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Автор Yeh, Gour‐Tsyh
Автор Brutsaert, Wilfried
Дата выпуска 1971
dc.description In most previous studies of three‐dimensional turbulent diffusion in the lower atmosphere, it was assumed that the principal axes of the diffusivity tensor coincide with the x direction of the mean wind, with the vertical z, and with the lateral y [Sutton, 1934; Monin, 1959; Laikhtman, 1964; Yeh and Brutsaert, 1971]. Thus the diffusivity was taken as a diagonal tensor with components K<sub>xx</sub>, K<sub>yy</sub>, and K<sub>zz</sub>. However recent experimental evidence [Zubkhovskii and Tsvang, 1966; Wesely et al., 1970] and theoretical analysis [Lettau, 1952; Matsuoka, 1961; Gee and Davies, 1964; Brutsaert, 1970] have suggested that the principal axes of the diffusivity tensor do not coincide with the vertical and the mean wind direction but are tilted and that there is an additional diffusivity, namely an off‐diagonal component K<sub>xz</sub> = K<sub>zx</sub>.
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Копирайт Copyright 1971 by the American Geophysical Union.
Название Sensitivity of the Solution for Heat Flux or Evaporation to Off‐Diagonal Turbulent Diffusivities
Тип letter
DOI 10.1029/WR007i003p00734
Electronic ISSN 1944-7973
Print ISSN 0043-1397
Журнал Water Resources Research
Том 7
Первая страница 734
Последняя страница 735
Выпуск 3
Библиографическая ссылка Brutsaert, W., On the anisotropy of the eddy diffusivity, J. Meteorol. Soc. Jap., 48, 411–416, 1970.
Библиографическая ссылка Brutsaert, W., G. T.Yeh, Implications of a type of empirical evaporation formula for lakes and pans, Water Resour. Res., 64, 1202–1208, 1970a.
Библиографическая ссылка Brutsaert, W., G. T.Yeh, A power wind law for turbulent transfer computations, Water Resour. Res., 65, 1387–1391, 1970b.
Библиографическая ссылка Gee, J. H., D. R.Davies, A further note on horizontal dispersion from an instantaneous ground source, Quart. J. Roy. Meteorol. Soc., 90, 474–480, 1964.
Библиографическая ссылка Laikhtman, D. L., Physics of the Boundary Layer of the Atmosphere, 200, Israel Program for Scientific Translations, Jerusalem, 1964.
Библиографическая ссылка Lettau, H., On eddy diffusion in shear zones, M.I.T. Symp. Geophys. Res. Pap., 19, 437, Cambridge, Massachusetts, 1952.
Библиографическая ссылка Matsuoka, H., Note on two‐dimensional diffusion in the atmospheric surface layer, J. Meteorol. Soc. Jap., 39, 324–330, 1961.
Библиографическая ссылка Monin, A. S., General survey of atmospheric diffusion, Advan. Geophys., 6, 29–40, 1959.
Библиографическая ссылка Sutton, O. G., Wind structure and evaporation in turbulent atmosphere, Proc. Roy. Soc., Ser. A, 146, 701–722, 1934.
Библиографическая ссылка Wesely, M. L., G. W.Thurtell, C. B.Tanner, Eddy correlation measurements of sensible heat flux near the earth's surface, J. Appl. Meteorol., 9, 44–50, 1970.
Библиографическая ссылка Yeh, G. T., W.Brutsaert, Perturbation solution of an equation of atmospheric turbulent diffusion, J. Geophys. Res., 7527, 5173–5178, 1970.
Библиографическая ссылка Yeh, G. T., W.Brutsaert, A numerical solution of the two‐dimensional steady state turbulent transfer equation, Mon. Weather Rev., 1971.
Библиографическая ссылка Zubkhovskii, S. L., L. R.Tsvang, Horizontal turbulent heat flow, Izv. Acad. Sci., USSR, Atmos. Oceanic Phys., 212, 798–799, 1966.

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