The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences. Vol. XXXVII. Part B7. Beijing 2008
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is recorded at a different sensor viewing angle (nominally listed
at -/+55°, -/+36°, 0°, (Barnsley et al., 2004)). A total of 16
multi-angular data acquistions between winter 2003 - 2007 have
been performed over the SNP site and nine acquisitions over
VOR, respectively, the latter mainly acquired during the
growing seasons of 2005 and 2006. We have set up a full pre
processing scheme for CHRIS/PROBA data for geometric and
atmospheric processing over mountainous terrain (Kneubiihler
et al., 2005), which is a pre-requisite for subsequent spectro-
directional data analyses.
2.2 Swiss National Park
The study site covered by CHRIS/PROBA data is located near
Ofenpass within the Swiss National Park (10° 14’ E, 46° 40’ N).
The Ofenpass represents an inner-alpine valley at an average
altitude of about 1900 m a.s.l. with an annual precipitation of
900-1100 mm. Embedded in this environment are dry, boreal
type subalpine forests. The south-facing floor of the Ofenpass
valley is considered as the core test site (Figure 1). It has long
been subject to ecological studies (Kotz et al., 2004) and is
described extensively in Schaepman et al. (2005). The forests
are largely dominated by mountain pine (Pinus montana ssp.
arborea) and some stone pine (Pinus cembra) as a second tree
species.
I
L
Smf’ ItaiP
Figure 1: Subset of the geometrically and atmospherically
corrected CHRIS/PROBA nadir scene acquired over the Swiss
National Park study site on 17 February 2004. The Ofenpass
valley stretches from left to right in the central part of the image.
2.3 Vordemwald
The study site Vordemwald (7° 53’ E, 47° 16’ N) is located on
the Swiss Plateau in central Switzerland (Figure 2). The hilly
area is dominated by agricultural fields in the lower parts (450-
500 m a.s.l.) and forests mainly on the hilltops (elevations up to
700 m a.s.l.) Agriculture concentrates on barley, wheat, maize,
sugar beet and pasture land (Kneubiihler et al., 2006). The
forest canopy is composed of a mixture of needle-leaf and
broadleaf species, dominated usually by European beech
(Fagus sylvatica L.) and Norway spruce (Picea abies L.). In
total, nine different species can be found belonging to two plant
functional groups (coniferous (evergreen) and broadleaf
(deciduous) species). 3
Figure 2: Subset of the geometrically and atmospherically
corrected CHRIS/PROBA nadir scene acquired over the study
site Vordemwald on the Swiss Plateau on 26 May 2005.
2.4 Geometric Processing
Since both the SNP and VOR study sites are located in either
high mountainous, rugged or at least hilly terrain, a parametric
approach for geometric correction of each data set of a
CHRIS/PROBA acquisition scenario (up to five viewing angles)
was applied. This approach is based on a three-dimensional (3-
D) physical model (Toutin, 2004) which is implemented in the
commercially available image processing software
PCI/Geomatica (PCI Geomatics, 2006). The method allows us
to achieve a high geometric accuracy with resulting root mean
square errors (RMSE) derived from GCPs at 0.46-0.79 pixels
along track and 0.39-0.73 pixels across track when using a
digital surface model (DSM) (© swisstopo) with 2 m resolution.
2.5 Atmospheric Processing
Atmospheric correction of the CHRIS radiance data was
performed using ATCOR-2/3 (Richter, 1998) which is based on
MODTRAN-4. ATCOR-3 is suitable for atmospheric correction
of sensor data acquired over rugged terrain. The software has
recently been adapted to include the option to process tilted
sensors by accounting for varying path lengths through the
atmosphere and varying transmittance. Validation showed a
good agreement between atmospherically corrected
CHRIS/PROBA data and spectral ground measurements with
deviations within ±1 stdev of the ground measurements of
homogenous targets for most bands. The CHRIS/PROBA data
are geo-corrected Hemispherical-Directional-Reflectance-
Factor (HDRF) data.
3. CASE STUDIES
3.1 Canopy Structure and Heterogeneity Assessment
Multi-angular observations of the reflectance anisotropy have
proven to be diagnostic for structural surface properties, which