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

被引:53
作者
Los, S. O.
Weedon, G. P.
North, P. R. J.
Kaduk, J. D.
Taylor, C. M.
Cox, P. M.
机构
[1] Univ Wales Swansea, Dept Geog, Climate & Land Surface Syst Interact Ctr, Swansea SA2 8AY, W Glam, Wales
[2] Univ Leicester, Dept Geog, Leicester LE1 7RH, Leics, England
[3] Natl Environm Res Council, Ctr Ecol & Hydrol, Wallingford, Oxon, England
[4] NERC, Ctr Ecol & Hydrol, Winfrith, England
基金
英国自然环境研究理事会;
关键词
D O I
10.1029/2006GL027065
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
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 degrees and 20 degrees N.
引用
收藏
页数:5
相关论文
共 31 条
[1]  
[Anonymous], 1998, Applied regression analysis, DOI 10.1002/9781118625590
[2]   DYNAMICS OF DESERTS AND DROUGHT IN SAHEL [J].
CHARNEY, JG .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1975, 101 (428) :193-202
[3]   Least angle regression - Rejoinder [J].
Efron, B ;
Hastie, T ;
Johnstone, I ;
Tibshirani, R .
ANNALS OF STATISTICS, 2004, 32 (02) :494-499
[4]   PREDICTION OF SEASONAL RAINFALL IN THE SAHEL REGION USING EMPIRICAL AND DYNAMICAL METHODS [J].
FOLLAND, C ;
OWEN, J ;
WARD, MN ;
COLMAN, A .
JOURNAL OF FORECASTING, 1991, 10 (1-2) :21-56
[5]   Oceanic forcing of Sahel rainfall on interannual to interdecadal time scales [J].
Giannini, A ;
Saravanan, R ;
Chang, P .
SCIENCE, 2003, 302 (5647) :1027-1030
[6]  
Hall F., 2005, ISLSCP INITIATIVE 2
[7]  
HELLDEN U, 1991, AMBIO, V20, P372
[8]   THE PATHFINDER AVHRR LAND DATA SET - AN IMPROVED COARSE RESOLUTION DATA SET FOR TERRESTRIAL MONITORING [J].
JAMES, ME ;
KALLURI, SNV .
INTERNATIONAL JOURNAL OF REMOTE SENSING, 1994, 15 (17) :3347-3363
[9]   Regions of strong coupling between soil moisture and precipitation [J].
Koster, RD ;
Dirmeyer, PA ;
Guo, ZC ;
Bonan, G ;
Chan, E ;
Cox, P ;
Gordon, CT ;
Kanae, S ;
Kowalczyk, E ;
Lawrence, D ;
Liu, P ;
Lu, CH ;
Malyshev, S ;
McAvaney, B ;
Mitchell, K ;
Mocko, D ;
Oki, T ;
Oleson, K ;
Pitman, A ;
Sud, YC ;
Taylor, CM ;
Verseghy, D ;
Vasic, R ;
Xue, YK ;
Yamada, T .
SCIENCE, 2004, 305 (5687) :1138-1140
[10]  
LAMB PJ, 1992, J CLIMATE, V5, P476, DOI 10.1175/1520-0442(1992)005<0476:FCSOTA>2.0.CO