Journal
WATER
Volume 13, Issue 11, Pages -Publisher
MDPI
DOI: 10.3390/w13111477
Keywords
precipitation; climate change; Sen's estimator; Mann-Kendall; Wadi Cheliff basin
Categories
Funding
- MDPI
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This study evaluated the spatiotemporal variability of precipitation in the Wadi Cheliff basin in Algeria, analyzing the annual variation, trend, and possible change points. The results revealed spatial differences in precipitation variability and trends between the southern and northern sides of the basin, with a negative trend in annual rainfall and potential change points identified between 1980 and 1985.
In the context of climate variability and hydrological extremes, especially in arid and semi-arid zones, the issue of natural risks and more particularly the risks related to rainfall is a topical subject in Algeria and worldwide. In this direction, the spatiotemporal variability of precipitation in the Wadi Cheliff basin (Algeria) has been evaluated by means of annual time series of precipitation observed on 150 rain gauges in the period 1970-2018. First, in order to identify the natural year-to-year variability of precipitation, for each series, the coefficient of variation (CV) has been evaluated and spatially distributed. Then, the precipitation trend at annual scale has been analyzed using two nonparametric tests. Finally, the presence of possible change points in the data has been investigated. The results showed an inverse spatial pattern between CV and the annual rainfall, with a spatial gradient between the southern and the northern sides of the basin. Results of the trend analysis evidenced a marked negative trend of the annual rainfall (22% of the rain gauges for a significant level equal to 95%) involving mainly the northern and the western-central area of the basin. Finally, possible change points have been identified between 1980 and 1985.
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