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Characterization of the interannual and intraseasonal variability of West African vegetation between 1982 and 2002 by means of NOAA AVHRR NDVI data
Philippon N., Jarlan L., Martiny N., Camberlin P., Mougin E.
Journal of Climate 20, 7 (2007) 1202-1218 - http://hal.archives-ouvertes.fr/hal-00293345
Articles dans des revues avec comité de lecture
Planète et Univers/Interfaces continentales, environnement
Characterization of the interannual and intraseasonal variability of West African vegetation between 1982 and 2002 by means of NOAA AVHRR NDVI data
Nathalie Philippon 1, Lionel Jarlan () 2, 3, Nadège Martiny () 1, Pierre Camberlin 1, E. Mougin 2
1 :  Centre de Recherches de Climatologie (CRC)
http://www.u-bourgogne.fr/climatologie
CNRS : UMR5210 – Université de Bourgogne
Faculté des Sciences 6 Boulevard Gabriel 21000 DIJON
France
2 :  Centre d'études spatiales de la biosphère (CESBIO)
http://www.cesbio.ups-tlse.fr
CNRS : UMR5126 – Institut de recherche pour le développement [IRD] – CNES – Observatoire Midi-Pyrénées – INSU – Université Paul Sabatier [UPS] - Toulouse III
bpi 2801 18 Av Edouard Belin 31401 TOULOUSE CEDEX 4
France
3 :  Groupe d'étude de l'atmosphère météorologique (CNRM-GAME)
http://www.cnrm.meteo.fr
CNRS : URA1357 – INSU – Météo France
METEO FRANCE CNRM 42 Av Gaspard Coriolis 31057 TOULOUSE CEDEX 1
France
The interannual and intraseasonal variability of West African vegetation over the period 1982-2002 is studied using the normalized difference vegetation index (NDVI) from the Advanced Very High Resolution Radiometer (AVHRR). The novel independent component analysis (ICA) technique is applied to extract the main modes of the interannual variability of the vegetation, among which two modes are worth describing. The first component (IC1) describes NDVI variability over the Sahel from August to October. A strong photosynthetic activity over the Sahel is related to above-normal convection and rainfall within the intertropical convergence zone (ITCZ) in summertime and is partly associated with colder (warmer) SST in the eastern tropical Pacific (the Mediterranean). The second component (IC2) depicts a dipole pattern between the Sahelian and Guinean regions during the northern summer followed by a southward-propagating signal from October to December. It is associated with a north-south dipole in convection and rainfall induced by variations in the latitudinal location of the ITCZ as a response to the occurrence of the tropical Atlantic dipole. The analysis of the intraseasonal variability of the Sahelian vegetation relies on the analysis of the seasonal marches and their main phenological stages. Green-up usually starts in early July and shows a very low year-to-year variability, while senescence ends by mid-November and is prone to larger interannual variability. Six types of vegetative seasonal marches are discriminated according to variations in the timing of phenological stages as well as in the greening intensity. These types appear to be strongly dependent on rainfall distribution and amount, particularly those recorded in late August. Finally, year-to-year memory effects are highlighted: NDVI recorded during the green-up phase in year j appears to be strongly related to the maximum NDVI value recorded at year j - 1.
Anglais

Journal of Climate
Publisher American Meteorological Society
ISSN 0894-8755 (eISSN : 1520-0442)
internationale
01/04/2007
20
7
1202-1218

SEA-SURFACE TEMPERATURE – INDEPENDENT COMPONENT ANALYSIS – SAHEL RAINFALL – RAINY-SEASON – ATMOSPHERIC DYNAMICS – AIR-TEMPERATURE – EL-NINO – INDEX – PRECIPITATION – PHENOLOGY

AMMA