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The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences. Vol. XXXVII. Part B4. Beijing 2008
difference between CDED level 1 and SRTM data of Mount
Carleton is described as follows: Mean error -1.2 ± 15.6 m,
absolute error 12.1 m, RMSE 15.6 m, Cl 51.2 m, LE 30.5 m
with 95% of the points to present difference with the range [-
50.0, 47.0 m]. We founded that vertical accuracy is terrain class
dependent. Accuracy particularly suffers on terrain with slope
values higher than 15°. High errors of CDED level 1 are not
typical of sloping regions. Aspect of the terrain influences both
the magnitude and the sign of errors in the difference between
CDED level 1 and SRTM data. But statistically, limited to our
study area, we can only mention the relative concentration of
errors in the NE and N directions. The obtained results proved
that the error is relatively geographic dependent in NE, N
directions and minimized in the other directions. Like other
DEM, CDED are slope-dependent. Mostly for SRTM model,
their accuracy vary in function of the specific vegetation type
(Miliaresis G.C et al. 2005). The role of vegetation was also
assessed in our study. It is shown that in the geographic area
studied, vegetation covers uniformly (various species) 36 x 24
km. Differences are concentrated on broadleaf and there is not a
correlation between the percentage of dominant species and
large range difference. The highest RMSE of 12.7 m among
species is for broadleaf class which is not dominant in the study
area. Assessment of the impact of the vegetation was made
using SRTM (CGIAR-CSI SRTM) and ICESat data. Both
SRTM and ICESat are subject of the influence of the vegetation.
We observed that SRTM is much closed to ICESat, but the
RMSE of 12.7 m confirm the accuracy of ICESat data versus
CDED level 1. The Pearson's correlation between ICESat and
CDED level 1, the tendency of the ICESat’profiles indicated
that data investigated in our study is reliable.
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