ESTIMATING THE FRACTION OF ABSORBED PHOTOSYNTHETICALLY ACTIVE RADIATION (FAPAR) AT FIFE WITH AIRBORNE BIDIRECTIONAL SPECTRAL REFLECTANCE DATA

Citation
Ecb. Decolstoun et al., ESTIMATING THE FRACTION OF ABSORBED PHOTOSYNTHETICALLY ACTIVE RADIATION (FAPAR) AT FIFE WITH AIRBORNE BIDIRECTIONAL SPECTRAL REFLECTANCE DATA, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 100(D12), 1995, pp. 25523-25535
Citations number
67
Categorie Soggetti
Metereology & Atmospheric Sciences
Volume
100
Issue
D12
Year of publication
1995
Pages
25523 - 25535
Database
ISI
SICI code
Abstract
The relationship between the fraction of absorbed photosynthetically a ctive radiation (f(APAR)) and spectral vegetation indices (SVIs) is af fected by various factors, including background effects and the view z enith angle of the sensor. This study investigated the effects of esti mating f(APAR) from multiple off-nadir airborne measurements acquired by the advanced solid-state array spectroradiometer (ASAS) during the First International Satellite Land Surface Climatology Project Field E xperiment. Using atmospherically corrected data, f(APAR) was estimated with both directional SVIs (normalized difference vegetation index (N DVI) and simple ratio (SR)) and PAR hemispherical reflectance (R(PAR)) calculated from PAR bidirectional reflectance factors for the seven v iewing angles of ASAS. Very weak linear relationships were found betwe en the ground-measured total f(APAR) values and ASAS measurements, ass umed to be due to the presence of varying amounts of senescent plant m aterials in the canopy. Exclusion of data collected in October when th e canopy was fully senescent somewhat improved these relationships. Ho wever, correction of total f(APAR) values by the fraction of green veg etation present (green f(APAR)) provided substantial improvement. For both SVIs the highest coefficients of determination (r(2) = 0.839 for NDVI; r(2) = 0.890 for SR) were found at 15 degrees in the backscatter ing direction decreasing to minimum values at +/-45 degrees, a trend t hought to be associated with the effect of canopy structure on the SVI s. Although R(PAR) was not strongly correlated with either the total o r the green f(APAR), it was related to the independently measured PAR flux reflected from the canopy indicating a potential for deriving PAR hemispherical reflectance from directional measurements for natural c over types such as grasslands.