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Proceedings Paper

Optical Properties Of The Marine Atmospheric Boundary Layer: Aerosol Profiles
Author(s): K. L. Davidson; C. W. Fairall
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Paper Abstract

The distribution of aerosols in the marine boundary layer can be viewed as a dynamic balance of production, transport and removal processes. The balance of these processes can be represented by a simple mixed-layer model. The vertical distribution of aerosols is dominated by turbulent transport. When mixing is dominated by surface shear or cloudtop cooling (as is typical in mid-latitudes), a single "well-mixed" layer is sufficient to describe the aerosol profile. When scattered cumulus clouds are present (called the "trade wind" or "weak cumulus convection" regime), the well-mixed layer is confined to the region below cloud base. In the region above cloudbase and below cloudtops, strong vertical gradients of aerosol concentration may be observed. A simple parameterization of this gradient is presented.

Paper Details

Date Published: 7 August 1986
PDF: 7 pages
Proc. SPIE 0637, Ocean Optics VIII, (7 August 1986); doi: 10.1117/12.964211
Show Author Affiliations
K. L. Davidson, Naval Postgraduate School (United States)
C. W. Fairall, The Pennsylvania State University (United States)

Published in SPIE Proceedings Vol. 0637:
Ocean Optics VIII
Marvin A. Blizard, Editor(s)

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