Rainfall and Water Resources Variability in Sub-Saharan Africa during the Twentieth Century

Journal of Hydrometeorology - Tập 10 Số 1 - Trang 41-59 - 2009
Declan Conway1, A. Persechino2, Sandra Ardoin‐Bardin3, Hamisai Hamandawana4, Claudine Dieulin3, Gil Mahé3
1School of Development Studies, and Tyndall Centre for Climate Change Research, University of East Anglia, Norwich, United Kingdom
2School of Development Studies, University of East Anglia, Norwich, United Kingdom
3UMR HydroSciences Montpellier, Montpellier, France
4Department of Geography and Environmental Sciences, North West University, Republic of South Africa

Tóm tắt

Abstract River basin rainfall series and extensive river flow records are used to characterize and improve understanding of spatial and temporal variability in sub-Saharan African water resources during the last century. Nine major international river basins were chosen for examination primarily for their extensive, good quality flow records. A range of statistical descriptors highlight the substantial variability in rainfall and river flows [e.g., differences in rainfall (flows) of up to −14% (−51%) between 1931–60 and 1961–90 in West Africa], the marked regional differences, and the modest intraregional differences. On decadal time scales, sub-Saharan Africa exhibits drying across the Sahel after the early 1970s, relative stability punctuated by extreme wet years in East Africa, and periodic behavior underlying high interannual variability in southern Africa. Central Africa shows very modest decadal variability, with some similarities to the Sahel in the adjoining basins. No consistent signals in rainfall and river flows emerge across the whole of the region. An analysis of rainfall–runoff relationships reveals varying behavior including strong but nonstationary relationships (particularly in West Africa); many basins with marked variations (temporal and spatial) in strength; weak, almost random behavior (particularly in southern Africa); and very few strong, temporally stable relationships. Twenty-year running correlations between rainfall and river flow tend to be higher during periods of greater rainfall station density; however, there are situations in which weak (strong) relationships exist even with reasonable (poor) station coverage. The authors conclude for sub-Saharan Africa that robust identification and attribution of hydrological change is severely limited by data availability, conflicting behavior across basins/regions, low signal-to-noise ratios, sometimes weak rainfall–runoff relationships, and limited quantification of the magnitude and effects of land use change.

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Journal of Hydrometeorology

Tập 10 Số 1

41-59

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