HydroSciences Montpellier (University Montpellier, CNRS, IRD), 300 Avenue du Professeur Emile Janbreau, 34090, Montpellier, France.
IIHR-Hydroscience & Engineering, The University of Iowa, Iowa City, IA, USA.
Sci Rep. 2022 Nov 7;12(1):18920. doi: 10.1038/s41598-022-23725-5.
River flooding has large societal and economic impacts across Africa. Despite the importance of this topic, little is known about the main flood generating mechanisms in Africa. This study is based on 13,815 flood events that occurred between 1981 and 2018 in 529 catchments. These flood events are classified to identify the different flood drivers: excess rains, long rains and short rains. Out of them, excess rains on saturated soils in Western Africa, and long rains for catchments in Northern and Southern Africa, are the two dominant mechanisms, contributing to more than 75% of all flood events. The aridity index is strongly related to the spatial repartition of the different flood generating processes showing the climatic controls on floods. Few significant changes were detected in the relative importance of these drivers over time, but the rather short time series available prevent a robust assessment of flood driver changes in most catchments. The major implication of these results is to underline the importance of soil moisture dynamics, in addition to rainfall, to analyze the evolution of flood hazards in Africa.
河流洪水泛滥对非洲的社会和经济造成了重大影响。尽管这个话题很重要,但人们对非洲主要的洪水生成机制知之甚少。本研究基于 1981 年至 2018 年期间在 529 个流域发生的 13815 次洪水事件。这些洪水事件被分类以确定不同的洪水驱动因素:过量降雨、长降雨和短降雨。其中,西非饱和土壤上的过量降雨和北非和南非流域的长降雨是两种主要机制,导致超过 75%的所有洪水事件。干旱指数与不同洪水生成过程的空间分布密切相关,显示了洪水的气候控制作用。虽然在不同时间段内,这些驱动因素的相对重要性几乎没有检测到显著变化,但由于可用的时间序列相对较短,大多数流域的洪水驱动因素变化的稳健评估受到阻碍。这些结果的主要意义是强调除了降雨之外,土壤湿度动态对分析非洲洪水灾害演变的重要性。