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    A Downscaled Wind Climatology on the Outer Continental Shelf

    Source: Journal of Applied Meteorology and Climatology:;2013:;volume( 052 ):;issue: 008::page 1878
    Author:
    Woods, Bryan K.
    ,
    Nehrkorn, Thomas
    ,
    Henderson, John M.
    DOI: 10.1175/JAMC-D-12-0216.1
    Publisher: American Meteorological Society
    Abstract: 31-yr time series of boundary layer winds has been developed for a region on the outer continental shelf. This simulated time series was designed to be suitable to study the wind resources for a potential offshore wind farm. Reanalysis data were used to initialize a series of high-resolution numerical simulations. The limited number of high-resolution numerical simulations was repeatedly sampled using an analog matching criterion that is based on the reanalysis data to create a 31-yr time series with 500-m spatial resolution and 10-min temporal resolution. Validation against buoy data indicates that combining the reanalysis and resampled high-resolution numerical simulations produces a much more accurate wind speed distribution than does the reanalysis alone. Both the model physics and downscaled resolution may be contributing to the observed performance gains.
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      A Downscaled Wind Climatology on the Outer Continental Shelf

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4217005
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    contributor authorWoods, Bryan K.
    contributor authorNehrkorn, Thomas
    contributor authorHenderson, John M.
    date accessioned2017-06-09T16:49:20Z
    date available2017-06-09T16:49:20Z
    date copyright2013/08/01
    date issued2013
    identifier issn1558-8424
    identifier otherams-74746.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4217005
    description abstract31-yr time series of boundary layer winds has been developed for a region on the outer continental shelf. This simulated time series was designed to be suitable to study the wind resources for a potential offshore wind farm. Reanalysis data were used to initialize a series of high-resolution numerical simulations. The limited number of high-resolution numerical simulations was repeatedly sampled using an analog matching criterion that is based on the reanalysis data to create a 31-yr time series with 500-m spatial resolution and 10-min temporal resolution. Validation against buoy data indicates that combining the reanalysis and resampled high-resolution numerical simulations produces a much more accurate wind speed distribution than does the reanalysis alone. Both the model physics and downscaled resolution may be contributing to the observed performance gains.
    publisherAmerican Meteorological Society
    titleA Downscaled Wind Climatology on the Outer Continental Shelf
    typeJournal Paper
    journal volume52
    journal issue8
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/JAMC-D-12-0216.1
    journal fristpage1878
    journal lastpage1890
    treeJournal of Applied Meteorology and Climatology:;2013:;volume( 052 ):;issue: 008
    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