Note on Two-dimensional Diffusion in the Atmospheric Surface Layer
Author:
Affiliation:
1. Meteorological Research Institute, Kyoto University
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1923/39/6/39_6_324/_pdf
Reference12 articles.
1. 1. Calder, K.L. (1949): Eddy diffusion and evaporation in flow over aerodynamically smooth and rough surfaces: A treatment based on laboratory laws of turbulent flow with special reference to conditions in the lower atmosphere. J. Mech. Applied Math., 2, 153-176.
2. 2. Davies, D.R. (1954): A note on the two-dimensional equation of diffusion in the atmosphere. Quart. J. Roy. Met. Soc., 84, 429-435, 635.
3. 3. Frost, R. (1946): Turbulence and diffusion in the lower atmosphere. Proc. Roy. Soc., London, A 186, 20-35.
4. 4. Hay, J. S. and Pasquill, F. (1957): Diffusion from a fixed source at a height of a few hundred feet in the atmosphere, J. Fluid Mech., 2, 299-310.
5. 5. Lettau, H. (1951): On eddy diffusion in shear zones. M.I.T. Symposium, Geophys. Res. Pap., No. 19, 437-445.
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1. Effects of shear on the turbulent diffusivity tensor;International Journal of Heat and Mass Transfer;1985-01
2. Sensitivity of the Solution for Heat Flux or Evaporation to Off-Diagonal Turbulent Diffusivities;Water Resources Research;1971-06
3. On the Anisotropy of the Eddy Diffusivity;Journal of the Meteorological Society of Japan. Ser. II;1970
4. A further note on horizontal dispersion from an instantaneous ground source;Quarterly Journal of the Royal Meteorological Society;1964-10
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