A 20-year satellite-reanalysis-based climatology of extreme precipitation characteristics over the Sinai Peninsula

M. Soltani, Bert Hamelers, Abbas Mofidi, Christopher G. Fletcher, Arie Staal, Stefan C. Dekker, P. Laux, J. Arnault, H. Kunstmann, Ties van der Hoeven, Maarten Lanters
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Abstract

Abstract. Extreme precipitation events and associated flash floods caused by synoptic cyclonic systems profoundly impact society and the environment, particularly in arid regions. This study brings forward a satellite-reanalysis-based approach to quantify extreme precipitation characteristics over the Sinai Peninsula (SiP) in Egypt from a statistical–synoptic perspective for the period of 2001–2020. With a multi-statistical approach developed in this research, SiP's wet and dry periods are determined. Using satellite observations of precipitation and a set of derived precipitation indices, we characterize the spatiotemporal variations of extreme rainfall climatologies across the SiP. Then, using the reanalysis datasets, synoptic systems responsible for the occurrence of extreme precipitation events along with the major tracks of cyclones during the wet and dry periods are described. Our results indicate that trends and spatial patterns of the rainfall events across the region are inconsistent in time and space. The highest precipitation percentiles (∼20 mm per month), frequencies (∼15 d per month with rainfall ≥10 mm d−1), standard deviations (∼9 mm month per month), and monthly ratios (∼18 %) are estimated in the northern and northeastern parts of the region during the wet period, especially in early winter; also, a substantial below-average precipitation condition (drier trend) is clearly observed in most parts except for the south. Mediterranean cyclones accompanied by the Red Sea and Persian troughs are responsible for the majority of extreme rainfall events year-round. A remarkable spatial relationship is found between SiP's rainfall and the atmospheric variables of sea level pressure, wind direction, and vertical velocity. A cyclone-tracking analysis indicates that 125 cyclones (with rainfall ≥10 mm d−1) formed within, or transferred to, the Mediterranean basin and precipitated over the SiP during wet periods compared to 31 such cyclones during dry periods. It is estimated around 15 % of cyclones with sufficient rainfall >40 mm d−1 would be capable of leading to flash floods during the wet period. This study, therefore, sheds new light on the extreme precipitation characteristics over the SiP and its association with dominant synoptic-scale mechanisms over the eastern Mediterranean region.
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西奈半岛极端降水特征的20年卫星再分析气候学
摘要天气气旋系统引起的极端降水事件和相关的山洪对社会和环境产生了深刻影响,尤其是在干旱地区。本研究提出了一种基于卫星再分析的方法,从非定常-天气学的角度量化2001-2020年埃及西奈半岛(SiP)的极端降水特征。利用本研究开发的多种统计方法,确定了SiP的丰水期和枯水期。利用卫星降水观测和一组导出的降水指数,我们描述了整个SiP极端降雨气候的时空变化。然后,利用这些分析数据集,描述了导致极端降水事件发生的天气系统,以及雨季和旱季气旋的主要路径。我们的结果表明,该地区降雨事件的趋势和空间格局在时间和空间上是不一致的。最高降水百分位数(~20 毫米/月),频率(~15 每月d,降雨量≥10 毫米 d−1),标准偏差(~9 毫米 每月)和月比率(~18 %) 估计在该地区的北部和东北部潮湿时期,特别是在初冬;此外,除南部外,大部分地区的降水量明显低于平均水平(干燥趋势)。地中海气旋伴随着红海和波斯波谷,是全年极端降雨事件的主要原因。SiP的降雨量与海平面压力、风向和垂直速度等大气变量之间存在显著的空间相关性。反气旋跟踪分析表明,125个气旋(降雨量≥10 毫米 d−1)在地中海盆地内形成或转移到地中海盆地,并在潮湿时期沉积在SiP上,而在干旱时期有31个这样的气旋。估计约为15 % 降雨量大于40的气旋 毫米 d−1能够在雨季引发洪水。因此,这项研究为SiP的极端降水特征及其与地中海东部地区主要天气尺度机制的联系提供了新的线索。
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