Growth of the Mixing Depth and the Diurnal Variation of Vertical Profiles of Temperature and Turbulence Characteristics in the Mixing Layer
Author:
Affiliation:
1. National Research Institute for Pollution and Resources
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/57/2/57_2_159/_pdf
Reference26 articles.
1. Ball, F. K., 1960: Control of inversion height by surface heating. Quart. J. Roy. Meteor. Soc., 86, 483-494.
2. Busch, N. E., S. W. Chang and R. A. Anthes, 1976: A multi-level model of the planetary boundary layer suitable for use with mesoscale dynamic models. J. Appl. Met., 15, 909-919.
3. Carson, D. J., 1973: The development of a dry inversion-capped convectively unstable layer. Quart. J. Roy. Meteor. Soc., 99, 450-467.
4. Deardorff, J. W., G. E. Willis and D. K. Lilly, 1969: Laboratory investigation of non-steady penetrative convection. J. Fluid Mech., 35, 7-31.
5. Deardorff, J. W., G. E. Willis and D. K. Lilly, 1970: Convective velocity and temperature scales for the unstable planetary boundary layer and for Rayleigh convection. J. Atmos. Sci., 27, 1211-1213.
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