off the bedrock walls (S.
on). In the case of the
ness retrieval is further
th of the channel and the
, 1997
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vn Ice Stream (location A in
ow of 88 m (blue) to a high
features is apparent between
'esent the displacement over
ted with some modification
nent, Vol. 67, Calculation of
ae area using airborne laser
V.B. Krabill, pp. 194-204
from Elsevier Science.
hown in Figure 3 along with
ived velocities were studied.
n region in the west, where
7 and 1998, as well as two
q Glacier, and the ice margin
f survey pairs are shown in
overlaid on ERS Synthetic
European Space Agency,
of the Jakobshavn Isbrae, the
flow vectors. The boundaries
more stagnant ice are easily
irection and magnitude of the
International Archives of Photogrammetry and Remote Sensing, Vol. 32, Part 3W14, La Jolla, CA, 9-11 Nov. 1999
i Bas The maximum velocity near the calving front is obtained in areas where the standard deviation of topography
ar m per ; 7 i ,
nearly per year was on the order of approximately one meter (Abdalati and
eu | : Krabill, 1999). Smoother surfaces do not produce sufficiently
in views are given for portions of the Kangerdlugssuaq unique correlations in between the reference image sub-section
€ € 1 € 1 € o . x p e
Glacier md the ice margin near 65?N; however, the Jakobshavn in the first observation, and the search image sub-section in the
transects yield the best results, as can be seen in Figure 3. This second.
is because the region has the most distinct topography and
these flights were flown on very clear days. Results could be Results for the Kangerdlugssuaq region were very limited
because on the dates of the later flights, low clouds inhibited
1998 AIM MISSIONS (14 flights)
Figure 3. Maps of 1998 flight trajectory (upper left panel) identifying areas with multiple surveys during the 1998 field season (and 1997
m Case A, the Jakobshavn Isbrae) Retrieved velocity vectors are overlaid on ERS-1 SAR imagery in the other three panels. The SAR
imagery is from the Digital SAR Mosaic provided by the EOSDIS NSIDC Distributed Active Archive Center at the National Snow and
Ice Data Center a he University of Colorado at Boulder. The mosaic was assembled from ERS-1 SAR (© European Space Agency
Copyright 1992), by M. Fahnestock and R. Kwok). The upper right panel is reprinted from Remote Sensing of Environment Vol 67,
Calculation of ice velocities in Jakobshavn Isbrae area using airborne laser altimetry, W. Abdalati, and W.B. Krabill PP. 194-204
Copyright (1999) with permission from Elsevier Science. "re