Abstract
The mixing height (MH), or the height above the surface where pollutants become vertically dispersed, is related to the atmospheric boundary layer (ABL) in homogeneous regions. This layer is characterised by turbulence generated mechanically (from the friction drag of the air moving across the rough and rigid surface of the Earth) and thermally (from the convection process or “bubbling-up” of air parcels from the heated surface). The height of the atmospheric boundary layer (or the depth of surface related influence) is changing in time for a given location depending on the strength of the surface generated mixing and reaches about 1 to 2 km during the day due to heating of the surface by the Sun and about 100 m during the night in conditions of radiative cooling. The boundary layer height changes also depending on the geographical, terrain and vegetation characteristics of a given area [1].
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
Oke, T. R. (1987), Boundary Layer Climates, Methuen, London.
Beyrich, F., Gryning, S.-E., Joffre, S., Rasmussen, A., Seibert, P. and Tercier, P. (1996), On the Determination of the Mixing Height - A Review, in J. G. Kretzschmar and G. Cosemans (Eds), 4th Workshop on Harmonization within Atmospheric Dispersion Modelling for Regulatory Purposes, 6–9 May 1996, Oostende, Belgium, E&M.RA9603,VITO, Belgium, pp. 155–162.
Stull, R. B. (1988), Introduction to Boundary Layer Meteorology, Kluwer Academic Publishers, Dordrecht.
Beyrich, F. (1997), Mixing Height Determination Using Remote Sensing Systems - General Remarks, in S.-E. Gryning, F. Beyrich and E. Batchvarova (Eds), The Determination of the Mixing Height - Current Progress and Problems,EURASAP Workshop Proceedings, 1–3 October 1997, Ris0 National Laboratory, Riso-R997(EN), pp. 71–74.
Gryning, S.-E. and Batchvarova, E. (1990), Analytical model for the growth of the coastal internal boundary layer during onshore flow, Q. J. R. Meteorol. Soc., 116, pp. 187–203.
Gryning, S. and Batchvarova, E. (1994), Parametrization of the Depth of the Entrainment Zone above the Dytime Mixed Layer, Q. J. R. Meteorol. Soc., 120, pp. 47–58.
Batchvarova, E. and Gryning, S.-E. (1994), An Applied Model for the Daytime Mixed Layer and the Entrainment Zone, Boundary-layer Meteorol., 71, pp. 311–323.
Gryning, S.-E. (1998), Some aspects of dispersion in the stratified atmospheric boundary layer over homogeneous terrain, Boundary-layer Meteorol., in print.
Batchvarova, E. and Gryning, S.-E. (1991), Applied model for the growth of the daytime mixed layer, Boundary-Layer Meteorol., 56, 261–274.
Samah, A. A. (1997), Modelling the development of mixing height in near equatorial region, in S.-E. Gryning, F. Beyrich and E. Batchvarova (Eds), The Determination of the Mixing Height - Current Progress and Problems, EURASAP Workshop Proceedings, 1–3 October 1997, Ris0 National Laboratory, Riso-R-997(EN), pp. 3134.
Batchvarova, E. and Gryning, S.-E. (1998), Wind Climatology, Atmospheric Turbulence and Internal Boundary Layer Development in Athens during the MEDCAPHOT-TRACE Experiment, Atmos. Environ., 32, pp. 2055–2069.
Kallos, G., Kossemenos, P. and Pielke, R. (1993), Synoptic and Mesoscale Circulation Assocoated with Air Pollution Episodes in Athens, Greece, Boundary-Layer Meteorol., 62, pp. 163–184.
Lalas, D. P., Tombru-Tsella, M., Petrakis, M., Assimakopoulos, D. N. and Helmis, C. G. (1983), Sea-Breeze Circulation and Photochemical Pollution in Athens, Greece, Atmos. Environ., 17, pp. 1621–1632.
Steyn, D. and Oke, T. R. (1982), The Depth of the Daytime Mixed Layer at Two Coastal Sites: A Model and its Validation, Boundary-Layer Meteorol., 24, pp. 151–180.
Gryning, S.-E. and Batchvarova, E. (1996), A Model for the Height of the Internal Boundary Layer over an Area with an Irregular Coastline, Boundary-Layer Meteorol., 78, pp. 405–413.
Kerman, B. R., Mickle, R. E., Portelli, R. V., Trivett, N. B. and Misra, P. K. (1982), The Nanticoke Shoreline Diffusion Experiment - II. Internal Boundary Layer Structure, Atmos. Environ., 16, pp. 423–437.
Raynor, G. S., SethuRaman, S. and Brown, R. M. (1979), Formation and Characteristics of Coastal Internal Boundary Layers During Onshore Flow, Boundary-Layer Meteorol., 16, pp. 487–514.
Chen, J. M. and Oke, T. R. (1994), Mixed-layer Heat Advection and Entrainment during the Sea Breeze, Boundary-Layer Meteorol., 68, pp. 139–158.
Stunder, M. and SethuRaman, S. (1985), A Comparative Evaluation of the Coastal Internal Boundary-Layer Height Equations, Boundary-Layer Meteorol.,32, pp. 177–204.
Batchvarova, E., Cai, X.-M., Gryning, S.-E. and Steyn, D. (1998), Modelling Internal-Boundary-Layer Development in a region with Complex Coastline, Boundary-layer Meteorol.,in print.
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 1999 Springer Science+Business Media Dordrecht
About this chapter
Cite this chapter
Batchvarova, E. (1999). Mixing Height in Coastal Areas-Experimental Results and Modelling, A Review. In: Zlatev, Z., et al. Large Scale Computations in Air Pollution Modelling. NATO Science Series, vol 57. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-4570-1_6
Download citation
DOI: https://doi.org/10.1007/978-94-011-4570-1_6
Publisher Name: Springer, Dordrecht
Print ISBN: 978-0-7923-5678-3
Online ISBN: 978-94-011-4570-1
eBook Packages: Springer Book Archive