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Applied Optics

Applied Optics


  • Vol. 41, Iss. 3 — Jan. 20, 2002
  • pp: 412–423

Pitfalls in atmospheric correction of ocean color imagery: how should aerosol optical properties be computed?

Banghua Yan, Knut Stamnes, Wei Li, Bingquan Chen, Jakob J. Stamnes, and Si-Chee Tsay  »View Author Affiliations

Applied Optics, Vol. 41, Issue 3, pp. 412-423 (2002)

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Current methods for the atmospheric correction of ocean-color imagery rely on the computation of optical properties of a mixture of chemically different aerosol particles through combination of the mixture with it into an effective, single-particle component that has an average refractive index. However, a multi-component approach in which each particle type independently grows and changes its refractive index with increasing humidity is more realistic. Computations based on Mie theory and radiative transfer are used to show that the two approaches result in top-of-the-atmosphere radiances that differ more than the water-leaving radiance. Thus, proper atmospheric correction requires a multicomponent approach for the computation of realistic aerosol optical properties.

© 2002 Optical Society of America

OCIS Codes
(010.1110) Atmospheric and oceanic optics : Aerosols
(010.1290) Atmospheric and oceanic optics : Atmospheric optics
(010.4450) Atmospheric and oceanic optics : Oceanic optics
(290.0290) Scattering : Scattering

Original Manuscript: April 9, 2001
Revised Manuscript: August 20, 2001
Published: January 20, 2002

Banghua Yan, Knut Stamnes, Wei Li, Bingquan Chen, Jakob J. Stamnes, and Si-Chee Tsay, "Pitfalls in atmospheric correction of ocean color imagery: how should aerosol optical properties be computed?," Appl. Opt. 41, 412-423 (2002)

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