Inversion of Nearshore X-Band Radar Images to Sea Surface Elevation Maps
A new method to invert X-band radar images for linear shoaling conditions is proposed. The commonly used approach for this type of inverse problems is the Fourier transform. Unlike in deep water conditions, in the shoaling region, waves are modulated both in terms of wavelength and amplitude. Howeve...
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doaj-043e3c98d3e54f4b9a31737b16f650e02020-11-24T20:53:34ZengMDPI AGRemote Sensing2072-42922018-11-011012191910.3390/rs10121919rs10121919Inversion of Nearshore X-Band Radar Images to Sea Surface Elevation MapsPavel Chernyshov0Teodor Vrecica1Yaron Toledo2School of Mechanical Engineering, Tel Aviv University, Tel Aviv 6997801, IsraelSchool of Mechanical Engineering, Tel Aviv University, Tel Aviv 6997801, IsraelSchool of Mechanical Engineering, Tel Aviv University, Tel Aviv 6997801, IsraelA new method to invert X-band radar images for linear shoaling conditions is proposed. The commonly used approach for this type of inverse problems is the Fourier transform. Unlike in deep water conditions, in the shoaling region, waves are modulated both in terms of wavelength and amplitude. However, Fourier analysis assumes spacial and temporal periodicity, and homogeneity limiting its applicability to this region. In order to overcome these limitations, a wavelet based technique is developed. The proposed technique treats every spatial radar image within the time sequence individually, so no information on the dispersion relation is required. For validation purposes, surface elevation range-time shoaling realizations based on the mild slope equation are prepared. A radar imaging model including tilt and shadowing modulations, speckle noise, and the radar equation is applied to these realizations to provide modeled grazing incidence radar images. The inversion process starts with the application of the continuous wavelet transform independently for each spacial image. The procedure continues with employing a successive range independent modulation transfer function to the wavelet spectra in the wavenumber domain. Then, after a phase shift correction, an inverse continuous wavelet transform is applied. The procedure is finalized by a calibration of the retrieved maps. After the calibration, a thorough comparison between the original and the reconstructed surface elevations is performed. It shows high efficiency of the proposed method in treating wave number and amplitude modulated signals, as well as in addressing local phase shifts due to tilt modulation and noise contamination. The new inversion method is proven to have high accuracy in inhomogeneous conditions. It shows high potential to be implemented for individual wave reconstruction using real aperture radars.https://www.mdpi.com/2072-4292/10/12/1919individual waves retrievalshoaling wavesX-band radarradar imagingwavelet analysis |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Pavel Chernyshov Teodor Vrecica Yaron Toledo |
spellingShingle |
Pavel Chernyshov Teodor Vrecica Yaron Toledo Inversion of Nearshore X-Band Radar Images to Sea Surface Elevation Maps Remote Sensing individual waves retrieval shoaling waves X-band radar radar imaging wavelet analysis |
author_facet |
Pavel Chernyshov Teodor Vrecica Yaron Toledo |
author_sort |
Pavel Chernyshov |
title |
Inversion of Nearshore X-Band Radar Images to Sea Surface Elevation Maps |
title_short |
Inversion of Nearshore X-Band Radar Images to Sea Surface Elevation Maps |
title_full |
Inversion of Nearshore X-Band Radar Images to Sea Surface Elevation Maps |
title_fullStr |
Inversion of Nearshore X-Band Radar Images to Sea Surface Elevation Maps |
title_full_unstemmed |
Inversion of Nearshore X-Band Radar Images to Sea Surface Elevation Maps |
title_sort |
inversion of nearshore x-band radar images to sea surface elevation maps |
publisher |
MDPI AG |
series |
Remote Sensing |
issn |
2072-4292 |
publishDate |
2018-11-01 |
description |
A new method to invert X-band radar images for linear shoaling conditions is proposed. The commonly used approach for this type of inverse problems is the Fourier transform. Unlike in deep water conditions, in the shoaling region, waves are modulated both in terms of wavelength and amplitude. However, Fourier analysis assumes spacial and temporal periodicity, and homogeneity limiting its applicability to this region. In order to overcome these limitations, a wavelet based technique is developed. The proposed technique treats every spatial radar image within the time sequence individually, so no information on the dispersion relation is required. For validation purposes, surface elevation range-time shoaling realizations based on the mild slope equation are prepared. A radar imaging model including tilt and shadowing modulations, speckle noise, and the radar equation is applied to these realizations to provide modeled grazing incidence radar images. The inversion process starts with the application of the continuous wavelet transform independently for each spacial image. The procedure continues with employing a successive range independent modulation transfer function to the wavelet spectra in the wavenumber domain. Then, after a phase shift correction, an inverse continuous wavelet transform is applied. The procedure is finalized by a calibration of the retrieved maps. After the calibration, a thorough comparison between the original and the reconstructed surface elevations is performed. It shows high efficiency of the proposed method in treating wave number and amplitude modulated signals, as well as in addressing local phase shifts due to tilt modulation and noise contamination. The new inversion method is proven to have high accuracy in inhomogeneous conditions. It shows high potential to be implemented for individual wave reconstruction using real aperture radars. |
topic |
individual waves retrieval shoaling waves X-band radar radar imaging wavelet analysis |
url |
https://www.mdpi.com/2072-4292/10/12/1919 |
work_keys_str_mv |
AT pavelchernyshov inversionofnearshorexbandradarimagestoseasurfaceelevationmaps AT teodorvrecica inversionofnearshorexbandradarimagestoseasurfaceelevationmaps AT yarontoledo inversionofnearshorexbandradarimagestoseasurfaceelevationmaps |
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