G. Schluessel et al., MODELING THE BIDIRECTIONAL REFLECTANCE DISTRIBUTION FUNCTION OF MIXEDFINITE PLANT CANOPIES AND SOIL, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 99(D5), 1994, pp. 10577-10600
An analytical model of the bidirectional reflectance for optically sem
i-infinite plant canopies has been extended to describe the reflectanc
e of finite depth canopies with contributions from the underlying soil
. The model depends on 10 independent parameters describing vegetation
and soil optical and structural properties. The model is inverted wit
h a nonlinear minimization routine using directional reflectance data
for lawn (leaf area index (LAI) is equal to 9.9), soybeans (LAI, 2.9)
and simulated reflectance data (LAI, 1.0) from a numerical bidirection
al reflectance distribution function (BRDF) model (Myneni et al., 1988
). While the ten-parameter model results in relatively low rms differe
nces for the BRDF, most of the retrieved parameters exhibit poor stabi
lity. The most stable parameter was the single-scattering albedo of th
e vegetation. Canopy albedo could be derived with an accuracy of less
than 5% relative error in the visible and less than 1% in the near-inf
rared. Sensitivity tests were performed to determine which of the 10 p
arameters were most important and to assess the effects of Gaussian no
ise on the parameter retrievals. Out of the 10 parameters, three were
identified which described most of the BRDF variability. At low LAI va
lues the most influential parameters were the single-scattering albedo
s (both soil and vegetation) and LAI, while at higher LAI values (> 2.
5) these shifted to the two scattering phase function parameters for v
egetation and the single-scattering albedo of the vegetation. The thre
e-parameter model, formed by fixing the seven least significant parame
ters, gave higher rms values but was less sensitive to noise in the BR
DF than the full ten-parameter model. A full hemispherical reflectance
data set for lawn was then interpolated to yield BRDF values correspo
nding to advanced very high resolution radiometer (AVHRR) scan geometr
ies collected over a period of nine days. The resulting retrieved para
meters and BRDFs are similar to those for the full sampling geometry,
suggesting that the limited geometry of AVHRR measurements might be us
ed to reliably retrieve BRDF and canopy albedo with this model.