TY - JOUR
T1 - Effect of the African greenbelt position on West African summer climate
T2 - a regional climate modeling study
AU - Bamba, Adama
AU - Diallo, Ismaila
AU - Touré, N’Datchoh D.E.
AU - Kouadio, Kouakou
AU - Konaré, Abdourahamane
AU - Dramé, Mamadou S.
AU - Diedhiou, Arona
AU - Silué, Siélé
AU - Doumbia, Madina
AU - Tall, Moustapha
N1 - Funding Information:
We thank the editor and two anonymous reviewers for their constructive comments leading to improvements of the manuscript. This paper is dedicated to the memory of Professor Abdourahamane Konaré, under whose scientific guidance and teaching the authors, namely Adama Bamba, N’datchoh E. Touré, Kouakou Kouadio, Silué Siélé, and Madina Doumbia earned their graduate degrees. This work was performed with the support of institutions like African Center of Excellence on Climate Change, Biodiversity and Sustainable Agriculture (CEA-CCBAD), the West African Science Service Centre on Climate Change and Adapted Land Use (WASCAL), and the African Monsoon Multidisciplinary Analysis-2050 (AMMA-2050) project funded by the British Department for International Development (DFID) and the Natural Environment Research Council (NERC) as part of the Future Climate For Africa research programme. The work of Ismaila Diallo was performed under the US National Science Foundation grants AGS-1419526.
Publisher Copyright:
© 2018, The Author(s).
PY - 2019/7/1
Y1 - 2019/7/1
N2 - This modeling study is conducted to examine the potential impact of the reforestation (greenbelt) location (either in Sahel or in Guinean region) on West African summer climate system. To this end, three simulations using the regional climate model RegCM4 driven by ERA-Interim reanalysis were performed at 50 km horizontal resolution over a West African domain for the period 2000–2011. The first experiment, namely the control (CTRL), uses the standard vegetation cover, while the two others incorporate throughout the model integration, a zonal reforestation band of evergreen broadleaf over different locations: (i) over a 13° N–17° N band latitudes in a Sahel-Sahara region (experiment hereafter referred to as GB15N) and (ii) between 8.5° N–11.5° N in the Guinea Coast region (experiment hereafter referred to as GB10N). A comparison of the CTRL experiment with observation reveals a faithful reproduction of the mean boreal and summer seasonal precipitation pattern, though substantial dry/wet biases remain, especially in the Atlantic Ocean. In addition, the seasonal cycle over sub-regions matches satisfactory the observed pattern. The GB15N reforestation leads to a precipitation increase in the range of 2–4 mm/day over the forested areas, whereas in the GB10N reforestation, precipitation increase is weaker and not necessarily located in the forested areas. Temperature cooling is observed over the reforested area and may be explained by a decrease of ground heat flux related to a reduction of the surface albedo.
AB - This modeling study is conducted to examine the potential impact of the reforestation (greenbelt) location (either in Sahel or in Guinean region) on West African summer climate system. To this end, three simulations using the regional climate model RegCM4 driven by ERA-Interim reanalysis were performed at 50 km horizontal resolution over a West African domain for the period 2000–2011. The first experiment, namely the control (CTRL), uses the standard vegetation cover, while the two others incorporate throughout the model integration, a zonal reforestation band of evergreen broadleaf over different locations: (i) over a 13° N–17° N band latitudes in a Sahel-Sahara region (experiment hereafter referred to as GB15N) and (ii) between 8.5° N–11.5° N in the Guinea Coast region (experiment hereafter referred to as GB10N). A comparison of the CTRL experiment with observation reveals a faithful reproduction of the mean boreal and summer seasonal precipitation pattern, though substantial dry/wet biases remain, especially in the Atlantic Ocean. In addition, the seasonal cycle over sub-regions matches satisfactory the observed pattern. The GB15N reforestation leads to a precipitation increase in the range of 2–4 mm/day over the forested areas, whereas in the GB10N reforestation, precipitation increase is weaker and not necessarily located in the forested areas. Temperature cooling is observed over the reforested area and may be explained by a decrease of ground heat flux related to a reduction of the surface albedo.
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U2 - 10.1007/s00704-018-2589-z
DO - 10.1007/s00704-018-2589-z
M3 - Article
AN - SCOPUS:85052516883
SN - 0177-798X
VL - 137
SP - 309
EP - 322
JO - Theorectical and Applied Climatology
JF - Theorectical and Applied Climatology
IS - 1-2
ER -