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

被引:1
|
作者
Sambieni, Kevin S. [1 ]
Hountondji, Fabien C. C. [2 ]
Sintondji, Luc O. [3 ]
Fohrer, Nicola [4 ]
Biaou, Severin [5 ]
Sossa, Coffi Leonce Geoffroy [6 ]
机构
[1] Univ Abomey Calavi, West African Sci Serv Ctr Climate Change & Adapted, Grad Res Program Climate Change & Water Resources, BP 526, Abomey Calavi, Benin
[2] Univ Parakou, Fac Agron, BP 123, Parakou, Benin
[3] Univ Abomey Calavi, Inst Natl Eau, BP 4521, Abomey Calavi, Benin
[4] Univ Kiel, Inst Nat Resource Conservat, Dept Hydrol & Water Resources Management, D-24098 Kiel, Germany
[5] Univ Parakou, Fac Agr, Lab Ecol Bot & Biol Vegetate, BP 123, Parakou, Benin
[6] Univ Sci Tech & Technol Bamako USTTB, West African Sci Serv Ctr Climate Change & Adapted, Grad Res Program Climate Change & Agr, BP 423, Bamako, Mali
关键词
adaptation; land cover; rainfall; temperature; Sota catchment; RAINFALL VARIABILITY; IMPACT;
D O I
10.3390/hydrology11030030
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
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 degrees C and 1.2 degrees 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.
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页数:25
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