DocumentCode :
1301692
Title :
Effect of Faraday rotation on L-band interferometric and polarimetric synthetic-aperture radar data
Author :
Rignot, Eric J M
Author_Institution :
Jet Propulsion Lab., California Inst. of Technol., Pasadena, CA, USA
Volume :
38
Issue :
1
fYear :
2000
fDate :
1/1/2000 12:00:00 AM
Firstpage :
383
Lastpage :
390
Abstract :
Electromagnetic waves traveling through the ionosphere undergo a Faraday rotation of the polarization vector, which modifies the polarization and phase characteristics of the electromagnetic signal. Using L-band (λ=24 cm), polarimetric synthetic aperture radar (SAR) data from the shuttle imaging radar C (SIR-C) acquired in 1994, the author simulates the effect of a change in the Faraday rotation angle ψ on spaceborne interferometric and polarimetric data. In one experiment, it was found that phase coherence is reduced by up to 33% when ψ changes between successive data acquisitions. If ψ changes by more than 40°, a differential phase signal, which varies from field to field, appears in the interferogram and impairs the mapping of surface topography and/or the detection of ground deformation. This signal is caused by phase differences between horizontal-polarized and vertical-polarized radar signals from intermediate levels of vegetation canopy, similar to the phase difference measured between H-polarized and V-polarized signals on a single date. In a second experiment, data from the Japanese Earth Resources Satellite (JERS-1) L-band radar acquired in an area of active deforestation in Rondonia, Brazil, are compared with SIR-C L-band polarimetric data acquired at the same incidence, two weeks later, but from a lower orbiting altitude. Large differences in scattering behavior are recorded between the two datasets in the areas of slash and burn forest, which are difficult to reconcile with surface changes. A simulation with SIR-C polarimetric data, however, suggests that those differences are consistent with a Faraday rotation angle of about 30±10° in the JERS-1 data and 0° in the SIR-C data. Based on these two experiments and on Global Positioning System (GPS) records of ionospheric activity, it is concluded that Faraday rotation should not affect the analysis of L-band spaceborne data during periods of low ionospheric activity (solar minima)
Keywords :
Faraday effect; UHF radio propagation; geophysical techniques; ionospheric electromagnetic wave propagation; radar polarimetry; remote sensing by radar; synthetic aperture radar; terrain mapping; vegetation mapping; 24 cm; Faraday rotation; Faraday rotation angle; InSAR; JERS-1; L-band; SAR; SIR-C; UHF; differential phase signal; forest; geophysical measurement technique; ionosphere; land surface; phase characteristics; phase coherence; polarization; radar polarimetry; radiowave propagation; synthetic-aperture radar; terrain mapping; transionospheric propagation; vegetation mapping; Electromagnetic scattering; Electromagnetic wave polarization; Global Positioning System; Ionosphere; L-band; Polarimetric synthetic aperture radar; Radar polarimetry; Spaceborne radar; Surface topography; Synthetic aperture radar;
fLanguage :
English
Journal_Title :
Geoscience and Remote Sensing, IEEE Transactions on
Publisher :
ieee
ISSN :
0196-2892
Type :
jour
DOI :
10.1109/36.823934
Filename :
823934
Link To Document :
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