PRE-PROCESSING OF DUAL-VIEW FIGOS DATA: TOWARDS OPERATIONAL BRDF
RETRIEVAL
A. Hueni a *, J. Schopfer a , D. Schlâpfer a , M. Kneubuehler a and J. Nieke b
a Remote Sensing Laboratories, University of Zurich, Winterthurerstrasse 190, 8057 Zurich, Switzerland. -
(ahueni, jschopf, dschlapf, kneub)@geo.uzh.ch
b ESA-ESTEC, Noordwijk, The Netherlands, -jens.nieke@esa.int
KEY WORDS: Spectral Database, Metadata, Spectral Processing, BRDF
ABSTRACT:
The Bidirectional Reflectance Distribution Function (BRDF) is an inherent property of natural and manmade materials. Its effects
depend on the illumination/observation geometry and wavelengths and are apparent in groundbased, airborne and spacebome
imagery. The BRDF is a fundamental quantity from which all other illumination/reflection configurations can be derived.
Calibration and validation of hyperspectral images requires knowledge of the BRDF if spectrodirectional effects are to be accounted
for. The BRDF can be retrieved from dual-view field goniometer system (FIGOS) data, which is stored in the spectral database
SPECCHIO. The retrieval must be precluded by pre-processing steps, which apply transformations on the raw field data and
according metadata. SPECCHIO has been updated to support such pre-processing. Intercalibrations of the involved instruments and
temporal corrections lead to a network of operations to be applied to the input data. A generalisation of the processing has led to the
concept of the Space Processing Chain, allowing the flexible combination of modules to form complex processing flows as required
by the goniometer data pre-processing. The newly added support of intercalibration factors in the SPECCHIO data model will be an
important asset in future round robin experiments. The Space Chain approach will operationalise the retrieval of BRDF from dual
view FIGOS data and generally increase the usefulness of the SPECCHIO system by the introduction of user configurable
processing.
1. INTRODUCTION
The BRDF (Bidirectional Reflectance Distribution Function) is
an object inherent property and describes the dependency of an
observed reflectance on the wavelength and the illumination
and observation geometry (Nicodemus et al., 1977). BRDF
effects can be readily identified in airborne and satellite
imagery and do hinder the straightforward utilization of such
data for subsequent analysis, as identical objects can appear to
have differing spectral signatures. The severity of surface
specific BRDF effects in airborne imagery is dependant on the
field of view (FOV), observation direction and orientation of
the flight strip relative to the sun. Effects are most pronounced
with large FOVs and flight directions perpendicular to the solar
principal plane (Beisl, 2001).
Correction of BRDF effects in imagery requires knowledge of
the BRDF of the involved objects to validate or parameterise
according algorithms. The acquisition of spectrodirectional in
situ data is a part of the calibration and validation (CalVal)
activities carried out by the Remote Sensing Laboratories (RSL)
(Nieke et al., 2007; Schopfer et al., 2007b).
Table 1 illustrates the possible combinations of conceptual
illumination and reflection geometries according to Nicodemus
(1977). An isotropic illumination L t is assumed for these
configurations.
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Table 1: Illumination and reflection geometries (adapted from
Nicodemus et al. (1977))
From a geometry point of view, the hemispherical conical
configuration describes the field case where the incoming
radiance originates from the sky (i.e. hemispherical
illumination) and the reflected radiance is sampled by an
instrument with a finite detector size, i.e. the target with area
dA reflects radiance into a solid angle towards the detector.
However, irradiance under field conditions is a mixture of
directional and diffuse, non-homogenous, hemispherical
components as shown in Table 2 (Schaepman-Strub et al.,
2006).
Corresponding author.