Mouhamadou Bamba Sylla

Dr. Mouhamadou Bamba Sylla

orcid

Research Focus & Metrics

Academic Career Length

18Years (2009-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

View All Publications
13 April 2016
Verified
Book Chapter
Closed access
PDF file
MSMouhamadou Bamba Sylla
Mouhamadou Bamba Sylla
PNPinghouinde Michel Nikiema
Pinghouinde Michel Nikiema
PGPeter Gibba
Peter Gibba
IKIbourahima Kebe
Ibourahima Kebe
NKNana Ama Browne Klutse
Nana Ama Browne Klutse

2 July 2009 in Climate Dynamics
Verified
Journal Article
Closed access
PDF file
MSMouhamadou Bamba Sylla
Mouhamadou Bamba Sylla
ECE. Coppola
E. Coppola
LML. Mariotti
L. Mariotti
FGF. Giorgi
F. Giorgi
PRP. M. Ruti
P. M. Ruti
XBX. Bi
X. Bi

27 July 2018 in Earth's Future
Verified
Journal Article
Open access
PDF file
MSMouhamadou Bamba Sylla
Mouhamadou Bamba Sylla
AFAissatou Faye
Aissatou Faye
FGFilippo Giorgi
Filippo Giorgi
Arona DIEDHIOUArona DIEDHIOU
Arona DIEDHIOU
HKHarald Kunstmann
Harald Kunstmann
Heat and discomfort indices are applied to the multimodel ensemble mean of COordinated Regional climate Downscaling EXperiment‐Africa regional climate model projections to investigate future changes in heat stress and the proportion of human population at risk under 1.5 °C and 2 °C global warming scenarios over West Africa. The results show that heat stress of category Extreme Caution is projected to extend spatially (up to 25%) over most of the Gulf of Guinea, Sahel, and Sahara desert areas, with different regional coverage during the various seasons. Similarly, the projected seasonal proportion of human population at discomfort substantially increases to more than 50% over most of the region. In particular, in June–August over the Sahel and the western Sahara desert, new areas (15% of West Africa) where most of the population is at risk emerge. This indicates that from 50% to almost everyone over most of the Sahel countries and part of the western Sahara desert is at risk of possible heat cramp, heat exhaustion, and heat stroke in future climate scenarios. These conditions become more frequent and are accompanied by the emergence of days with dangerous heat stress category during which everyone feels discomfort and is vulnerable to a likely heat cramp and heat exhaustion. In general, all the above features are more extended and more frequent in the 2 °C than in the 1.5 °C scenario. Protective measures are thus required for outdoor workers, occupational settings in hot environments, and people engaged in strenuous activities.

10 January 2015 in Theoretical and Applied Climatology
Verified
Journal Article
Closed access
PDF file
NKNana Ama Browne Klutse
Nana Ama Browne Klutse
MSMouhamadou Bamba Sylla
Mouhamadou Bamba Sylla
IDIsmaila Diallo
Ismaila Diallo
ASAbdoulaye Sarr
Abdoulaye Sarr
ADAlessandro Dosio
Alessandro Dosio
MBMatthias Büchner
Matthias Büchner

27 July 2020 in Climate Dynamics
Verified
Journal Article
Open access
PDF file
WSwindmanagda sawadogo
windmanagda sawadogo
MRMichelle Reboita
Michelle Reboita
AFAissatou Faye
Aissatou Faye
RRRosmeri da Rocha
Rosmeri da Rocha
RORomaric C. Odoulami
Romaric C. Odoulami
FGFilippo Giorgi
Filippo Giorgi
Renewable energy is key for the development of African countries, and knowing the best location for the implementation of solar and wind energy projects is important within this context. The purpose of this study is to assess the impact of climate change on solar and wind energy potential over Africa under low end (RCP2.6) and high end (RCP8.5) emission scenarios using a set of new high resolution (25 km) simulations with the Regional Climate Model version 4 (RegCM4) produced as part of the CORDEX-CORE initiative. The projections focus on two periods: (i) the near future (2021–2040) and ii) the mid-century future (2041–2060). The performance of the RegCM4 ensemble mean (Rmean) in simulating relevant present climate variables (1995–2014) is first evaluated with respect to the ERA5 reanalysis and satellite-based data. The Rmean reproduces reasonably well the observed spatial patterns of solar irradiance, air temperature, total cloud cover, wind speed at 100 m above the ground level, photovoltaic power potential (PVP), concentrated solar power output (CSPOUT) and wind power density (WPD) over Africa, though some biases are still evident, especially for cloud-related variables. For the future climate, the sign of the changes is consistent in both scenarios but with more intense magnitude in the middle of the century RCP8.5 scenario. Considering the energy variables, the Rmean projects a general decrease in PVP, which is more pronounced in the mid-century future and under RCP8.5 (up to 2%). Similarly, a general increase in CSPOUT (up to 2%) is projected over the continent under both the RCP2.6 and RCP8.5 scenarios. The projection in WPD shows a similar change (predominant increase) in the near and mid-century future slices under both RCPs with a maximum increase of 20%. The present study suggests that the RCP2.6 emission scenario, in general, favours the implementation of renewable energy in Africa compared to the RCP8.5.

3 October 2015 in Climatic Change
Verified
Journal Article
Closed access
PDF file
MSMouhamadou Bamba Sylla
Mouhamadou Bamba Sylla
NENellie Elguindi
Nellie Elguindi
FGFilippo Giorgi
Filippo Giorgi
DWDominik Wisser
Dominik Wisser