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    Ocean Wave Directional Spectra Estimation from an HF Ocean Radar with a Single Antenna Array: Methodology

    Source: Journal of Atmospheric and Oceanic Technology:;2006:;volume( 023 ):;issue: 002::page 268
    Author:
    Hisaki, Yukiharu
    DOI: 10.1175/JTECH1836.1
    Publisher: American Meteorological Society
    Abstract: A method to estimate ocean wave directional spectra using a high-frequency (HF) ocean radar was developed. The governing equations of wave spectra are integral equations of first- and second-order radar cross sections, the wave energy balance equation, and the continuity equation of surface winds. The parameterization of the source function is the same as that in WAM. Furthermore, the method uses the constraints that wave spectral values are smooth in both wave frequency and direction and that the propagation terms are small. The unknowns to be estimated are surface wind vectors at radial grids whose centers are the radar position, and wave spectral values at radial and wave frequency?direction grids. The governing equations are discretized in the radial and wave frequency?direction grids and are converted into a nonlinear minimization problem. Identical twin experiments showed that the present method can estimate wave spectra and dynamically extrapolate wave spectra, even in an inhomogeneous wave field.
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      Ocean Wave Directional Spectra Estimation from an HF Ocean Radar with a Single Antenna Array: Methodology

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4227532
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    contributor authorHisaki, Yukiharu
    date accessioned2017-06-09T17:23:03Z
    date available2017-06-09T17:23:03Z
    date copyright2006/02/01
    date issued2006
    identifier issn0739-0572
    identifier otherams-84220.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4227532
    description abstractA method to estimate ocean wave directional spectra using a high-frequency (HF) ocean radar was developed. The governing equations of wave spectra are integral equations of first- and second-order radar cross sections, the wave energy balance equation, and the continuity equation of surface winds. The parameterization of the source function is the same as that in WAM. Furthermore, the method uses the constraints that wave spectral values are smooth in both wave frequency and direction and that the propagation terms are small. The unknowns to be estimated are surface wind vectors at radial grids whose centers are the radar position, and wave spectral values at radial and wave frequency?direction grids. The governing equations are discretized in the radial and wave frequency?direction grids and are converted into a nonlinear minimization problem. Identical twin experiments showed that the present method can estimate wave spectra and dynamically extrapolate wave spectra, even in an inhomogeneous wave field.
    publisherAmerican Meteorological Society
    titleOcean Wave Directional Spectra Estimation from an HF Ocean Radar with a Single Antenna Array: Methodology
    typeJournal Paper
    journal volume23
    journal issue2
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/JTECH1836.1
    journal fristpage268
    journal lastpage286
    treeJournal of Atmospheric and Oceanic Technology:;2006:;volume( 023 ):;issue: 002
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian