Optical Extinction in Clouds at Multiple Wavelengths

Document ID: 353

Schuster, G. L.1
Esposito, Steven T.1
Philbrick, C. Russell1

1 The Pennsylvania State University, Department of Meteorology
 The Pennsylvania State University, Department of Electrical Engineering and Applied Research Laboratory
 

Presented: United States Naval Academy
Annapolis, Maryland, July 6-10 1998

Report Introduction

The Lidar Atmospheric Profile Sensor, { LAPS) developed at Penn State University is used to measure the total atmospheric extinction coefficient at 28 4 nm, 530 nm, and 607 nm during the Southern California Ozone Study { SCOS). Extinction data at these wavelengths are presented during the development of a low-level cloud. While greater extinction at the ultra-violet {UV) wavelength is observed below the cloud {because of larger contributions of molecular Rayleigh scattering, small particle aerosol scattering and ozone absorption), the visible extinction becomes comparable to the UV extinction at cloud base. A time series of the visible extinction as the cloud grows is presented.

 

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Citation:        "Optical Extinction in Clouds at Multiple Wavelengths", Schuster, G. L., S. T. Esposito, C. R. Philbrick, Nineteenth International Laser Radar Conference, NASA, July 1998, pp. 193 - 194