An observation-based estimate of the strength of rainfall-vegetation interactions in the Sahel

Over the course of the twentieth century the African Sahel experienced large variations in annual precipitation; including the wet period during the 1950s and 1960s and the long‐term drought during the 1970s and 1980s. Feedbacks between the land surface and atmosphere can affect rainfall variability...

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Published inGeophysical research letters Vol. 33; no. 16; pp. L16402 - n/a
Main Authors Los, S. O., Weedon, G. P., North, P. R. J., Kaduk, J. D., Taylor, C. M., Cox, P. M.
Format Journal Article
LanguageEnglish
Published Washington, DC American Geophysical Union 01.08.2006
Blackwell Publishing Ltd
Subjects
Biogeosciences
Climate dynamics
Earth sciences
Earth, ocean, space
Exact sciences and technology
Global Change
Land cover change
Land/atmosphere interactions
Remote sensing
Water/energy interactions
Sahel
Africa
atmosphere
satellites
rainfall
Vegetation index
atmospheric precipitation
strength
Africa
vegetation
Climate models
Long term
Interannual variation
coupling
Feedback
Ground surface
drought
Statistical model
hot spots
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Summary:Over the course of the twentieth century the African Sahel experienced large variations in annual precipitation; including the wet period during the 1950s and 1960s and the long‐term drought during the 1970s and 1980s. Feedbacks between the land surface and atmosphere can affect rainfall variability at monthly, annual and decadal time scales. However, the strength of the coupling between the land surface and precipitation is still highly uncertain, with climate‐model derived estimates differing by an order of magnitude. Here a statistical model of vegetation greenness is used to estimate the vegetation‐rainfall coupling strength in the Sahel, based on monthly satellite‐derived vegetation index and meteorological data. Evidence is found for a positive feedback between vegetation and rainfall at the monthly time scale, and for a vegetation memory operating at the annual time scale. These vegetation‐rainfall interactions increase the interannual variation in Sahelian precipitation; accounting for as much as 30% of the variability in annual precipitation in some hot spot regions between 15° and 20°N.
Bibliography:ArticleID:2006GL027065
Tab-delimited Table 1.
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ISSN:0094-8276
1944-8007
DOI:10.1029/2006GL027065