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    On the Kolmogorov Constants for the Temperature-Humidity Cospectrum and the Refractive Index Spectrum

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 017::page 2399
    Author:
    Andreas, Edgar L.
    DOI: 10.1175/1520-0469(1987)044<2399:OTKCFT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Structure parameters for the temperature (C?2) and humidity (Cq2) spectra and for the temperature-humidity cospectrum (C?q) that I have measured and additional values of C?q/(C?2Cq2)1/2 reported in the literature yield an estimate of the ratio of Kolmogorov constants ??q/(???q)1/2 via the temperature-humidity covariance budget. Here ??, ?q and ??q are the Kolmogorov constants for the temperature and humidity spectra and the temperature-humidity cospectrum, respectively. The data suggest that ??q/(???q)1/2 = 0.80 ± 0.16; consequently, since ?? = ?q0.40 ± 0.02, ??q = 0.32 ± 0.08. Considering the uncertainties involved, however, I cannot reject the hypothesis ?? = ?q =??q. With the dissipation rate (Nn) derived from the refractive index variance budget, and with this apparent equality of ??, ?q, and ??q, the refractive index spectrum (Φn) has the Kolmogorov-Corrsin form Φn(k) = ?nNn??1/3k?5/3 in an inertial-convective subrange, with the Kolmogorov constant ?n also roughly 0.40.
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      On the Kolmogorov Constants for the Temperature-Humidity Cospectrum and the Refractive Index Spectrum

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155747
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    contributor authorAndreas, Edgar L.
    date accessioned2017-06-09T14:27:34Z
    date available2017-06-09T14:27:34Z
    date copyright1987/09/01
    date issued1987
    identifier issn0022-4928
    identifier otherams-19611.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155747
    description abstractStructure parameters for the temperature (C?2) and humidity (Cq2) spectra and for the temperature-humidity cospectrum (C?q) that I have measured and additional values of C?q/(C?2Cq2)1/2 reported in the literature yield an estimate of the ratio of Kolmogorov constants ??q/(???q)1/2 via the temperature-humidity covariance budget. Here ??, ?q and ??q are the Kolmogorov constants for the temperature and humidity spectra and the temperature-humidity cospectrum, respectively. The data suggest that ??q/(???q)1/2 = 0.80 ± 0.16; consequently, since ?? = ?q0.40 ± 0.02, ??q = 0.32 ± 0.08. Considering the uncertainties involved, however, I cannot reject the hypothesis ?? = ?q =??q. With the dissipation rate (Nn) derived from the refractive index variance budget, and with this apparent equality of ??, ?q, and ??q, the refractive index spectrum (Φn) has the Kolmogorov-Corrsin form Φn(k) = ?nNn??1/3k?5/3 in an inertial-convective subrange, with the Kolmogorov constant ?n also roughly 0.40.
    publisherAmerican Meteorological Society
    titleOn the Kolmogorov Constants for the Temperature-Humidity Cospectrum and the Refractive Index Spectrum
    typeJournal Paper
    journal volume44
    journal issue17
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1987)044<2399:OTKCFT>2.0.CO;2
    journal fristpage2399
    journal lastpage2406
    treeJournal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 017
    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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