Abstract
The growth of a two-dimensional internal boundary layer (IBL), which develops when a neutral or unstably stratified flow over a uniform terrain encounters a step-change in surface roughness, is numerically investigated by a higher-order turbulence closure theory. It is found that the thickness δ of the IBL increases as δ ~ x n, where x is the downstream distance from the roughness-transition line. For a given set of upstream conditions, the value of the exponent n depends only on the Monin-Obukhov length L, and it is approximately independent of the roughness-change parameter M = In (z01/z02). At large fetches, δ increases markedly with increasing instability.
Similar content being viewed by others
References
Blackadar, A. K., Glass, P. E., and Panofsky, H. A.: 1967, ‘Effect of Stability on the Wind Profile Under Conditions of Inhomogeneous Terrain Roughness’, Publ. No. Sc-M-68–191, Sandia Laboratories, Albuquerque, 107–116.
Blackadar, A. K. and Panofsky, H. A.: 1970, ‘The Effects of a Change of Terrain on Wind Profiles’, Rept., Dept. of Meteorology, Penn. State Univ., 83 pp.
Bradley, E. F.: 1968, ‘A Micrometeorological Study of Velocity Profiles and Surface Drag in the Region Modified by a Change in Surface Roughness’, Quart. J. Roy. Meteorol. Soc. 94, 361–379.
Panofsky, H. A.: 1973, ‘Tower Micrometeorology’, in D. A. Haugen (eded.), Workshop on Micrometeorology, Am. Meteorol. Soc., Boston, Mass., 151–176.
Panofsky, H. A.: 1974, private communication.
Panofsky, H. A. and Townsend, A. A.: 1964, ‘Change in Terrain Roughness and Wind Profile’, Quart. J. Roy. Meteorol. Soc. 90, 147–155.
Peterson, E. W.: 1969, ‘On the Relation between the Shear Stress and the Velocity Profile after a Change in Surface Roughness’, J. Atmospheric Sci. 26, 773–774.
Rao, K. S., Wyngaard, J. C., and Coté, O. R.: 1974a, ‘The Structure of Two-Dimensional Internal Boundary Layer over a Sudden Change of Surface Roughness’, J. Atmospheric Sci. 31, 738–746.
Rao, K. S., Wyngaard, J. C., and Coté, O. R.: 1974b, ‘Local Advection of Momentum, Heat, and Moisture in Micrometeorology’, Boundary-Layer Meteorol., 7, 331–348.
Taylor, P. A.: 1970, ‘A Model of Airflow Above Changes in Surface Heat Flux, Temperature and Roughness for Neutral and Unstable Conditions’, Boundary-Layer Meteorol. 1, 18–39.
Wyngaard, J. C., Coté, O. R., and Rao, K. S.: 1974, ‘Modeling the Atmospheric Boundary Layer’, Adv. Geophys. 16A, 193–212, Academic Press Inc., New York.
Author information
Authors and Affiliations
Additional information
NRC-NAS Resident Research Associate at AFCRL, 1973–74
Rights and permissions
About this article
Cite this article
Rao, K.S. Effect of thermal stratification on the growth of the internal boundary layer. Boundary-Layer Meteorol 8, 227–234 (1975). https://doi.org/10.1007/BF00241339
Received:
Issue Date:
DOI: https://doi.org/10.1007/BF00241339