Understanding hydroclimatic variability in the Sahel and Sudanian zones is critical for improving climate resilience and resource management. This study presents a comparative analysis of drought dynamics in two representative agroecological sites of Mali Cinzana (Sahelian zone) and Kola (Sudanian zone) over the period 1994-2022. Using meteorological data, drought characteristics were assessed through the Standardized Precipitation Index (SPI) and the Standardized Precipitation Evapotranspiration Index (SPEI), complemented by trend detection methods (Mann-Kendall, Sen’s slope) and the Pettitt test for structural breaks. Results reveal marked local divergences despite the geographical proximity of the sites. At Cinzana, rainfall and temperature trends were not statistically significant, although a positive and significant trend in SPEI-12 suggests a tendency toward wetter annual conditions consistent with the Sahelian “regreening” observed since the 1990s. In contrast, Kola exhibited a statistically significant warming, particularly in minimum temperature (+0.057?C/year, p < 0.001), with a breakpoint in 2008 indicating accelerated nighttime warming. Drought indices at Kola revealed significant negative trends in SPI-12, SPEI-6, and SPEI-9, highlighting an intensification of aridification processes. Correlation analysis between SPI and SPEI confirmed that rainfall remains the dominant driver of drought variability at multi-annual scales, while evapotranspiration, amplified by warming, plays an increasingly critical role at seasonal scales. Overall, these findings demonstrate the coexistence of greening and drying trajectories within short geographic distances, reflecting the high spatial heterogeneity of Sahelian climate dynamics. This heterogeneity underscores the need for fine-scale analyses to refine regional climate projections and to design differentiated adaptation strategies for water resource management and agricultural production.
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