Paper
15 December 2004 The height of homogeneous aerosol atmosphere in visible and IR wavelength range
Victor N. Uzhegov, Yury A. Pkhalagov, Dmitry M. Kabanov, Sergei M. Sakerin, Mikhail V. Panchenko
Author Affiliations +
Proceedings Volume 5743, Eleventh International Symposium on Atmospheric and Ocean Optics/Atmospheric Physics; (2004) https://doi.org/10.1117/12.606315
Event: Eleventh International Symposium on Atmospheric and Ocean Optics/Atmospheric Physics, 2004, Tomsk, Russian Federation
Abstract
The estimates of the “effective” height of the homogeneous aerosol atmosphere in wide wavelength range (0.44 to 3.9 μm) are obtained for the first time on the basis of simultaneous measurements of the spectral transparency of the atmosphere on near-ground long path and in the atmospheric column. This parameter qualitatively characterizes the height of the mixing layer for particles of different size. The spectral aerosol extinction coefficients in the near-ground layer of α(λ) and the optical thickness of the atmosphere τ(λ) were measured. The effective height of the homogeneous atmosphere was defined as H0(λ)=τ(λ)/α(λ).
© (2004) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
Victor N. Uzhegov, Yury A. Pkhalagov, Dmitry M. Kabanov, Sergei M. Sakerin, and Mikhail V. Panchenko "The height of homogeneous aerosol atmosphere in visible and IR wavelength range", Proc. SPIE 5743, Eleventh International Symposium on Atmospheric and Ocean Optics/Atmospheric Physics, (15 December 2004); https://doi.org/10.1117/12.606315
Lens.org Logo
CITATIONS
Cited by 1 scholarly publication.
Advertisement
Advertisement
RIGHTS & PERMISSIONS
Get copyright permission  Get copyright permission on Copyright Marketplace
KEYWORDS
Atmospheric particles

Aerosols

Atmospheric optics

Visible radiation

Mass attenuation coefficient

Atmospheric sciences

Ocean optics

Back to Top