Skip to main content
Log in

A statistical analysis of air pollution data in terms of meteorological conditions

  • Published:
Boundary-Layer Meteorology Aims and scope Submit manuscript

Abstract

The air pollution in the planetary boundary layer (PBL) at a height of about 1 km is considered. Assuming stationarity and horizontal homogeneity of the underlying surface, the turbulent state in the PBL is completely determined by the following external parameters: the Rossby number, one parameter for thermal stratification and two for baroclinicity. The turbulent state in the PBL under the same conditions is also determined completely by the following internal parameters: one for thermal stratification and two for baroclinicity. If the internal or external parameters completely determine the PBL turbulent state, then they should completely determine the diffusion processes in it. That is why for the analysis of pollution data, it is recommended that these representative meteorological parameters should be used rather than selected ones. The external parameters which may be obtained from synoptic data have a definite advantage for statistical processing of air pollution data. This is clearly of importance for forecasting. On the other hand, the connection between pollution and the internal parameters is comparatively well-studied theoretically. That is why for the prediction of pollution, it is necessary to know the dependence between the internal and external parameters, as given by the resistance law. An example of statistical processing of air pollution data in the PBL is treated in terms of the external parameters. In addition, an example is given of a theoretical prediction of pollution using synoptic data.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Clarke, R. H.: 1970, Observational Studies in the Atmospheric Boundary Layer, Quart. J. Roy. Meteorol. Soc. 96, 91–114.

    Google Scholar 

  • Deacon, E. L.: 1973, Geostrophic Drag Coefficients, Boundary-Layer Meteorol. 5, 321–340.

    Google Scholar 

  • Hess, G. D.: 1973, On Rossby-number Similarity Theory for a Baroclinic Planetary Boundary Layer, J. Atmos. Sci. 8, 1722–1723.

    Google Scholar 

  • Monin, A. S. and Zilitinkevich, S. S.: 1966, Planetary Boundary Layer and Large-scale Atmospheric Dynamics, GARP Rep. Study Conf. Stockholm, 1–37.

  • Venkatesh, S. and Csanady, G. T.: 1974; A Baroclinic Planetary Boundary-Layer Model and its Application to the Wangara Data, Boundary-Layer Meteorol. 5, 459–473.

    Google Scholar 

  • Wippermann, F. and Yordanov, D.: 1972; A Perspective for Routine Prediction of Concentration Patterns, Atmos. Envir. 6, 877–888.

    Google Scholar 

  • Yordanov, D.: 1973; Prediction of Concentration Patterns in the Surface Layer under Barotropic and Adiabatic Conditions, Arch. Met. Geoph. Biokl. A, 22, 285–295.

    Google Scholar 

  • Yordanov, D.: 1974: A Simple Baroclinic Model for the Planetary Boundary Layer, Compt. Rend. Akad. Bulg. Sci. (in print).

  • Yordanov, D. and Wippermann, F.: 1972; The Parameterization of the Turbulent Fluxes of Momentum, Heat and Moisture at the Ground in a Baroclinic Planetary Boundary Layer, Beitr. Phys. Atmos. 45, 58–65.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Yordanov, D. A statistical analysis of air pollution data in terms of meteorological conditions. Boundary-Layer Meteorol 11, 27–32 (1977). https://doi.org/10.1007/BF00221821

Download citation

  • Received:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF00221821

Keywords

Navigation