The average dissipation rate of turbulent kinetic energy in the neutral and unstable atmospheric surface layer

Journal of Geophysical Research Atmospheres

Volumn 102, Issue D12, 1997, Pages 13423-13432

  Albertson, John D ^a   Parlange, Marc B ^b   Kiely, Gerard ^b   Eichinger, William E ^b  

^a University of Iowa   (United States)

^b NONE

Author keywords

[No Author keywords available]

Indexed keywords

ATMOSPHERE; CONVECTION; TURBULENCE;

ATMOSPHERE; CONVECTION; TURBULENCE;

EID: 16444385573     PISSN: 01480227     EISSN: None     Source Type: Journal    
DOI: 10.1029/96JD03346     Document Type: Article

References (5)

1. Albertson, J.D., M.B. Parlange, G.G. Katul, C.-R. Chu, H. Stricker, and S. Tyler, Sensible heat flux from arid regions: A simple fluxvariance method, Water Resour. Res., 31, 969-973, 1995.
2. Albertson, J.D. , G. Kiely, and M.B. Parlange, Surface fluxes of momentum, heat, and water vapor, in Radiation and Water in the Climate System, edited by E.Raschke, NATO ASI Ser. 1: Global Environ. Change, pp. 59-82, Springer-Verlag, New York, 1996.
3. Anselmet, F., Y. Gagne, E.J. Hopfinger, and R.A. Antonia, High-order velocity structure functions in turbulent shear flows,J. Fluid Mech., 140, 63-89, 1984.
4. Batchelor, G.K., Pressure fluctuations in isotropic turbulence, Proc. Cambridge Philos. Soc., 47, 359-374, 1951.
5. Bernstein, A.B., A new dimensional approach to the flux-gradient approach near the ground, Q. J. R. Meteorol. Soc., 92, 560-566, 1966.