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Models of size spectrum of tropospheric aerosol

  • Part 1 Formation and Characteristics of Atmospheric Aerosols
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Atmospheric Aerosols and Nucleation

Part of the book series: Lecture Notes in Physics ((LNP,volume 309))

Abstract

Quality criteria of a model distribution are considered. Information losses due to the nonorthogonality of spectrum-parameters transformation are discussed. Models are compared with a view to approximation accuracy and losses of information. Smerkalov's average tropospheric aerosol spectrum and 271 observed spectra have been used for test. Highest accuracy and lowest losses of information were yielded by the distribution n1 (r) = a/ ((r/rx)k+ (rx/r)1) having power asymptotes on both, the left and the right, sides.

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References

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Paul E. Wagner Gabor Vali

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© 1988 Springer-Verlag

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Tammet, H. (1988). Models of size spectrum of tropospheric aerosol. In: Wagner, P.E., Vali, G. (eds) Atmospheric Aerosols and Nucleation. Lecture Notes in Physics, vol 309. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-50108-8_1020

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  • DOI: https://doi.org/10.1007/3-540-50108-8_1020

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  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-540-50108-4

  • Online ISBN: 978-3-540-45924-8

  • eBook Packages: Springer Book Archive

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