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Effect of thermal stratification on the growth of the internal boundary layer

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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.

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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.

    Google Scholar 

  • 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.

    Google Scholar 

  • Panofsky, H. A.: 1973, ‘Tower Micrometeorology’, in D. A. Haugen (eded.), Workshop on Micrometeorology, Am. Meteorol. Soc., Boston, Mass., 151–176.

    Google Scholar 

  • 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.

    Google Scholar 

  • 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.

    Google Scholar 

  • 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.

    Google Scholar 

  • 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.

    Google Scholar 

  • 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.

    Google Scholar 

  • 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.

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NRC-NAS Resident Research Associate at AFCRL, 1973–74

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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

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