Full text: XVIIIth Congress (Part B7)

=75° 
Sy 
-0° 
  
Neither Walthall’s model nor our proposal to account for the 
specular peak are based on theoretical assumptions. f. as 
defined in equation 7 is just an empirical function to describe 
the measured data. 
4 RESULTS OF THE BRDF-MODEL-FITTING TO 
THE SELECTED SURFACE SAMPLES 
Fig. 5-10 show the BRDF of the samples as fitted by equation 
1. There was no uniform angular dependence of the samples. 
The BRDF of some of the samples increased with increasing 
zenith angles (e.g. concrete), whereas the BRDF of other 
samples decreased with increasing zenith angles (e.g. plastic). 
The variation due to the diffuse component is usually less 
than 15.96 (not taking into account zenith angles greater 
than 75^). The intensity of the specular peak dominates the 
visual impression of figures 5 to 10. 
No simple rules could be deduced from the wavelength depen- 
dence of the coefficients ao to as, which describe the diffuse 
component. The wavelength dependence of the coefficients 
as to ag, which describe the specular component, is almost 
always linear or even constant. 
The coefficients of the samples are given in tables 11 — 13 at 
a wavelength of A = 650, 750,850 nm respectively. The er- 
ror was calculated from the corresponding covariance matrix. 
The relative error of the fitted BRDF varies between 2 and 
7%. 
All the selected samples pass the x? test. We conclude that 
the function of [Walthall, 1985] with the modifications of 
[Liang, 1994], extended by a specular peak, is best suited 
for describing the BRDF of the samples studied by us. 
5 OUTLOOK 
We plan to apply the here discussed experimental results to 
multispectral imagery recorded with the DAEDALUS AADS 
1268 scanner. The imagery was acquired during several cam- 
paigns in cooperation with the German Aerospace Research 
Establishment (DLR) and is described in previous communi- 
cations [Hepp, 1994]. 
ACKNOWLEDGEMENTS 
Dr. Barbara Bartsch put the spectrometer OVID at our dis- 
posal. She and Dr. Martin Kollewe enabled us to carry out 
the measurements. We want to thank them for their contri- 
butions. 
REFERENCES 
[Walthall, 1985] C. L. Walthall and J. M. Norman and J. 
M. Welles and G. Campbell and B. L. Blad, 1985. Simple 
equation to approximate the bidirectional reflectance from 
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24, pp. 383-387. 
[Liang, 1994] S. Liang and A. H. Strahler, 1994. Retrieval 
of Surface BRDF from Multiangle Remotely Sensed Data, 
Remote Sensing of Environment, 50, pp. 18-30. 
[Nicodemus, 1970] F.E. Nicodemus, 1970. Reflectance 
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[Flasse, 1993] Stephane P. Flasse and Michel M. Verstraete 
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[Jackson, 1992] R. D. Jackson and T. Clarke and S. Moran, 
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[Oren, 1995] M. Oren and S.K. Nayar, 1995. Generalization 
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[Minnaert, 1941] M. Minnaert, 1941. The reciprocity princi- 
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497 
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B7. Vienna 1996 
 
	        
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