In: Wagner W., Székely, B. (eds.): ISPRS TC VII Symposium - 100 Years ISPRS, Vienna, Austria, July 5-7, 2010, IAPRS, Vol. XXXVIII, Part 7B
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3.3 Validation of the terrain roughness parameters
In a first processing step the derived terrain roughness layers
(standard deviation of detrended terrain points, mean echo
widths of terrain points) are compared. A linear regression from
both roughness images, according to the formula y = a + b*x,
where x and y represent raster maps was calculated. In addition
to the entire image, subareas were selected, each representing
an individual land cover type (see subareas in Fig. 1) i.e. grass
(3), bushes (2), young (1) and old (4) forest for calculating the
linear regression. Finally, a plausibility check was done by field
investigations. Furthermore, the effect of varying footprint sizes
caused by multiple echoes on the derived echo widths is
studied. To ensure, that only echoes with footprints sizes, which
are in a similar range, are used, only single echoes (i.e.
extended targets) that are below the defined height thresholds
were selected. The selected single echoes are used to generate
additional roughness layers.
4. RESULTS AND DISCUSSION
Fig. 5 shows the standard deviation of the detrended terrain
points as well as mean echo widths of using all echoes. High
standard derivations (bright areas) indicate a high terrain
roughness. Large echo widths (bright areas) are caused by a
certain vertical distribution of scatterers within a laser shot
footprint and hence large echo widths indicate high terrain
roughness. The visual comparison of the derived roughness
layers (Fig. 5) clearly shows similar spatial patterns of areas
with high values of terrain roughness. It can also be shown that
this similarity is apparent for all applied height thresholds. The
highest correlation coefficients (R-0.62 - 0.63) are available for
the roughness layers derived from echoes with heights (dz) less
than 0.25 m and 0.50 m, respectively. The linear regression
between the standard deviation of the detrended terrain points
and the mean echo widths derived from the extended targets
show a slight decrease of the correlation coefficients e.g. for
echoes with dz < 0.5 m from R=0.63 to R=0.58.
Figure 5. Roughness layers derived from FWF-ALS data. Left: Mean standard deviation per raster cell of detrended terrain points for
different height thresholds. Right: Mean echo width per raster cell calculated from terrain and near terrain points respectively.