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Article Dans Une Revue Hydrological Sciences Journal Année : 2009

The sensitivity of Sahelian runoff to climate change

Résumé

A simple method is used to study the response of runoff in the Sahel to climate change. The statistical characteristics of rainfall are calculated over the western part of the Sahel for the period 1961–1990, using the BADOPLU network. Daily rainfall is simulated using a Markov process with Weibull distribution for rainfall depths. Runoff is modelled using a conceptual SCS model and the curve numbers are calculated for West Africa. Climate change is provided by simulations using the Arpège GCM (Scenario A1B), and a perturbation method is used on the parameters which describe the rainfall. Changes in rainfall are assumed to occur through increases in frequency, not intensity. Using Arpège, runoff is mainly found to increase, in depth and in number of events, by the end of the 21st century. Changes in evaporation and land use are not included in the analysis. The impact of this 21st century potential climate change (rainfall) on the runoff is found to be of the same magnitude as the impact of changes in land use.

Domaines

Océanographie
Fichier non déposé

Dates et versions

hal-00406922 , version 1 (23-07-2009)

Identifiants

Citer

M. Gerbaux, N. M.J. Hall, N. Dessay, I. Zin. The sensitivity of Sahelian runoff to climate change. Hydrological Sciences Journal, 2009, 54 (1), pp.5-16. ⟨10.1623/hysj.54.1.5⟩. ⟨hal-00406922⟩
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