In this letter, we introduce the possibility of the sea-surface slope measurements using second-order statistics of return waveforms from sea surface in a continuous-wave radar scatterometer. It has been shown that the estimation of the variance of sea-surface slopes can be obtained by measuring the signal power or the power-spectrum width of return waveforms. We found that the power-spectrum-width-based estimation approach is more sensitive to the variance of the sea-surface slope for weak sea-surface disturbances in contrast to the power-based one.
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%0 Journal Article
%1 Ka2013a
%A Ka, Min-Ho
%A Baskakov, A.I.
%A Terechov, V.A.
%A Kononov, A.A.
%D 2013
%J Geoscience and Remote Sensing Letters, IEEE
%K approach;radar by disturbances;Radar estimation estimation;second-order function;power measurement;weak measurements;Sea measurements;sea-surface noise ocean power radar radar;Surface radar;continuous-wave ratio;Spaceborne scatterometer;power-spectrum-width-based scatterometer;remote sea-surface sensing sensing;sea sensing;sea-surface slope slope;sea-surface spectrum;radar statistics;signal surface;Signal techniques;remote to variance waves;Correlation waves;oceanographic
%N 3
%P 593-597
%R 10.1109/LGRS.2012.2215305
%T Estimation of the Sea-Surface Slope Variance Based on the Power Spectrum Width of a Radar Scatterometer
%V 10
%X In this letter, we introduce the possibility of the sea-surface slope measurements using second-order statistics of return waveforms from sea surface in a continuous-wave radar scatterometer. It has been shown that the estimation of the variance of sea-surface slopes can be obtained by measuring the signal power or the power-spectrum width of return waveforms. We found that the power-spectrum-width-based estimation approach is more sensitive to the variance of the sea-surface slope for weak sea-surface disturbances in contrast to the power-based one.
@article{Ka2013a,
abstract = {In this letter, we introduce the possibility of the sea-surface slope measurements using second-order statistics of return waveforms from sea surface in a continuous-wave radar scatterometer. It has been shown that the estimation of the variance of sea-surface slopes can be obtained by measuring the signal power or the power-spectrum width of return waveforms. We found that the power-spectrum-width-based estimation approach is more sensitive to the variance of the sea-surface slope for weak sea-surface disturbances in contrast to the power-based one.},
added-at = {2015-05-19T04:26:01.000+0200},
author = {Ka, Min-Ho and Baskakov, A.I. and Terechov, V.A. and Kononov, A.A.},
biburl = {https://www.bibsonomy.org/bibtex/2ee979bed4a3d5e9369441c6157437129/starlinq},
doi = {10.1109/LGRS.2012.2215305},
interhash = {c7de6c1e7fb5f08d4d3f83e31584bf89},
intrahash = {ee979bed4a3d5e9369441c6157437129},
issn = {1545-598X},
journal = {Geoscience and Remote Sensing Letters, IEEE},
keywords = {approach;radar by disturbances;Radar estimation estimation;second-order function;power measurement;weak measurements;Sea measurements;sea-surface noise ocean power radar radar;Surface radar;continuous-wave ratio;Spaceborne scatterometer;power-spectrum-width-based scatterometer;remote sea-surface sensing sensing;sea sensing;sea-surface slope slope;sea-surface spectrum;radar statistics;signal surface;Signal techniques;remote to variance waves;Correlation waves;oceanographic},
month = May,
number = 3,
owner = {Vladimir},
pages = {593-597},
timestamp = {2015-05-19T04:27:27.000+0200},
title = {Estimation of the Sea-Surface Slope Variance Based on the Power Spectrum Width of a Radar Scatterometer},
volume = 10,
year = 2013
}