sensor
Figure 1: Definition of the angles
A denotes the surface of the sample
sensor can be found in [Bartsch, 1994]. Each spectrum is
recorded simultaneously for all wavelength bands by means
of a CCD-Array. We used 61 spectral bands in the range
A = 600 — 900nm (AA = 5 nm), with a distance between
sensor and samples of 1 m. The area on the sample covered
by the instantaneous field of view (IFOV) of the sensor is
about 10 cm?.
A goniometer was constructed to hold the samples for all pos-
sible combinations of incidence and reflection angles. The go-
niometer allows to place the surface with arbitrary inclination
towards sensor and light source (see [Meister, 1996]).
The samples were selected with respect to azimuthal symme-
try, so that the BRDF's of the samples depend only on the
azimuth difference angle v = |®; — ®,|. We determined the
BRDF of six samples: aluminum sprayed with red paint, a
sheet of white smooth plastic, a concrete-type sidewalk cover
block and three roof coverings (a red roofing tile, a slate-type
tile and sprinkled roof paper). The values of the BRDF were
measured at grid points of 0?,25?,50?,75? for the zenith
angles 0; and 0, respectively, and at 0°,90°, 180° for the az-
imuth difference angle v = |; — b,|,(see figure 1), making
up a total of ca. 35 measured spectra for each sample.
As a reference target we used a commercially available
Spectralon panel (Labsphere Inc., Boulder, Colorado) with
an albedo of p = 0.5 . Since we were not satisfied with
the simplifying assumption of Lambertian behavior of
the Spectralon panel, we adopted the following two step
procedure (the second step was proposed by [Jackson, 1993]):
2.1 Step 1: Laboratory Measurement of the BRDF of
the Spectralon Target ;
In the laboratory measurements, we used a 100 W halogene
bulb as light source. We measured the reflected radiance
L, [W m7?sr7*nm7*] from the Spectralon panel at the com-
binations of angles described above. Integrating L, over the
projected solid angle 2 as defined by [Nicodemus, 1970] and
494
dividing the result by the albedo of the Spectralon yields the
incident irradiance E; [W m^?nm^!]:
Eod JE
1 v=m 0,=5
2 / / 2: L«(0i,v,0.) cos, sin 0,d0,dy (1)
P Jv=0 „=0
These quantities allow to calculate the BRDF of the Spec-
tralon :
Speciralonyy, V, 0.) = PS (2)
For small aperture solid angles, the BRDF can be approxi-
mated by
Spectralon (9. es Ly (6s, V, 0,)
r (8; v, 0.) z ES s (3)
The results agree qualitatively very well with earlier measure-
ments of the BRDF of Spectralon panels with an albedo of
1.0 by [Flasse, 1993] and [Jackson, 1992]. The BRDF values
decrease with large zenith angles. The Spectralon panels with
an albedo of 0.5 have a specular peak, that does not exist for
the Spectralon panels with an albedo of 1.0 . The intensity
of the specular peak increases rapidly with large zenith angles
(see figures 3 and 4).
Our measurements suggest, that the BRDF of Spectralon
obeys Helmholtz's theorem of reciprocity, i. e. , exchanging
incidence and reflection angles does not change the BRDF
value:
f» (0i, v,0.) — f.(0-,v,0i) (4)
This equation was confirmed by the measurement of the
BRDF at 2 x 11 different combinations of angles (0i, v,6,).
The BRDF of the Spectralon panel is presented in figures 3
and 4.
The wavelength dependence of the diffuse component and the
specular component of the BRDF of the Spectralon panel is
linear, see [Meister, 1996].
2.2 Step 2: Outdoor Measurement of the BRDF's of
the selected surfaces
Four measurements of the reflected radiance L,()) are nec
essary in order to obtain the Bidirectional Reflectance Factors
(BRF) of the samples for each combination of angles :
1. L, of the Spectralon panel illuminated by the sun and
skylight
2. L, of the Spectralon panel illuminated by skylight only.
To this aim, the Spectralon panel was cast in shadow.
The contribution of diffuse skylight to the global ir
radiance was 2096 on average, obviously depending
strongly on the angle of incidence 6;.
The difference between these two measurements yields
the radiance AL, reflected by the Spectralon panel
which can be attributed to direct sunlight only. The in-
coming radiance E?'"" from the sun can be calculated
from the BRDF of the Spectralon panel, determined in
step 1:
fSpectraton (8; y, 0) (5)
Ej (0;) — AL. Gi, ” 6.)
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B7. Vienna 1996
"o f" en.