In: Wagner W., Székely, B. (eds.): ISPRS TC VII Symposium - 100 Years ISPRS, Vienna, Austria, July 5-7, 2010, IAPRS, Vol. XXXVIII, Part 7B
4
For the real mass movements, there is very little accuracy gain
by interpolating to lower than 0.1 pixels. As the result of the
control shows, when the movement is only translation, the
magnitude of the deviation is very low. Besides, it seems that,
for the control set, interpolation to more detail level improves
the accuracy further.
Mass movement
Mean
displa
cemen
t(m)
Maxi
mum
displa
cemen
t (m)
Standard
deviation
of
displacem
ent (m)
Maximu
m
velocity
(ma')
Aletsch Rock
slide
1.5
4.2
0.45
0.14
Muragl
Rockglacier
2.4
5.8
1.20
0.45
Ghiacciaio del
Belvedere
Glacier
12.22
18.83
5.0
226
Control
7.50
7.50
0
7.50
Table 2. Summary statistics for the displacement magnitudes
and average velocity of the mass movements and the
translation-only control image as estimated from the matching
of the high-resolution original ortho-images
Figure 1. Displacement vectors on the Ghiacciaio del Belvedere
(Sept - Oct 2001)
Figure 2. Displacement vectors on the Muragl rockglacier
(1981-1994) and Aletsch rockslides (1976 - 2006) from left to
right respectively.
3,3 Relative performance of the sub-pixel precisions
Figure 5 shows the mean deviation between the matching
position of the interpolated image pairs and that of the same
resolution (but original) reference image pairs plotted against
sub-pixel precision for the control set. When the difference
between the images is only the here-applied translation, sub
pixel interpolation of the image intensities up to l/8 th of the
original pixel size prior to matching can perfectly substitute
images of comparable original resolution. This perfect
substitution can be achieved by using bi-cubic interpolation of
the correlation surface only up to l/4 th of the original pixel size.
For example, a 16m resolution image interpolated to 2m using
bi-cubic interpolation before matching performs exactly as a 2m
resolution image pair as long as there is no other source of
difference between the image pairs than rigid translation. But
when the level of detail goes beyond l/8 lh , there appears
deviation between the two. The magnitude of these numbers
depends, of course, on the translation magnitude applied in the
control set. However, the test shows the better performance of
bi-cubic intensity interpolation over the other sub-pixel
algorithms tested.
For all the real mass movement types (Figure 6), as the
difference in pixel size between the coarse resolution and the
reference resolution increases, the deviation of the sub-pixel
matching position from the matching position of the same (but
original) image resolution increases regardless of the algorithm.
This means, not surprisingly, that the sub-pixel algorithm
resembles images of comparable resolution less and less as the
sub-pixel detail increases. At every resolution, the mean
deviation is the lowest when intensity interpolation is used
before matching followed by the bi-cubic interpolation of the
correlation surface. The parabola- and Gaussian-based peak
localisations perform poorer and alike. This confirms the above
results.
Remarkably, at a certain level of sub-pixel detail (about 1/16 th ),
the deviation between the sub-pixel algorithm and same
resolution original image gets so high that interpolating beyond
that level has no meaningful advantage although the control set
gives less deviation even at greater level of detail.
Bi-cubic
(correlation)
Bi-cubic
(intensity)
Gaussian
Parabolic
Sub-pixel precision (pixel)
Figure 3 Accuracy of the different sub-pixel precision
approaches for the control set expressed as the mean deviation
of the matching positions from that of the reference high-
resolution original ortho-images
Sub-pixel precision (pixel)
—■— Bi-cubic
(correlation)
—»— Bi-cubic
—•— Parabolic
—*— Gaussian
No
interpolation
Figure 4 Accuracy of the different sub-pixel precision
approaches expressed as the mean deviation of the matching
positions from that of the reference high-resolution original
ortho-images (averaged for the three mass movement types)