Abstract
The structure of the atmospheric boundary layer is discouragingly complex. The variability of the surface conditions as roughness, wetness and temperature provides an infinite variety of boundary conditions that the atmosphere has to respond to, and to this comes the rotation of the earth adding another variable. However all this complexity might be handled by large computers if the flow in the boundary layer was not turbulent. Turbulence is an essential ingredient, which dilute and transfers gases, aerosols and pollutants in the boundary layer. Without turbulence the surface layer would be polluted beyond the level of living. But turbulence is also a source of confusion and easily lets you down because progress in its description and understanding is disappointingly slow.
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References
Panofsky, H. and Dutton, J. A. (1984) Atmospheric Turbulence. Wiley-Interscience, New York.
Pielke, R. (1984) Mesoscale Meteorological Modeling. Academic press. New York.
Mason, P. J. (1988) The Formation of Areally Averaged Roughness Lengths, Quart. J. Roy. Meterol. Soc. 114, 399–420.
Mahrt, L. (1996) The Bulk Aerodynamic Formulation over Heterogeneous Surfaces, Boundary-Layer Meteorol. 78, 87–119.
Mahrt, L. (1999) Surface Heterogeneity and Vertical Structure of the Boundary Layer, Boundary-Layer Meteorol. 96, 33–62.
Batchvarova, E. and Gryning, S.E. (1991) Applied Model for the Growth of the Daytime Mixed Layer, Boundary-Layer Meteorol. 56, 261–274.
Batchvarova, E. and Gryning, S.-E. (1994) An Applied Model for the Height of the Daytime Mixed Layer and the Entrainment Zone, Boundary-Layer Meteorol. 71, 311–323.
Gryning, S.-E. and Batchvarova, E. (1999) Regional Heat Flux over the NOPEX Area Estimated from the Evolution of the Mixed Layer, Agric. For. Meteorol. 98–99, 98–99.
Batchvarova, E. A., Gryning, S.E. and Hasager, C. B. (2001) Regional fluxes of momentum and sensible heat over a sub-arctic landscape during late winter, Boundary-Layer Meteorol. 99, 489–597.
Stull, R.B. (1988) An introduction to boundary Layer Meteorology. Kluwer Academic Pub. Boston.
Wood, N. and Mason, P. (1991) The Influence of Static Stability on the Effective Roughness Lengths for Momentum and Heat Transfer, Quart. J. Roy. Meterol. Soc. 117, 1025–1056.
Harding, R., Gryning, S.-E., Halldin, S. and Lloyd, C. (2001) Progress in the understanding of land/atmosphere exchange at high latitudes, Theoretical and Applied Climatology 70, 5–18.
Gryning, S. E., Batchvarova, E. and De Bruin, H. A. R. (2000) Energy Balance of Sparse Coniferous High-Latitude Forest under Winter Conditions, Boundary-Layer Meteorol. 99, 465–488.
Gryning, S.-E. and Batchvarova, E. (1994) Parametrization of the Depth of the Entrainment Zone above the Daytime Mixed Layer, Quart. J. Roy. Meteorol. Soc. 120, 47–58.
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© 2003 Springer Science+Business Media Dordrecht
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Gryning, SE. (2003). Meteorological Data for Regional Model Validation. In: Melas, D., Syrakov, D. (eds) Air Pollution Processes in Regional Scale. NATO Science Series, vol 30. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-1071-9_12
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DOI: https://doi.org/10.1007/978-94-007-1071-9_12
Publisher Name: Springer, Dordrecht
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