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Application of the Governing Equations to Turbulent Flow

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An Introduction to Boundary Layer Meteorology

Part of the book series: Atmospheric Sciences Library ((ATSL,volume 13))

Abstract

To quantitatively describe and forecast the state of the boundary layer, we turn to the equations of fluid mechanics that describe the dynamics and thermodynamics of the gases in our atmosphere. Motions in the boundary layer are slow enough compared to the speed of light that the Galilean/Newtonian paradigm of classical physics applies. These equations, collectively known as the equations of motion, contain time and space derivatives that require initial and boundary conditions for their solution.

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References

  • André, J.-C, G. De Moor, P. Lacan-ère, G. Therry, and R. du Vachat, 1978: Modeling the 24-hour evolution of the mean and turbulent structure of the planetary boundary layer. J. Amos. Sci. 35 1861–1883.

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  • Businger, J.A., 1982: Equations and concepts. Chapt. 1 in Atmospheric Turbulence and Air Pollution Modelling, Nieuwstadt and van Dop (Editors). Reidel. 358pp.

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  • Carlson, M.A. and R.B. Stull, 1986: Subsidence in the nocturnal boundary layer. J. Climate and Appi Meteor., 25, 1088–1099.

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  • Clarke, R.H., A.J. Dyer, R.R. Brook, D.G. Reid, and A.J. Troup, 1971: The Wangara Experiment: Boundary Layer Data. Div. of Meteor. Physics Tech. Paper No. 19. Commonwealth Scientific and Industrial Research Organization (CSIRO), Australia. 341pp.

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  • Crum, T.D., R.B. Stull, and E.W. Eloranta, 1987: Coincident lidar and aircraft observations of entrainment into thermals and mixed layers. J. Climate and Appi. Meteor., 26, 774–788.

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  • Mahrt, L., 1986: On the shallow motion approximations. J. Atmos. Sci., 43, 1036–1044.

    Article  Google Scholar 

  • Stull, R.B. and E.W. Eloranta, 1984: Boundary layer experiment — 1983.Bull. Am. Meteor. Soc., 65, 450–456.

    Article  Google Scholar 

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© 1988 Kluwer Academic Publishers

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Stull, R.B. (1988). Application of the Governing Equations to Turbulent Flow. In: Stull, R.B. (eds) An Introduction to Boundary Layer Meteorology. Atmospheric Sciences Library, vol 13. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-3027-8_3

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  • DOI: https://doi.org/10.1007/978-94-009-3027-8_3

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-90-277-2769-5

  • Online ISBN: 978-94-009-3027-8

  • eBook Packages: Springer Book Archive

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