Mapping of Sahelian vegetation parameters from ERS scatterometer data with an evolution strategies algorithm

The West African Sahel rainfall regime is known for its spatio-temporal variability at different scales which has a strong impact on vegetation development. This study presents results of the combined use of a simple water balance model, a radiative transfer model and ERS scatterometer data to produ...

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Main Authors: Jarlan, L., Mazzega, P., Mougin, E., Lavenu, F., Marty, G., Frison, P.L., Hiernaux, Pierre H.Y.
Format: Journal Article
Language:Inglés
Published: Elsevier 2003
Subjects:
Online Access:https://hdl.handle.net/10568/33134
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author Jarlan, L.
Mazzega, P.
Mougin, E.
Lavenu, F.
Marty, G.
Frison, P.L.
Hiernaux, Pierre H.Y.
author_browse Frison, P.L.
Hiernaux, Pierre H.Y.
Jarlan, L.
Lavenu, F.
Marty, G.
Mazzega, P.
Mougin, E.
author_facet Jarlan, L.
Mazzega, P.
Mougin, E.
Lavenu, F.
Marty, G.
Frison, P.L.
Hiernaux, Pierre H.Y.
author_sort Jarlan, L.
collection Repository of Agricultural Research Outputs (CGSpace)
description The West African Sahel rainfall regime is known for its spatio-temporal variability at different scales which has a strong impact on vegetation development. This study presents results of the combined use of a simple water balance model, a radiative transfer model and ERS scatterometer data to produce map of vegetation biomass and thus vegetation cover at a spatial resolution of 25 km. The backscattering coefficient measured by spaceborne wind scatterometers over Sahel shows a marked seasonality linked to the drastic changes of both soil and vegetation dielectric properties associated to the alternating dry and wet seasons. For lack of a direct observation, METEOSAT rainfall estimates are used to calculate temporal series of soil moisture with the help of a water balance model. This a priori information is used as input of the radiative transfer model that simulates the interaction between the radar wave and the surface components (soil and vegetation). Then, an inversion algorithm is applied to retrieve vegetation aerial mass from the ERS scatterometer data. Because of the nonlinear feature of the inverse problem to be solved, the inversion is performed using a global stochastic nonlinear inversion method. A good agreement is obtained between the inverse solutions and independent field measurements with mean and standard deviation of -54 and 130 kg of dry matter by hectare (kg DM/ha), respectively. The algorithm is then applied to a 350,000 km2 area including the Malian Gourma and Seno region and a Sahelian part of Burkina Faso during two contrasted seasons (1999 and 2000). At the considered resolution, the obtained herbaceous mass maps show a global qualitative consistency (r2=0.71) with NDVI images acquired by the VEGETATION instrument.
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spelling CGSpace331342024-04-25T06:01:23Z Mapping of Sahelian vegetation parameters from ERS scatterometer data with an evolution strategies algorithm Jarlan, L. Mazzega, P. Mougin, E. Lavenu, F. Marty, G. Frison, P.L. Hiernaux, Pierre H.Y. vegetation rain models soil water The West African Sahel rainfall regime is known for its spatio-temporal variability at different scales which has a strong impact on vegetation development. This study presents results of the combined use of a simple water balance model, a radiative transfer model and ERS scatterometer data to produce map of vegetation biomass and thus vegetation cover at a spatial resolution of 25 km. The backscattering coefficient measured by spaceborne wind scatterometers over Sahel shows a marked seasonality linked to the drastic changes of both soil and vegetation dielectric properties associated to the alternating dry and wet seasons. For lack of a direct observation, METEOSAT rainfall estimates are used to calculate temporal series of soil moisture with the help of a water balance model. This a priori information is used as input of the radiative transfer model that simulates the interaction between the radar wave and the surface components (soil and vegetation). Then, an inversion algorithm is applied to retrieve vegetation aerial mass from the ERS scatterometer data. Because of the nonlinear feature of the inverse problem to be solved, the inversion is performed using a global stochastic nonlinear inversion method. A good agreement is obtained between the inverse solutions and independent field measurements with mean and standard deviation of -54 and 130 kg of dry matter by hectare (kg DM/ha), respectively. The algorithm is then applied to a 350,000 km2 area including the Malian Gourma and Seno region and a Sahelian part of Burkina Faso during two contrasted seasons (1999 and 2000). At the considered resolution, the obtained herbaceous mass maps show a global qualitative consistency (r2=0.71) with NDVI images acquired by the VEGETATION instrument. 2003-09 2013-07-03T05:26:06Z 2013-07-03T05:26:06Z Journal Article https://hdl.handle.net/10568/33134 en Limited Access Elsevier Remote Sensing of Environment;87(1): 72-84
spellingShingle vegetation
rain
models
soil
water
Jarlan, L.
Mazzega, P.
Mougin, E.
Lavenu, F.
Marty, G.
Frison, P.L.
Hiernaux, Pierre H.Y.
Mapping of Sahelian vegetation parameters from ERS scatterometer data with an evolution strategies algorithm
title Mapping of Sahelian vegetation parameters from ERS scatterometer data with an evolution strategies algorithm
title_full Mapping of Sahelian vegetation parameters from ERS scatterometer data with an evolution strategies algorithm
title_fullStr Mapping of Sahelian vegetation parameters from ERS scatterometer data with an evolution strategies algorithm
title_full_unstemmed Mapping of Sahelian vegetation parameters from ERS scatterometer data with an evolution strategies algorithm
title_short Mapping of Sahelian vegetation parameters from ERS scatterometer data with an evolution strategies algorithm
title_sort mapping of sahelian vegetation parameters from ers scatterometer data with an evolution strategies algorithm
topic vegetation
rain
models
soil
water
url https://hdl.handle.net/10568/33134
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