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    Shallow Angle Wave Profiling Lidar

    Source: Journal of Atmospheric and Oceanic Technology:;2007:;volume( 024 ):;issue: 006::page 1150
    Author:
    Belmont, M. R.
    ,
    Horwood, J. M. K.
    ,
    Thurley, R. W. F.
    ,
    Baker, J.
    DOI: 10.1175/JTECH2032.1
    Publisher: American Meteorological Society
    Abstract: A lidar scanning system is described that is primarily designed to measure sea wave shape. The device is capable of measuring real-time spatial profiles over distances of hundreds of meters, and as the lidar must inevitably operate from modest elevations (e.g., from a vessel?s masthead), it is inherently a very shallow angle metrology device. This results in a highly nonuniform distribution of the wave elevation values. The vertical and horizontal resolution is primarily set by the characteristics of the optical system employed and range/data capacity is set by signal-to-noise ratio considerations. Illustrative data are presented as consecutive profiles taken 0.2 s apart for highly trochoidal waves under conditions where the height was recorded to ±0.03 m and horizontal sample separation to ±0.025 m. A comparison is presented with traditional wave staff measurements.
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      Shallow Angle Wave Profiling Lidar

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4227749
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    contributor authorBelmont, M. R.
    contributor authorHorwood, J. M. K.
    contributor authorThurley, R. W. F.
    contributor authorBaker, J.
    date accessioned2017-06-09T17:23:36Z
    date available2017-06-09T17:23:36Z
    date copyright2007/06/01
    date issued2007
    identifier issn0739-0572
    identifier otherams-84415.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4227749
    description abstractA lidar scanning system is described that is primarily designed to measure sea wave shape. The device is capable of measuring real-time spatial profiles over distances of hundreds of meters, and as the lidar must inevitably operate from modest elevations (e.g., from a vessel?s masthead), it is inherently a very shallow angle metrology device. This results in a highly nonuniform distribution of the wave elevation values. The vertical and horizontal resolution is primarily set by the characteristics of the optical system employed and range/data capacity is set by signal-to-noise ratio considerations. Illustrative data are presented as consecutive profiles taken 0.2 s apart for highly trochoidal waves under conditions where the height was recorded to ±0.03 m and horizontal sample separation to ±0.025 m. A comparison is presented with traditional wave staff measurements.
    publisherAmerican Meteorological Society
    titleShallow Angle Wave Profiling Lidar
    typeJournal Paper
    journal volume24
    journal issue6
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/JTECH2032.1
    journal fristpage1150
    journal lastpage1156
    treeJournal of Atmospheric and Oceanic Technology:;2007:;volume( 024 ):;issue: 006
    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