TY - JOUR
T1 - Deconvolution of remotely sensed spectral mixtures for retrieval of LAI, fAPAR and soil brightness
AU - Van Leeuwen, W. J.D.
AU - Huete, A. R.
AU - Walthall, C. L.
AU - Prince, S. D.
AU - Bégué, A.
AU - Roujean, J. L.
N1 - Funding Information:
The execution of a collaborative, international experiment such as HAPEX-Sahel requires the dedicated efforts of a great many people, many of whom cannot be named here. We wish to thank our collaborators in Niger at DMN, DRE, University of Niamey, INRAN, A&oport de Niamey Authority, Groupement Aerien National, AGRHYMET, ICRISAT, and ACMAD. Financial support for HAPEX-Sahel was obtained from ORS-TOM, M6t6o France, INSU/CNRS, Centre National d'Etude Spatiale (CNES), Minist6re de la Recherche et de l'Espace, Minist~re de l'Environment, Ministate de l'Education Nationale et de la Culture, and the Conseil R6gional Midi Pyr6ne6s (all of France), ODA, NERC and the NERC TIGER Programme, JEP (all of United Kingdom), NASA (USA), The European Community and Environment, and from several national funding agencies of Denmark, the Netherlands, and Germany. Thanks to Mike Spanner and Rangshai Halthore at Goddard Space Flight Center who provided aerosol optical depth data for the correction of ASAS imagery. We are grateful to Garba Seydou, Mike Guilbault, Shelly Thawley, Niall Hanan, Lara Prihodko, Janet Franklin, Jeff Duncan, NaDene Sorensen and many others who prepared and helped with HAPEX field work in Niger, 1992. This work was supported by MODIS contract NAS5-31364 (A.R. Huete) and NASA grants NAGW-1949 (A.R. Huete), NAGW-1967 (S.D. Prince), NAG5-1471 (S.D. Prince), and Eos-NAWG-2425 (S. Sorooshian).
PY - 1997/2
Y1 - 1997/2
N2 - Linear mixture models have been used to invert spectral reflectances of targets at the Earth's surface into proportions of plant and soil components. However, operational use of mixture models has been limited by a lack of biophysical interpretation of the results. The main objectives of this study were (1) to relate the deconvolved components of mixture model with biophysical properties of vegetation and soil at the surface and (2) to apply the mixture model results to remotely sensed imagery. A radiative transfer model (SAIL: Scattering by Arbitrarily Inclined Leaves) was used to generate reflectance 'mixtures' from leaf and bare soil spectral measurements made at HAPEX-Sahel (Hydrological Atmospheric Pilot EXperiment) study sites. The SAIL model was used to create canopy reflectances and fractions of absorbed photosynthetically active radiation (fAPAR) for a range of mixed targets with varying leaf area index (LAI) and soils. A spectral mixture model was used to deconvolve the simulated reflectance data into component fractions, which were then calibrated to the SAIL-generated LAI, fAPAR and soil brightness. The calibrated relationships were validated with observational ground data (LAI, fAPAR and reflectance) measured at the HAPEX Sahel fallow bush/grassland, fallow grassland and millet sites. Both the vegetation and soil component fractions were found to be dependent upon soil background brightness, such that inclusion of the soil fraction information significantly improved the derivation of vegetation biophysical parameters. Soil brightness was also shown to be a useful parameter to infer soil properties. The deconvolution methodology was then applied to a nadir image of a HAPEX-Sahel site measured by the Advanced Solid State Array Spectroradiometer (ASAS). Site LAI and fAPAR were successfully estimated by combining the fractional estimates of vegetation and soils, obtained through deconvolution of the ASAS image, with the calibrated relationships between vegetation fraction, LAI and fAPAR, obtained from the SAIL data.
AB - Linear mixture models have been used to invert spectral reflectances of targets at the Earth's surface into proportions of plant and soil components. However, operational use of mixture models has been limited by a lack of biophysical interpretation of the results. The main objectives of this study were (1) to relate the deconvolved components of mixture model with biophysical properties of vegetation and soil at the surface and (2) to apply the mixture model results to remotely sensed imagery. A radiative transfer model (SAIL: Scattering by Arbitrarily Inclined Leaves) was used to generate reflectance 'mixtures' from leaf and bare soil spectral measurements made at HAPEX-Sahel (Hydrological Atmospheric Pilot EXperiment) study sites. The SAIL model was used to create canopy reflectances and fractions of absorbed photosynthetically active radiation (fAPAR) for a range of mixed targets with varying leaf area index (LAI) and soils. A spectral mixture model was used to deconvolve the simulated reflectance data into component fractions, which were then calibrated to the SAIL-generated LAI, fAPAR and soil brightness. The calibrated relationships were validated with observational ground data (LAI, fAPAR and reflectance) measured at the HAPEX Sahel fallow bush/grassland, fallow grassland and millet sites. Both the vegetation and soil component fractions were found to be dependent upon soil background brightness, such that inclusion of the soil fraction information significantly improved the derivation of vegetation biophysical parameters. Soil brightness was also shown to be a useful parameter to infer soil properties. The deconvolution methodology was then applied to a nadir image of a HAPEX-Sahel site measured by the Advanced Solid State Array Spectroradiometer (ASAS). Site LAI and fAPAR were successfully estimated by combining the fractional estimates of vegetation and soils, obtained through deconvolution of the ASAS image, with the calibrated relationships between vegetation fraction, LAI and fAPAR, obtained from the SAIL data.
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U2 - 10.1016/S0022-1694(96)03199-X
DO - 10.1016/S0022-1694(96)03199-X
M3 - Article
AN - SCOPUS:0030615657
SN - 0022-1694
VL - 188-189
SP - 697
EP - 724
JO - Journal of Hydrology
JF - Journal of Hydrology
IS - 1-4
ER -