2019
DOI: 10.3390/rs11212518
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On Sea Ice Measurement by a C-Band Scatterometer at VV Polarization: Methodology Optimization Based on Computer Simulations

Abstract: We consider sea ice and water microwave backscatter features at the C-band with vertical transmit and receive polarization and present a method for sea ice/water discrimination using a multiple fixed fan-beam satellite scatterometer. The method is based on the criterion of the minimum statistical distance of measured backscatter values to the sea ice and water (CMOD7) geophysical model functions. Implementation of the method is considered both for a typical three fan-beam geometry as well as for a potential fi… Show more

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Cited by 4 publications
(14 citation statements)
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“…Very recently, we have proposed the following sea ice/water discrimination method in [25]. The method uses the statistical distance of measured NRCS values to GMFs of the sea ice or water when the sea ice S ice and water S water summation results, which are compared as follows to decide whether the sea ice or water is observed: are the closest values of the sea ice and water GMFs, respectively, corresponding to the measured i-NRCS value.…”
Section: Methodsmentioning
confidence: 99%
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“…Very recently, we have proposed the following sea ice/water discrimination method in [25]. The method uses the statistical distance of measured NRCS values to GMFs of the sea ice or water when the sea ice S ice and water S water summation results, which are compared as follows to decide whether the sea ice or water is observed: are the closest values of the sea ice and water GMFs, respectively, corresponding to the measured i-NRCS value.…”
Section: Methodsmentioning
confidence: 99%
“…Recently, we have proposed a method for the discrimination of sea ice and water by the current spacecraft scatterometers [25]. The method is based on the criterion of the statistical distance of measured NRCSs to the sea ice GMF and the water GMF.…”
Section: Introductionmentioning
confidence: 99%
See 2 more Smart Citations
“…Recently, we have considered the sea ice/water discrimination method (1) with regard to its adaptation to the typical three fixed fan-beam geometry of a spaceborne scatterometer ASCAT [18]. For that purpose, the water GMF has been represented by CMOD7, and the sea ice GMF has been represented in the azimuthally isotropic form of [17], [20]…”
mentioning
confidence: 99%