Abstract

This work aims at characterizing the conditional probability of single or consecutive dry and wet days in West Africa using the first-order Markov chain approach during the monsoon season (June to October). The results show that the probabilities of having a wet day (PW), a wet day preceded by another wet day (PWW) and a wet day preceded by a dry day (PDW) are stronger in regions where the rainfall is maximum (mountain regions). In contrast, the probabilities of having a dry day (PD), a dry day preceded by a wet day (PWD) and a dry day preceded by another dry day (PDD) are lower in the regions with higher precipitation. The seasonal cycle of PWW (PDD) is consistent with that of PW (PD), respectively in Western Sahel and Central Sahel regions. At the interannual timescale, MK test results show that PW and PDW (PD and PDD) exhibit statistically significant increasing (decreasing) trends the Western Sahel and the Central Sahel. Besides, the shorter dry spells (3 days) show statistically significant decreasing trends only in the Western Sahel. The longer dry spells (5, 7 and 10 days) show statistically significant downward trends over the Western and Central Sahel. Wet spells probabilities show non-significant decreasing trends in all sub-domains, except in the Western Sahel for the 10 days spells. Knowledge of theses probabilities will contribute to develop efficient strategies for water resources management and agricultural decision making in West African countries. Key words: Markov chain, rainfall, occurrence, wet spell, dry spell, West Africa.

Highlights

  • Crop yields in West Africa depend mainly on the rainfall regime of the West African Monsoon (WAM)

  • Over the Gulf of Guinea and during the first rainy season (April-June) there is no significant trend observed in mean precipitation during the last thirty years but an increased occurrence of more intense rainfall is noted along the coast in agreement with the rise of the frequency of devastating floods

  • PDD is the probability of having a dry day preceded by another dry day PWW is the probability of having a wet day preceded by another wet day FDD is the number of dry days preceded by another dry day FWW is the number of wet days preceded by another wet day PDW is the probability of having a wet day preceded by a dry day and PWD is the probability of having a dry day preceded by a wet day

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Summary

Introduction

Crop yields in West Africa depend mainly on the rainfall regime of the West African Monsoon (WAM). Bichet and Diedhiou (2018a) found that the recent increase in rainfall over the entire West African Sahel band is mainly due to an increase in the number of wet days with more a strengthening of rainfall intensity in the central part of the subregions (Mali Niger Chad) and an increase of short dry spells occurrences. According to Taylor et al (2017) the recent increase of the number of wet days and of the intensity of rainfall in the Central Sahel is associated with a tripled frequency of extreme Sahelian storms since 1982 due to global warming. During the second rainy season (September-November) there is a significant increase in mean precipitation associated with an increase in precipitation intensity and frequency (Bichet and Diedhiou 2018b)

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