Analysis of return periods and return levels of Yearly July–September extreme droughts in the West African Sahel

被引:0
|
作者
Roméo Chamani
David Monkam
Zéphirin Yepdo Djomou
机构
[1] University of Douala,Laboratory of Fundamental Physics, Faculty of Science
[2] University of Yaounde I,Department of Physics, Faculty of Science
[3] University of Douala,Department of Physics, Faculty of Science
[4] National Institute of Cartography,undefined
来源
Climate Dynamics | 2019年 / 52卷
关键词
West African Sahel; Extreme droughts; Peaks-over-threshold; Return periods; Return levels;
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摘要
This paper aims to model the occurrence of Yearly July–September (YJAS) extreme droughts in the West African Sahel (WAS) and to estimate return periods and return levels of these events through stationary peaks-over-threshold model. For this purpose, the historical gridded monthly rainfall data from Climatic Research Unit for the period 1901–2009 were used. The results show that return levels of YJAS dry extremes have increased since 1970, implying that YJAS extreme droughts are consistently more severe after 1970 than they were before. Approximately 62%\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$62\%$$\end{document} of the WAS area in the postchange period of 1971–2009 was dominated by dry spells not longer than 1 year. The dynamics of the YJAS extremes drying trend indicate that the changes at the tails of YJAS dry extreme distribution have contributed to the dry trend in mean YJAS rainfall in the WAS. The estimated 40-year return level of these events based on 1971–2009 period was less than the average of dry extremes of the same period, suggesting that droughts could intensify in the future even though with some amelioration. Such a finding could prove helpful in anticipation of climate risks in this region where adaptive capacities are very low.
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页码:3421 / 3433
页数:12
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