Turbulent Vertical Transport due to Thin Intermittent Mixing Layers in the Stratosphere and Other Stable Fluids.

作者: E. M. DEWAN

DOI: 10.1126/SCIENCE.211.4486.1041

关键词:

摘要: Pollution effects in the stratosphere and ocean are exacerbated by buoyant stability. Turbulence such media is confined to thin layers. To estimate vertical transport turbulence, one can view situation as nature's way of simulating finite-difference diffusion equation. This analogy finally yields a diffusivity parameter which valid for this extremely inhomogeneous case.

参考文章(6)
D. Cadet, Vertical wind shear measurements in the lower stratosphere Quarterly Journal of the Royal Meteorological Society. ,vol. 101, pp. 485- 493 ,(1975) , 10.1002/QJ.49710142907
K. A. Browning, Structure of the atmosphere in the vicinity of large-amplitude Kelvin-Helmholtz billows Quarterly Journal of the Royal Meteorological Society. ,vol. 97, pp. 283- 299 ,(1971) , 10.1002/QJ.49709741304
J. D. Woods, Wave-induced shear instability in the summer thermocline Journal of Fluid Mechanics. ,vol. 32, pp. 791- 800 ,(1968) , 10.1017/S0022112068001035
D. Atlas, J. I. Metcalf, J. H. Richter, E. E. Gossard, The Birth of “CAT” and Microscale Turbulence Journal of the Atmospheric Sciences. ,vol. 27, pp. 903- 913 ,(1970) , 10.1175/1520-0469(1970)027<0903:TBOAMT>2.0.CO;2
Damjanovich S, Balázs M, Somogyi B, Rédai I, Changes in the intramembrane viscosity of sheep erythrocytes in the presence of membrane bound proteins. Acta biochimica et biophysica Academiae Scientiarum Hungaricae. ,vol. 15, pp. 177- ,(1980)