we investigate the dynamics of 82 EPEs (≥100 mm d−1) over the territory of Ukraine in the recent decades (1979–2019), of which the majority occurred in summer. The EPEs are identified based on precipitation observations from 215 meteorological stations and posts in Ukraine. The atmospheric variables for the case study analysis of selected EPEs and for climatological composites and trajectory calculations were taken from ERA5 reanalyses. Moisture sources contributing to the EPEs in Ukraine are identified with kinematic backward trajectories and the subsequent application of a moisture source identification scheme based on the humidity mass budget along these trajectories. The large-scale atmospheric circulation associated with EPEs was studied for a selection of representative EPEs in all seasons and with the aid of composites of all events per season. Results show that EPEs in summer occur all across Ukraine, but in other seasons EPE hotspots are mainly in the Carpathians and along the Black Sea and Sea of Azov. All EPEs were associated with a surface cyclone, with most having an upper-level trough, except for the winter events that occurred in situations with very strong westerly jets. Isentropic potential vorticity anomalies associated with EPEs in Ukraine show clear dipole structures in all seasons, however, interestingly with a different orientation of these anomaly dipoles between seasons. The analysis of moisture sources revealed a very strong case-to-case variability and often a combination of local and remote sources. Oceanic sources dominate in winter, but land evapotranspiration accounts for 60 %–80 % of the moisture that rains out in EPEs in the other seasons. Taken together, these findings provide a novel insight into large-scale characteristics of EPEs in Ukraine, a region with a unique geographical setting and with moisture sources as diverse as Newfoundland, the Azores, the Caspian Sea, and the Arctic Ocean.
1979 年至 2019 年乌克兰的极端降水:气候学、大尺度流动条件和水汽来源
摘要。了解极端降水事件(EPEs)及其潜在的动力学过程和水汽输送模式对于降低与极端降水事件相关的风险至关重要。在本研究中,我们调查了最近几十年(1979-2019 年)乌克兰境内发生的 82 次极端降水事件(≥100 mm d-1)的动态变化,其中大部分发生在夏季。这些 EPE 是根据乌克兰 215 个气象站和观测站的降水观测数据确定的。用于选定 EPE 的案例研究分析以及气候学合成和轨迹计算的大气变量来自 ERA5 再分析。通过运动后向轨迹和随后应用基于这些轨迹的湿度质量预算的湿度源识别方案,确定了造成乌克兰 EPE 的湿度源。研究了与 EPEs 相关的大尺度大气环流,选择了所有季节中具有代表性的 EPEs,并对每个季节的所有事件进行了合成。结果表明,夏季的 EPE 发生在整个乌克兰,但在其他季节,EPE 的热点地区主要在喀尔巴阡山脉、黑海和亚速海沿岸。所有 EPE 都与地面气旋有关,其中大部分都有高层低槽,只有冬季事件是在有很强的西风喷流的情况下发生的。与乌克兰 EPE 相关的等熵位涡度异常在所有季节都显示出明显的偶极结构,但有趣的是,这些异常偶极的方向在不同季节有所不同。对水汽源的分析表明,不同情况下的水汽源差异很大,而且往往是本地水汽源和远程水汽源的结合。海洋水汽来源在冬季占主导地位,但在其他季节,陆地蒸发造成的水汽占降雨量的 60%-80% 。乌克兰地理环境独特,水汽来源多种多样,包括纽芬兰、亚速尔群岛、里海和北冰洋。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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