On the Kolmogorov Constants for the Temperature-Humidity Cospectrum and the Refractive Index SpectrumSource: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 017::page 2399Author:Andreas, Edgar L.
DOI: 10.1175/1520-0469(1987)044<2399:OTKCFT>2.0.CO;2Publisher: 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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contributor author | Andreas, Edgar L. | |
date accessioned | 2017-06-09T14:27:34Z | |
date available | 2017-06-09T14:27:34Z | |
date copyright | 1987/09/01 | |
date issued | 1987 | |
identifier issn | 0022-4928 | |
identifier other | ams-19611.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4155747 | |
description 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. | |
publisher | American Meteorological Society | |
title | On the Kolmogorov Constants for the Temperature-Humidity Cospectrum and the Refractive Index Spectrum | |
type | Journal Paper | |
journal volume | 44 | |
journal issue | 17 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1987)044<2399:OTKCFT>2.0.CO;2 | |
journal fristpage | 2399 | |
journal lastpage | 2406 | |
tree | Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 017 | |
contenttype | Fulltext |