Abstract

The Sahel region in West Africa has been experiencing a persistent drought throughout the last three decades. Here, we present a new perspective on the underlying physical mechanism behind this phenomenon. We use a coupled biosphere‐atmosphere model including explicit representation of ecosystem dynamics to demonstrate that, regardless of the nature of the initial forcing, the natural response of the local grass ecosystem to the dry conditions of the late 1960s played a critical role in maintaining the drought through the following decades. The onset of the drought has been marked by a forced shift from a self‐sustaining wet climate equilibrium to a similarly self‐sustaining but dry climate equilibrium.

Keywords

EcosystemBiosphereForcing (mathematics)Environmental scienceClimate changeClimatologyNatural (archaeology)EcologyAtmospheric sciencesPrecipitationGeographyBiologyGeologyMeteorology

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Publication Info

Year
2000
Type
article
Volume
27
Issue
6
Pages
795-798
Citations
173
Access
Closed

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Guiling Wang, Elfatih A. B. Eltahir (2000). Ecosystem dynamics and the Sahel Drought. Geophysical Research Letters , 27 (6) , 795-798. https://doi.org/10.1029/1999gl011089

Identifiers

DOI
10.1029/1999gl011089