International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XXXIX-B7, 2012
XXII ISPRS Congress, 25 August — 01 September 2012, Melbourne, Australia
: Figure 9: Liqui-InSAR for Western Turkey coastal zones
6. CONCLUSION AND SUGGESTIONS
The results achieved by combining the available SAR image pairs
of the areas that are acquired successively with maximum temporal
baseline of 16 seconds looks interesting and considerable for the
aquatic bodies. Although it is usually assumed that the application
of SAR Interferometry technique is not worthy for water bodies,
the results suggests different idea. Instantaneous movement of
aquatic bodies is synoptically recognizable using this technique
with sub-centimeter accuracy. It is potentially useful for both the
oceanographic and Earth observation studies.
The parallel baseline component plays key role in producing
interferograms. The direction of sea water movement as well as
rate of displacement can be estimated using this technique.
90
Parviz Farikhi
Knowing the direction of the motion of sea water surface and its
long term trends could be useful for coastal zone management and
the interaction ofsea water and coastal areas. There could be
other potential benefits that need to be further investigated and
studied. By increasing the coverage area of the successive SAR
images access to the information about the behavior of the sea
water movement in larger extent would be possible. A suggestion
could be the use of a system similar to NASA's STS-99 mission
that used two SAR antennas with 60-m separation to collect data
for the Shuttle Radar Topography Mission (SRTM), however the
imaging procedure by two antennas can be carried out with a
small delay ranging between 8 and 15 seconds. The idea needs to
be examined and tested for various cases and different locations.
The wavelength used by radar antenna could also play a key role.
Making the similar experiments, which has been carried out by C-
band SAR systems, for SAR systems that work in other bands
particularly L- and X-bands is expected to show new and
considerable results.
Using single-pass InSAR, the data for same area from different
view angles can be acquired. The temporal and perpendicular
baselines are then tend to zero and as a result the parallel baseline
component remains only that would make precise assessments of
the aquatic body displacement and its direction of motion
possible.
SAR satellites are still few in number, which is the main
limitation in the stream of imagery, and the requirements for
collection of repeat images that can be used to generate
interferograms are stringent. As a result, useful image pairs, even
in large archives of imagery, are not common. The successful
application of InSAR requires seamless cooperation among
several agencies. Further development of this promising technique
depends on expanding and strengthening interagency and
international coordination in the acquisition of SAR data,
including the launching of additional L-band or multiband SAR
satellites.
References
Colwell, Robert N., 1983. Manual of Remote Sensing, Vol. I (2™
ed.). American Society of Photogrammetry, (Chapter 10), pp.
429-475.
Henderson, Floyd M., Lewis, Anthony J., 1998. Principles and
Applications of Imaging Radar, (3 Ed.). John Wiley & Sons,
Inc., (Chapter 6), pp. 359-380.
Kanevsky, Mikhail., 2009. Radar Imaging of the Ocean Waves,
(1* ed.). Oxford, UK: Elsevier B.V., (Chapter 7).
Sacek, Vladimir, 2006. Notes on AMATEUR TELESCOPE
OPTICS, http://www.telescope-optics.net/index.htm (12
December 201 1).
Tarikhi, Parviz, 2009. DEMs from InSAR, Position Magazine,
Issue 43, October & November 2009, pp. 39-42.
Tarikhi, Parviz, 2010a. InSAR: a new generation, Position
Magazine, Issue 50, Dec. 2010 & Jan. 2011, pp.42-46.
Tarikhi, Parviz, 2010b. Using InSAR Technique for Water
Bodies, http://parviztarikhi.wordpress.com/features-2/using-insar-
technique-for-water-bodies/ (10 December 2011)
Thompson, A. Richard, Moran, James M., Swenson, George W.,
2001, Interferometry and Synthesis in Radio Astronomy a
ed.), Wiley-VCH Verlag GmbH
Acknowledgement
All of the SLC images for this study were provided by the
European Space Research Institute (ESRIN) of the European Space
Agency (ESA) to both of which kind appreciations are extended.
P
-
A C) Un "- vr) (o) c) "3 uuu