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    Doppler-Radar Measurements of Clear Air Atmospheric Turbulence at 1290 MHz

    Source: Journal of Applied Meteorology:;1981:;volume( 020 ):;issue: 003::page 266
    Author:
    Balsley, Ben
    ,
    Peterson, Vern L.
    DOI: 10.1175/1520-0450(1981)020<0266:DRMOCA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: We present Doppler-radar observations for the refractivity turbulence structure constant CN2 obtained with the Chatanika Radar Facility, near Fairbanks, Alaska, during a 7-day observing period in October 1976. We find that 1) CN2 typically decreases with altitude above 10 km at a rate of ?1.3 dB km?1. This is considerably less rapid than at low latitudes. 2) Patches of irregularities appear to be advected with the wind. 3) Azimuthal variations of CN2 show no aspect sensitivity with respect to either the topography or the wind direction. 4) Radar echoes do not show evidence of specular reflection at this frequency, in contrast to findings at lower frequencies.
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      Doppler-Radar Measurements of Clear Air Atmospheric Turbulence at 1290 MHz

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4145119
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    • Journal of Applied Meteorology

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    contributor authorBalsley, Ben
    contributor authorPeterson, Vern L.
    date accessioned2017-06-09T13:58:06Z
    date available2017-06-09T13:58:06Z
    date copyright1981/03/01
    date issued1981
    identifier issn0021-8952
    identifier otherams-10045.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145119
    description abstractWe present Doppler-radar observations for the refractivity turbulence structure constant CN2 obtained with the Chatanika Radar Facility, near Fairbanks, Alaska, during a 7-day observing period in October 1976. We find that 1) CN2 typically decreases with altitude above 10 km at a rate of ?1.3 dB km?1. This is considerably less rapid than at low latitudes. 2) Patches of irregularities appear to be advected with the wind. 3) Azimuthal variations of CN2 show no aspect sensitivity with respect to either the topography or the wind direction. 4) Radar echoes do not show evidence of specular reflection at this frequency, in contrast to findings at lower frequencies.
    publisherAmerican Meteorological Society
    titleDoppler-Radar Measurements of Clear Air Atmospheric Turbulence at 1290 MHz
    typeJournal Paper
    journal volume20
    journal issue3
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1981)020<0266:DRMOCA>2.0.CO;2
    journal fristpage266
    journal lastpage274
    treeJournal of Applied Meteorology:;1981:;volume( 020 ):;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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