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    Point Downscaling of Surface Wind Speed for Forecast Applications

    Source: Journal of Applied Meteorology and Climatology:;2018:;volume 057:;issue 003::page 659
    Author:
    Tang, Brian H.
    ,
    Bassill, Nick P.
    DOI: 10.1175/JAMC-D-17-0144.1
    Publisher: American Meteorological Society
    Abstract: AbstractA statistical downscaling algorithm is introduced to forecast surface wind speed at a location. The downscaling algorithm consists of resolved and unresolved components to yield a time series of synthetic wind speeds at high time resolution. The resolved component is a bias-corrected numerical weather prediction model forecast of the 10-m wind speed at the location. The unresolved component is a simulated time series of the high-frequency component of the wind speed that is trained to match the variance and power spectral density of wind observations at the location. Because of the stochastic nature of the unresolved wind speed, the downscaling algorithm may be repeated to yield an ensemble of synthetic wind speeds. The ensemble may be used to generate probabilistic predictions of the sustained wind speed or wind gusts. Verification of the synthetic winds produced by the downscaling algorithm indicates that it can accurately predict various features of the observed wind, such as the probability distribution function of wind speeds, the power spectral density, daily maximum wind gust, and daily maximum sustained wind speed. Thus, the downscaling algorithm may be broadly applicable to any application that requires a computationally efficient, accurate way of generating probabilistic forecasts of wind speed at various time averages or forecast horizons.
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      Point Downscaling of Surface Wind Speed for Forecast Applications

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4261595
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    contributor authorTang, Brian H.
    contributor authorBassill, Nick P.
    date accessioned2019-09-19T10:06:23Z
    date available2019-09-19T10:06:23Z
    date copyright1/29/2018 12:00:00 AM
    date issued2018
    identifier otherjamc-d-17-0144.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4261595
    description abstractAbstractA statistical downscaling algorithm is introduced to forecast surface wind speed at a location. The downscaling algorithm consists of resolved and unresolved components to yield a time series of synthetic wind speeds at high time resolution. The resolved component is a bias-corrected numerical weather prediction model forecast of the 10-m wind speed at the location. The unresolved component is a simulated time series of the high-frequency component of the wind speed that is trained to match the variance and power spectral density of wind observations at the location. Because of the stochastic nature of the unresolved wind speed, the downscaling algorithm may be repeated to yield an ensemble of synthetic wind speeds. The ensemble may be used to generate probabilistic predictions of the sustained wind speed or wind gusts. Verification of the synthetic winds produced by the downscaling algorithm indicates that it can accurately predict various features of the observed wind, such as the probability distribution function of wind speeds, the power spectral density, daily maximum wind gust, and daily maximum sustained wind speed. Thus, the downscaling algorithm may be broadly applicable to any application that requires a computationally efficient, accurate way of generating probabilistic forecasts of wind speed at various time averages or forecast horizons.
    publisherAmerican Meteorological Society
    titlePoint Downscaling of Surface Wind Speed for Forecast Applications
    typeJournal Paper
    journal volume57
    journal issue3
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/JAMC-D-17-0144.1
    journal fristpage659
    journal lastpage674
    treeJournal of Applied Meteorology and Climatology:;2018:;volume 057:;issue 003
    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
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