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    Capability of Surface-Based Clear-Air Doppler Radar for Monitoring Meteorological Structure of Elevated Layers

    Source: Journal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 003::page 474
    Author:
    Gossard, Earl E.
    ,
    Chadwick, Russell B.
    ,
    Detman, Thomas R.
    ,
    Gaynor, John
    DOI: 10.1175/1520-0450(1984)023<0474:COSBCA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Radars and acoustic sounding systems sense properties of the turbulence structure of the atmosphere. If atmospheric turbulence can be related to the mean gradient parameters, Doppler radars and acoustic sounders can provide information about height profiles of quantities such as temperature and refractive index as well as wind in stable regions of the atmosphere. In this paper turbulent and mean quantities were measured on the 300 m meteorological tower at the Boulder Atmospheric Observatory near Erie, Colorado, and the relationships between the turbulent and mean gradient quantities were examined in order to evaluate hypotheses for simplifying the kinetic energy balance and refractive index variance equations. FM-CW radar measurements of backscattered power and Doppler spectral width were also made for comparison with tower-measured refractive index spectra and Doppler velocity spectra. Height distributions of the turbulent dissipation rate within stable layers are shown and viscous cutoff radar wavelengths calculated.
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      Capability of Surface-Based Clear-Air Doppler Radar for Monitoring Meteorological Structure of Elevated Layers

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4145831
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    • Journal of Climate and Applied Meteorology

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    contributor authorGossard, Earl E.
    contributor authorChadwick, Russell B.
    contributor authorDetman, Thomas R.
    contributor authorGaynor, John
    date accessioned2017-06-09T14:00:05Z
    date available2017-06-09T14:00:05Z
    date copyright1984/03/01
    date issued1984
    identifier issn0733-3021
    identifier otherams-10687.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145831
    description abstractRadars and acoustic sounding systems sense properties of the turbulence structure of the atmosphere. If atmospheric turbulence can be related to the mean gradient parameters, Doppler radars and acoustic sounders can provide information about height profiles of quantities such as temperature and refractive index as well as wind in stable regions of the atmosphere. In this paper turbulent and mean quantities were measured on the 300 m meteorological tower at the Boulder Atmospheric Observatory near Erie, Colorado, and the relationships between the turbulent and mean gradient quantities were examined in order to evaluate hypotheses for simplifying the kinetic energy balance and refractive index variance equations. FM-CW radar measurements of backscattered power and Doppler spectral width were also made for comparison with tower-measured refractive index spectra and Doppler velocity spectra. Height distributions of the turbulent dissipation rate within stable layers are shown and viscous cutoff radar wavelengths calculated.
    publisherAmerican Meteorological Society
    titleCapability of Surface-Based Clear-Air Doppler Radar for Monitoring Meteorological Structure of Elevated Layers
    typeJournal Paper
    journal volume23
    journal issue3
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1984)023<0474:COSBCA>2.0.CO;2
    journal fristpage474
    journal lastpage485
    treeJournal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 003
    contenttypeFulltext
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    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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