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Biophysical effects of land cover changes in West Africa: a systematic review

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dc.contributor.author Yahaya Seydou, Abdel Nassirou
dc.contributor.author Sy, Souleymane
dc.contributor.author Quesada, Benjamin
dc.contributor.author Bliefernicht, Jan
dc.contributor.author Manevski, Kiril
dc.contributor.author Amekudzi, Leonard K
dc.contributor.author Appiah-Adjei, Emmanuel K
dc.contributor.author Ogunjobi, Kehinde O
dc.contributor.author Traore, Bouba
dc.contributor.author Gyamfi, Charles
dc.contributor.author Kunstmann, Harald
dc.date.accessioned 2026-04-21T09:11:12Z
dc.date.available 2026-04-21T09:11:12Z
dc.date.issued 2025-06-09
dc.identifier.uri http://197.159.135.214/jspui/handle/123456789/1145
dc.description A Publication submitted to the West African Science Service Centre on Climate Change and Adapted Land Use and the Kwame Nkrumah University of Science and Technology, Kumasi, Ghana, in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Climate Change and Land Use en_US
dc.description.abstract West Africa is undergoing rapid agricultural intensification driven by population growth, leading to significant anthropogenic land use and land cover change (LCC), including both deforestation and afforestation. These changes can profoundly affect the regional climate system by altering the surface energy balance, moisture fluxes, and atmospheric circulation, potentially exacerbating the vulnerability of human, ecological, and economic systems. Despite the ability of climate models to simulate LCC impacts, considerable uncertainties remain, particularly in simulations of precipitation and temperature responses. This study provides the first multidisciplinary systematic review of LCC impacts in West Africa. Data from 26 selected publications were eventually synthesized from an initial pool of nearly 6000 studies. Results indicate that deforestation generally contributes to regional warming, with significant historical temperature increases of +0.26 ± 0.12 ◦C and projected increases of +0.88 ± 0.25 ◦C under the future scenarios. Conversely, afforestation could have significantly cooled the climate, lowering temperatures by −0.24 ± 0.14 ◦C historically and −0.22 ± 0.14 ◦C in future scenarios, without even accounting for carbon sequestration. Deforestation decreases regional precipitation by 80 ± 58 mm yr−1 historically and −55 ± 102 mm yr−1 in future scenarios, while large-scale afforestation could substantially reduce droughts with increased precipitation, averaging +40 ± 67 mm yr−1 historically and 80 ± 58 mm yr−1 in future scenarios. These results emphasize the need to integrate LCC-induced climate effects into land-based mitigation strategies, climate policy, and assessment frameworks. en_US
dc.description.sponsorship The Federal Ministry of Research, Technology and Space (BMFTR) en_US
dc.language.iso en en_US
dc.publisher WASCAL en_US
dc.subject Land use en_US
dc.subject Land cover change en_US
dc.subject Deforestation en_US
dc.subject Afforestation en_US
dc.subject Climate modeling en_US
dc.subject PRISMA en_US
dc.subject West Africa en_US
dc.title Biophysical effects of land cover changes in West Africa: a systematic review en_US
dc.type Article en_US


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