2017
DOI: 10.1002/2016rs006116
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Improved TEC retrieval based on spaceborne PolSAR data

Abstract: It is well known that for Earth observations, the spaceborne synthetic aperture radar (SAR) systems at L‐band can be seriously affected by the ionosphere. Fortunately, the destructive ionospheric information, total electron content (TEC), can be retrieved and removed by model inversion from SAR echoes and becomes a subject of interest for ionospheric research. Considering the system noise and channel phase imbalance, this paper focuses on accurate TEC retrieval from the Faraday rotation angle, which is embedde… Show more

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Cited by 17 publications
(16 citation statements)
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“…A linearly-polarized electromagnetic wave propagating through the ionosphere splits into two circularly-polarized waves, which are equal in energy but rotate in opposite directions [ 7 ]. They recombine a new wave once leaving the ionosphere, but as a result, the new wave experiences a rotation of polarization plane compared with the original wave in the presence of the geomagnetic field and the free electrons in the ionosphere [ 7 , 8 , 9 , 12 ], and this phenomenon is well known as FR. The one-way FRA in radians can be approximately expressed as where is a constant of value of , is the carrier frequency in hertz, is the geomagnetic field intensity in webers per square meter, is the angle between the wave propagation and geomagnetic vector in radians, is the local Total Electron Content (TEC) integrated along the propagation path, measured in TEC units (TECU) of electrons/ , and is the incident angle at the ionospheric altitude in radians.…”
Section: Faraday Rotation Analysismentioning
confidence: 99%
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“…A linearly-polarized electromagnetic wave propagating through the ionosphere splits into two circularly-polarized waves, which are equal in energy but rotate in opposite directions [ 7 ]. They recombine a new wave once leaving the ionosphere, but as a result, the new wave experiences a rotation of polarization plane compared with the original wave in the presence of the geomagnetic field and the free electrons in the ionosphere [ 7 , 8 , 9 , 12 ], and this phenomenon is well known as FR. The one-way FRA in radians can be approximately expressed as where is a constant of value of , is the carrier frequency in hertz, is the geomagnetic field intensity in webers per square meter, is the angle between the wave propagation and geomagnetic vector in radians, is the local Total Electron Content (TEC) integrated along the propagation path, measured in TEC units (TECU) of electrons/ , and is the incident angle at the ionospheric altitude in radians.…”
Section: Faraday Rotation Analysismentioning
confidence: 99%
“…Under the assumption that has no obvious variation in the course of propagation, and ignoring the noise, the measured scattering matrix can be written as [ 6 , 8 , 9 , 11 , 12 ]: where is the overall gain of the system; represents the comprehensive reflection consist of the phase delay of the propagation and the system-dependent phase; represents the channel cross-talk; is the channel imbalance; are the four elements of the true scattering matrix, are the four elements of the measured scattering matrix, respectively.…”
Section: Faraday Rotation Analysismentioning
confidence: 99%
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“…where N matrix is the system noise and Ω denotes the FR angle. According to Equation (1), many methods for FR retrieval have been developed [5][6][7][8]13,14]. In this work, the B&B method is selected as a reference due to its well-known robustness [15,16].…”
Section: Introductionmentioning
confidence: 99%