Climate and Land Use/Land Cover Changes within the Sota Catchment (Benin, West Africa)

Author:

Sambieni Kevin S.1ORCID,Hountondji Fabien C. C.2,Sintondji Luc O.3,Fohrer Nicola4ORCID,Biaou Séverin5ORCID,Sossa Coffi Leonce Geoffroy6

Affiliation:

1. Graduate Research Program on Climate Change and Water Resources, West African Science Service Center on Climate Change and Adapted Land Use, University of Abomey-Calavi, Abomey-Calavi BP 526, Benin

2. Faculté d’Agronomie, Université de Parakou, Parakou BP 123, Benin

3. Institut National de l’Eau, Université d’Abomey-Calavi, Abomey-Calavi BP 4521, Benin

4. Department of Hydrology and Water Resources Management, Institute for Natural Resource Conservation, Kiel University, 24098 Kiel, Germany

5. Laboratoire d’Écologie, de Botanique et de Biologie Végétale, Faculté d’Agronomie, Université de Parakou, Parakou BP 123, Benin

6. Graduate Research Program on Climate Change and Agriculture, West African Science Service Centre on Climate Change and Adapted Land Use (WASCAL), Université des Sciences, des Techniques et des Technologies de Bamako (USTTB), Bamako BP E 423, Mali

Abstract

Climate and land cover changes are key factors in river basins’ management. This study investigates on the one hand 60-year (1960 to 2019) rainfall and temperature variability using station data combined with gridded data, and on the other hand land cover changes for the years 1990, 2005, and 2020 in the Sota catchment (13,410 km2, North Benin, West Africa). The climate period is different from the chosen land use change period due to the unavailability of satellite images. Standardized anomaly index, break points, trend analysis, and Thiessen’s polygon were applied. Satellite images were processed and ground truthing was carried out to assess land cover changes. The analyses revealed a wet period from 1960 to 1972, a dry period from 1973 to 1987, and another wet period from 1988 to 2019. The annual rainfall decreases from the south to the north of the catchment. In addition, rainfall showed a non-significant trend over the study period, and no significant changes were identified between the two normals (1960–1989 and 1990–2019) at catchment scale, although some individual stations exhibited significant trends. Temperatures, in contrast, showed a significant increasing trend over the study period at catchment scale, with significant break points in 1978, 1990, and 2004 for Tmax, and 1989 for Tmin. An increase of 0.4 °C and 1.2 °C is noted, respectively, for Tmax and Tmin between the two normals. The study also revealed increases in agricultural areas (212.1%), settlements (76.6%), waterbodies (2.9%), and baresoil (52%) against decreases in woodland (49.6%), dense forest (42.2%), gallery forest (21.2%), and savanna (31.9%) from 1990 to 2020. These changes in climate and land cover will have implications for the region. Appropriate adaptation measures, including Integrated Water Resources Management and afforestation, are required.

Funder

West African Science Service Center on Climate Change and Adapted Land Use

Publisher

MDPI AG

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