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Surface Waves in Light Scattering by Spherical and Non-Spherical Particles

  • Petr Chýlek
  • J. T. Kiehl
  • M. K. W. Ko
  • A. Ashkin

Abstract

Resonances in partial wave scattering amplitudes an and bn are responsible for the ripple structure of the extinction curve and for sharp peaks in the backscattering (glory). A connection between the resonances and surface waves is suggested.

Keywords

Surface Wave Partial Wave Extinction Curve Partial Wave Amplitude Extinction Cross Section 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. Ashkin, A., 1970, Phys. Rev. Letters, 24, 156.CrossRefGoogle Scholar
  2. Ashkin, A. and Dziedzic, J. M., 1976, Iys. Rev. Letters, 36, 267.CrossRefGoogle Scholar
  3. Ashkin, A. and Dziedzic, J. M., 1977, Phys. Rev. Letters, 38, 1351.Google Scholar
  4. Chýlek, P., 1973, J. Opt. Soc. Am, 63, 699.CrossRefGoogle Scholar
  5. Chýlek, P., 1976, J. Opt. Soc. Am, 66, 285.CrossRefGoogle Scholar
  6. Chýlek, P., Kiehl, J. and Ko, M., 1978a, Phys. Rev, A18, 2229.CrossRefGoogle Scholar
  7. Chýlek, P., Kiehl, J. and Ko, M., 1978b, Appt. Opt, 17, 3019.CrossRefGoogle Scholar

Copyright information

© Plenum Press, New York 1980

Authors and Affiliations

  • Petr Chýlek
    • 1
    • 2
  • J. T. Kiehl
    • 3
    • 2
  • M. K. W. Ko
    • 4
  • A. Ashkin
    • 5
  1. 1.Atmospheric Sciences Research CenterState Univ. of N.Y. at AlbanyAlbanyUSA
  2. 2.National Center for Atmospheric ResearchBoulderUSA
  3. 3.Department of Atmospheric ScienceState Univ. of N.Y. at AlbanyAlbanyUSA
  4. 4.Atmospheric and Environmental ResearchCambridgeUSA
  5. 5.Bell Telephone LaboratoriesHolmdelUSA

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