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

Author:

Conway Declan1,Persechino Aurelie2,Ardoin-Bardin Sandra3,Hamandawana Hamisai4,Dieulin Claudine3,Mahé Gil3

Affiliation:

1. School of Development Studies, and Tyndall Centre for Climate Change Research, University of East Anglia, Norwich, United Kingdom

2. School of Development Studies, University of East Anglia, Norwich, United Kingdom

3. UMR HydroSciences Montpellier, Montpellier, France

4. Department of Geography and Environmental Sciences, North West University, Republic of South Africa

Abstract

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.

Publisher

American Meteorological Society

Subject

Atmospheric Science

Reference87 articles.

1. Adaptation to climate change in the developing world.;Adger;Prog. Dev. Stud.,2003

2. Ardoin-Bardin, S. , 2004: Hydroclimate variability and impacts on water resources of large hydrological catchments in the Sudanese–Sahelian area (in French). Ph.D. thesis, University of Montpellier II, 437 pp.

3. Analysis of convective activity and its relationship to the rainfall over the Rift Valley lakes of East Africa during 1983–90 using the Meteosat infrared channel.;Ba;J. Appl. Meteor.,1998

4. Homogenization and completion of hydrometric data in Senegal catchment upstream of Bakel (in French).;Bader,1990

5. Study of Manantali’s dam impacts on hydrological regime of the Senegal river at Bakel (in French).;Bader,1992

Cited by 155 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

同舟云学术

1.学者识别学者识别

2.学术分析学术分析

3.人才评估人才评估

"同舟云学术"是以全球学者为主线,采集、加工和组织学术论文而形成的新型学术文献查询和分析系统,可以对全球学者进行文献检索和人才价值评估。用户可以通过关注某些学科领域的顶尖人物而持续追踪该领域的学科进展和研究前沿。经过近期的数据扩容,当前同舟云学术共收录了国内外主流学术期刊6万余种,收集的期刊论文及会议论文总量共计约1.5亿篇,并以每天添加12000余篇中外论文的速度递增。我们也可以为用户提供个性化、定制化的学者数据。欢迎来电咨询!咨询电话:010-8811{复制后删除}0370

www.globalauthorid.com

TOP

Copyright © 2019-2024 北京同舟云网络信息技术有限公司
京公网安备11010802033243号  京ICP备18003416号-3