scholarly journals The Effect of Radar Ocean Surface Sampling on Wave Spectrum Estimation Using X-Band Marine Radar

IEEE Access ◽  
2018 ◽  
Vol 6 ◽  
pp. 17570-17585 ◽  
Author(s):  
Al-Abbass Al-Habashneh ◽  
Cecilia Moloney ◽  
Eric W. Gill ◽  
Weimin Huang
2015 ◽  
Vol 7 (12) ◽  
pp. 16537-16554 ◽  
Author(s):  
Al-Abbass Al-Habashneh ◽  
Cecilia Moloney ◽  
Eric Gill ◽  
Weimin Huang

Author(s):  
Victoria Zinchenko ◽  
Leonid Vasilyev ◽  
Svein Olav Halstensen ◽  
Yuming Liu

We demonstrate and verify, by the use of both synthetic and real wave data, a newly developed capability of short-time phase-resolved wave prediction based on incoherent X-band marine radar measurements. An inversion algorithm is developed to convert X-band radar sea surface measurements into the phase-resolved wave field and the associated wave spectrum based on the linear gravity wave theory. The wave components obtained from the reconstruction are then used to initialize the wave propagation model that is used to provide a short-time deterministic forecast of wave field evolution downstream. Both wave spectrum and spatial-temporal wave elevation evolution obtained based on the X-band measurements are compared with the independent point wave measurements by Miros RangeFinder. The agreements between them are reasonably well, which has a significant implication on practical applications of short-time deterministic wave prediction in optimal marine operations.


Sensors ◽  
2021 ◽  
Vol 21 (23) ◽  
pp. 7828
Author(s):  
Jochen Horstmann ◽  
Jan Bödewadt ◽  
Ruben Carrasco ◽  
Marius Cysewski ◽  
Jörg Seemann ◽  
...  

Marine radars are increasingly popular for monitoring meteorological and oceanographic parameters such as ocean surface wind, waves and currents as well as bathymetry and shorelines. Within this paper a coherent on receive marine radar is introduced, which is based on an incoherent off the shelf pulsed X-band radar. The main concept of the coherentization is based on the coherent on receive principle, where the coherence is achieved by measuring the phase of the transmitted pulse from a leak in the radar circulator, which then serves as a reference phase for the transmitted pulse. The Doppler shift frequency can be computed from two consecutive pulse-pairs in the time domain or from the first moment of the Doppler spectrum inferred by means of a short time Fast Fourier Transform. From the Doppler shift frequencies, radial speed maps of the backscatter of the ocean surface are retrieved. The resulting backscatter intensity and Doppler speed maps are presented for horizontal as well as vertical polarization, and discussed with respect to meteorological and oceanographic applications.


2019 ◽  
Vol 11 (9) ◽  
pp. 1031 ◽  
Author(s):  
Zhongbiao Chen ◽  
Biao Zhang ◽  
Vladimir Kudryavtsev ◽  
Yijun He ◽  
Xiaoqing Chu

The cross-spectral correlation approach has been used to estimate the wave spectrum from optical and radar images. This work aims to improve the cross-spectral approach to derive current velocity from the X-band marine radar image sequence, and evaluate the application conditions of the method. To reduce the dependency of gray levels on range and azimuth, radar images are preprocessed by the contrast-limited adaptive histogram equalization. Two-dimensional cross-spectral coherence and phase are derived from neighboring X-band marine radar images, and the phases with large coherences are used to estimate the phase velocity and angular frequency of waves, which are first fitted with the theoretical dispersion relation by different least square models, and then the current velocity can be determined. Compared with the current velocities measured by a current meter, the root-mean-square error, correlation coefficient, bias, and relative error are 0.15 m/s. 0.88, –0.05 m/s, and 7.79% for the north-south velocity, and 0.14 m/s, 0.86, 0.06 m/s, and 10.75% for the east-west velocity in the experimental area, respectively. The preprocessing, critical coherence, and the number of images for applying the cross-spectral approach, are discussed.


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