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    The Combined Effect of Temperature and Humidity Fluctuations on Refractive Index

    Source: Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 001::page 43
    Author:
    Wesely, Marvin L.
    DOI: 10.1175/1520-0450(1976)015<0043:TCEOTA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Depending on whether the radiation under consideration is acoustic, visible or microwave, either temperature or humidity fluctuations are ordinarily assumed to be an insignificant source of refractive index fluctuations. For applications in the atmospheric surface layer or in a free convection layer, the value of the local Bowen ratio ?, which is the ratio of sensible to latent heat flux densities, can be used to determine when variations in both temperature T and water vapor pressure e are important considerations. When |?| < 0.3 for applications involving visible radiation, |?| < 0.6 for acoustic radiation, and |?|>0.32 for microwave radiation, both T and e fluctuations have at least a 10% effect on the amplitudes of refractive index fluctuations, provided T and e are highly correlated. If T and e are uncorrelated, this 10% level is |?| < 0.067, |?| < 0.13 and |?| > 1.45 for acoustic, visible and microwave radiation, respectively. With knowledge of ? and the extent of the T and e correlation, refractive index ?fluxes? and structure function coefficients can be calculated from (or inversely, can be used to calculate) the corresponding parameters for temperature and humidity.
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      The Combined Effect of Temperature and Humidity Fluctuations on Refractive Index

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4232458
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    contributor authorWesely, Marvin L.
    date accessioned2017-06-09T17:38:28Z
    date available2017-06-09T17:38:28Z
    date copyright1976/01/01
    date issued1976
    identifier issn0021-8952
    identifier otherams-9016.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232458
    description abstractDepending on whether the radiation under consideration is acoustic, visible or microwave, either temperature or humidity fluctuations are ordinarily assumed to be an insignificant source of refractive index fluctuations. For applications in the atmospheric surface layer or in a free convection layer, the value of the local Bowen ratio ?, which is the ratio of sensible to latent heat flux densities, can be used to determine when variations in both temperature T and water vapor pressure e are important considerations. When |?| < 0.3 for applications involving visible radiation, |?| < 0.6 for acoustic radiation, and |?|>0.32 for microwave radiation, both T and e fluctuations have at least a 10% effect on the amplitudes of refractive index fluctuations, provided T and e are highly correlated. If T and e are uncorrelated, this 10% level is |?| < 0.067, |?| < 0.13 and |?| > 1.45 for acoustic, visible and microwave radiation, respectively. With knowledge of ? and the extent of the T and e correlation, refractive index ?fluxes? and structure function coefficients can be calculated from (or inversely, can be used to calculate) the corresponding parameters for temperature and humidity.
    publisherAmerican Meteorological Society
    titleThe Combined Effect of Temperature and Humidity Fluctuations on Refractive Index
    typeJournal Paper
    journal volume15
    journal issue1
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1976)015<0043:TCEOTA>2.0.CO;2
    journal fristpage43
    journal lastpage49
    treeJournal of Applied Meteorology:;1976:;volume( 015 ):;issue: 001
    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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