Identifying the pathways of extreme rainfall in South Africa using storm trajectory analysis and unsupervised machine learning techniques

Rhys Philips, Katelyn Ann Johnson, A. P. Barnes, Thomas Rodding Kjeldsen
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Abstract

This study has utilised National Oceanic and Atmospheric Administration (NOAA) NCEP/NCAR Reanalysis 1 project meteorological data and the HYSPLIT model to extract the air parcel trajectories for selected historical extreme rainfall events in South Africa. The k-means unsupervised machine learning algorithm has been used to cluster the resulting trajectories, and from this, the spatial origin of moisture for each of the rainfall events has been determined. It has been demonstrated that rainfall events on the east coast with moisture originating from the Indian Ocean have distinctly larger average maximum daily rainfall magnitudes (279 mm) compared to those that occur on the west coast with Atlantic Ocean influences (149 mm) and those events occurring in the central plateau (150 mm) where moisture has been continentally recirculated. Further, this study has suggested new metrics by which the HYSPLIT trajectories may be assessed and demonstrated the applicability of trajectory clustering in a region not previously studied. This insight may in future facilitate improved early warning systems based on monitoring of atmospheric systems, and an understanding of rainfall magnitudes and origins can be used to improve the prediction of design floods for infrastructure design.
利用风暴轨迹分析和无监督机器学习技术确定南非极端降雨的路径
本研究利用美国国家海洋和大气管理局(NOAA)NCEP/NCAR Reanalysis 1 项目气象数据和 HYSPLIT 模型,提取了南非历史上部分极端降雨事件的空气包裹轨迹。使用 k-means 无监督机器学习算法对得到的轨迹进行聚类,并由此确定每个降雨事件的水汽空间来源。研究表明,与受大西洋影响的西海岸降雨事件(149 毫米)和受大陆水汽再循环影响的中部高原降雨事件(150 毫米)相比,受印度洋水汽影响的东海岸降雨事件的平均最大日降雨量(279 毫米)明显更大。此外,这项研究还提出了评估 HYSPLIT 轨迹的新指标,并证明了轨迹聚类在以前未研究过的地区的适用性。这种洞察力可能有助于改进基于大气系统监控的早期预警系统,对降雨量和降雨起源的了解可用于改进基础设施设计中的设计洪水预测。
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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