Get 20M+ Full-Text Papers For Less Than $1.50/day. Start a 14-Day Trial for You or Your Team.

Learn More →

Measurements of Rainfall Properties Using Long Optical Path Imaging

Measurements of Rainfall Properties Using Long Optical Path Imaging Measurements of long-path optical attenuation of visible light due to rainfall are described, from which rainfall parameters are derived. Novel aspects of the method are the use of a distant uncontrolled and broadband spotlight source, and analysis of image characteristics to obtain the distribution of drop radius a. A theory is developed that uses the image attenuation and spatial resolution to retrieve the two parameters, n 0 and ΛΛ, of the distribution n ( a ) == n 0 e −−ΛΛ a . In particular, n 0 is obtained to within about 20%%; this error is relatively small compared to n 0 jumps of more than 100%% commonly observed in rainfall data. The method holds promise as an inexpensive path-averaged remotely sensed method for obtaining rainfall intensity and drop size distributions. Its validity is confirmed by a Monte Carlo model for photon scatter and imaging. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Journal of Atmospheric and Oceanic Technology American Meteorological Society

Measurements of Rainfall Properties Using Long Optical Path Imaging

Loading next page...
 
/lp/american-meteorological-society/measurements-of-rainfall-properties-using-long-optical-path-imaging-wcGNdab1pi

References (13)

Publisher
American Meteorological Society
Copyright
Copyright © 1998 American Meteorological Society
ISSN
1520-0426
DOI
10.1175/1520-0426(2000)017<0761:MORPUL>2.0.CO;2
Publisher site
See Article on Publisher Site

Abstract

Measurements of long-path optical attenuation of visible light due to rainfall are described, from which rainfall parameters are derived. Novel aspects of the method are the use of a distant uncontrolled and broadband spotlight source, and analysis of image characteristics to obtain the distribution of drop radius a. A theory is developed that uses the image attenuation and spatial resolution to retrieve the two parameters, n 0 and ΛΛ, of the distribution n ( a ) == n 0 e −−ΛΛ a . In particular, n 0 is obtained to within about 20%%; this error is relatively small compared to n 0 jumps of more than 100%% commonly observed in rainfall data. The method holds promise as an inexpensive path-averaged remotely sensed method for obtaining rainfall intensity and drop size distributions. Its validity is confirmed by a Monte Carlo model for photon scatter and imaging.

Journal

Journal of Atmospheric and Oceanic TechnologyAmerican Meteorological Society

Published: Sep 16, 1998

There are no references for this article.