4.6 Article

The impacts of land use and land cover change on biophysical processes in West Africa using a regional climate model experimental approach

Journal

INTERNATIONAL JOURNAL OF CLIMATOLOGY
Volume 43, Issue 4, Pages 1731-1755

Publisher

WILEY
DOI: 10.1002/joc.7943

Keywords

albedo; deforestation; dew point temperature; land use land cover change; rainfall; soil moisture; temperature

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This study assessed the potential impacts of land use change on regional climate in West Africa and found significant changes in precipitation, temperature, and dew point temperature due to land use land cover change (LULCC). Deforestation and conversion of forest to barren land led to a decrease in precipitation, while reforestation increased precipitation. LULCC also affected atmospheric conditions, including wind speed, wind direction, and humidity.
Using 2001 and 2016 land use (LU) data and three developed deforestation LU scenarios, namely Deforest I, II and III, the possible impacts of the ongoing land use land cover change (LULCC) over West Africa (WA) and the uncertainty regarding the impacts on regional climate were assessed. Twelve Weather Research and Forecasting (WRF) model simulations were configured with the default and integrated MODIS satellite dataset for two sets of 3 months (December-February DJF 2011-2012 and July-September JAS 2012) over WA. Between 2001 and 2016, changes that occurred in precipitation, temperature and dew point temperature due to LULCC are mostly not significant at the 95% level with a decrease of 0.8, 0.0 and 0.1%, respectively. Deforest I, II and III caused significant changes with an increase of 44.4, 44.7, 41.5%; 0.8, 0.9, 1.1%; and 0.3, 0.1, -0.2%, respectively, for precipitation, temperature and dew point temperature. Precipitation was lower in the simulation with 2016 LU than it was with 2001 LU, which may have also been influenced by the reforestation that occurred between the periods. However, Deforest III resulted in a widespread nonsignificant rise in precipitation, as the modified areas showed a significant decrease during JAS period. Areas where forests were converted into barren lands revealed severe increase in the surface albedo which is a strong factor that its alteration is capable of influencing precipitation and other variables over WA. LULCC also altered the atmospheric column by modifying the strength of the African Easterly Jet (AEJ), Tropical Easterly Jet (TEJ), wind speed, and monsoonal, vertical, meridional and zonal winds. Heat related fields, such as dew point and air temperature, and moisture fields such as relative humidity were also modified by LULCC. Therefore, as WA reacts strongly to LULCC, sustainable land management practices should be encouraged to control its adverse effects.

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