820 IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, VOL. 48, NO. 2, FEBRUARY 2010
First Analysis of TerraSAR-X Along-Track
InSAR-Derived Current Fields
Roland Romeiser, Member, IEEE, Steffen Suchandt, Hartmut Runge, Ulrich Steinbrecher, and Steffen Grünler
Abstract—We present the first analysis of surface current fields
derived from TerraSAR-X along-track interferometric synthetic
aperture radar (along-track InSAR, ATI) data. The images were
acquired over the mouth of the Elbe river (Germany) during
six satellite overpasses in spring and summer 2008, using the
experimental “aperture switching” mode of TerraSAR-X. In this
mode, the phased-array synthetic aperture radar (SAR) antenna
is split into two halves for receiving, but in contrast to the “dual
receive antenna” mode, which uses two independent receivers in
parallel, a single receiver is multiplexed to process signals from
the two antenna halves in an alternating manner at a doubled
pulse repetition frequency. The effective ATI baseline is on the
order of 0.8 m. The SAR/ATI raw data processing is described in
another paper in this issue. This paper focuses on the conversion
of the basic interferograms into line-of-sight surface current fields,
which includes an elimination of ship signatures, identification,
and correction (as far as possible) of imaging artifacts, additional
filtering and smoothing, and a subtraction of contributions of wave
motions to detected velocities according to a theoretical model.
We evaluate the quality of the results by comparison with current
fields from a numerical flow model and with available in situ data.
The ATI performance of TerraSAR-X is found to be basically con-
sistent with theoretical expectations. After applying the same data
processing algorithms to all six images, mean differences between
TerraSAR-X-derived currents and reference currents in our main
test area range from -0.11 to +0.08 m/s in five of the six cases with
one outlier at +0.42 m/s. The spatial current variations within
the TerraSAR-X-derived current fields are consistent with the
model in three cases, but unrealistically strong variations across
the images are found in the other three cases. We attribute this to
shortcomings of our preliminary raw data processing algorithms,
which can probably be fixed after some more detailed analysis and
testing. The results obtained so far encourage us to believe that our
internal performance goal of a typical current measuring accuracy
of 0.1 m/s at an effective spatial resolution better than 1 km can
be met.
Manuscript received January 28, 2009; revised June 22, 2009. First published
October 30, 2009; current version published January 20, 2010. This work was
supported in part by the U.S. Office of Naval Research under Grants N00014-
06-1-0931, N00014-08-1-0581, and N00014-09-1-0366 and by the German
Research Foundation (DFG) under Grant STA 410/8-1.
R. Romeiser was with the Institute of Oceanography, Center for Marine and
Climate Research, University of Hamburg, 20146 Hamburg, Germany. He is
now with the Rosenstiel School of Marine and Atmospheric Science, University
of Miami, Miami, FL 33149 USA (e-mail: rromeiser@rsmas.miami.edu).
S. Suchandt and H. Runge are with the Remote Sensing Technology In-
stitute, German Aerospace Center (DLR), 82234 Wessling, Germany (e-mail:
steffen.suchandt@dlr.de; hartmut.runge@dlr.de).
U. Steinbrecher is with the Microwaves and Radar Institute, German
Aerospace Center (DLR), 82234 Wessling, Germany (e-mail: ulrich.
steinbrecher@dlr.de).
S. Grünler is with the Institute of Oceanography, Center for Marine and
Climate Research, University of Hamburg, 20146 Hamburg, Germany (e-mail:
steffen.gruenler@zmaw.de).
Color versions of one or more of the figures in this paper are available online
at http://ieeexplore.ieee.org.
Digital Object Identifier 10.1109/TGRS.2009.2030885
Index Terms—Current measurement, interferometry, radar
data processing, radar imaging, radar signal analysis, radar
velocity measurement, rivers, synthetic aperture radar.
I. I NTRODUCTION
T
HE IDEA of operating TerraSAR-X in an along-track in-
terferometric synthetic aperture radar (along-track InSAR,
ATI) mode for direct target velocity measurements has been
discussed since 2002. The ATI technique—originally devel-
oped in the 1980s at the Jet Propulsion Laboratory, described
for the first time in [1], and demonstrated with an airborne
instrument in [2] and [3]—requires two synthetic aperture radar
(SAR) antennas separated in flight (along-track) direction by a
short distance. The two antennas acquire images of the same
scene with a time lag on the order of milliseconds. Phase
differences between the two complex images are proportional
to the Doppler shift of the backscattered signal and thus to line-
of-sight target velocities. This way, an ATI system permits high-
resolution imaging of surface current fields in the open ocean,
coastal waters, and rivers, which is attractive for a variety of
applications in the fields of oceanographic and hydrological
research, operational monitoring, and offshore engineering.
After a first introduction of the basic instrument design of
TerraSAR-X with 384 individual transmit/receive modules in
[4], the possibility of implementing a “dual receive antenna”
(DRA) mode for ATI, using two halves of the antenna panel as
independent receive antennas, was discussed in [5] and exam-
ined in more detail in [6]. In addition to the original concept
of using the main receiver and an existing backup receiver of
the system in parallel, the idea of an “aperture switching” (AS)
mode was presented in [7] and [8]. In AS mode, a multiplexed
single receiver is used for both antenna halves at a doubled
pulse repetition frequency. This is associated with an increased
noise level, a reduced swath width, and problems with azimuth
ambiguities in the raw data processing, but switching the SAR
from conventional operation to AS mode is a less complex
procedure than switching to DRA mode, thus the AS mode can
be used more easily and more frequently. The requirements of
both ATI modes were taken into account in the hardware and
software developments for TerraSAR-X before launch.
The theoretical performance of TerraSAR-X in DRA and
AS modes for current measurements was analyzed in [9],
based on the numerical ATI imaging model described in [10]
and spaceborne ATI experiences gained with an image of the
Dutch Wadden Sea from the Shuttle Radar Topography Mission
(SRTM) [11]. According to the model simulations, current
measurements with an accuracy of 0.1 m/s and an effective
spatial resolution better than 1 km should be possible in both
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