Abstract:
Increasing levels of climatic warming are expected to affect the global development of energy
consumption. The cooling degree day (CDD) is one of the climate-driven indices that captures the
impact of climate on energy demand. However, little is known about the spatiotemporal trends of
CDD in relation to a changing climate and economy in West Africa and its main implications.
Hence, in order to analyze how energy demand could evolve, this study aims to assess the changes
in CDD under 1.5, 2.0, 2.5, and 3.0 ◦C global warming levels (GWLs), with and without
population exposure and trends under the two representative concentration pathways (RCPs) of
RCP4.5 and RCP8.5 for West Africa. A climate-reflective base temperature (T-base) is used and was
determined using a piecewise linear regression method. Seasonal electricity consumption was
derived using a decomposition feature. An ensemble of seven Global Climate Models (GCMs) were
used for the future temperature projections. The future population was based on shared
socioeconomic pathway outputs. Based on the analysis, the reported average T-base for the West
African region is 24 ◦C. An increasing CDD trend was identified in all of the RCP scenarios, but is
more pronounced in RCP8.5. RCP8.5 departs from the mean historical period of approximately
20% by 2100 with the standardized value. The same trend is observed under different GWLs as the
warming level increased and was most striking in the Sahelian zone. Population exposure to CDD
(labelled CDDP) increases with warming levels, but is more pronounced in highly agglomerated
areas. The CDDP index best captures the spatial representation of areas with high cooling demand
potential with respect to the demographic distribution. This study can serve to inform better
energy demand assessment scenarios and supply planning against the backdrop of changing
climate conditions in West Africa.
Description:
A publication submitted to the West African Science Service Centre on Climate Change and Adapted Land Use and the Université Abdou Moumouni, Niger in partial fulfillment of the requirements for the degree of Master of Science Degree in Climate Change and Energy