Effects of Coincidence on Measurements with a Forward Scattering Spectrometer ProbeSource: Journal of Atmospheric and Oceanic Technology:;1988:;volume( 005 ):;issue: 006::page 823Author:Cooper, William A.
DOI: 10.1175/1520-0426(1988)005<0823:EOCOMW>2.0.CO;2Publisher: American Meteorological Society
Abstract: A PMS Forward Scattering Spectrometer Probe (FSSP) may fail to detect a droplet that enters the illuminated volume in coincidence with another droplet, or such a coincident pair may be assigned an erroneous size. This effect is shown to distort the droplet size spectra measured by the FSSP, and the effects can be quite important in clouds having droplet concentrations exceeding 500 cm?3. The most common coincidence error is one that arises when a droplet within the sample volume of the FSSP is rejected or sized incorrectly because of the coincident passage of another droplet outside that sample volume. Droplet spectra are measured to be too broad, and to contain too many large but too few small droplets, as a result of this effect. Some implications for past and future studies using this probe are discussed.
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contributor author | Cooper, William A. | |
date accessioned | 2017-06-09T15:23:01Z | |
date available | 2017-06-09T15:23:01Z | |
date copyright | 1988/12/01 | |
date issued | 1988 | |
identifier issn | 0739-0572 | |
identifier other | ams-422.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4180845 | |
description abstract | A PMS Forward Scattering Spectrometer Probe (FSSP) may fail to detect a droplet that enters the illuminated volume in coincidence with another droplet, or such a coincident pair may be assigned an erroneous size. This effect is shown to distort the droplet size spectra measured by the FSSP, and the effects can be quite important in clouds having droplet concentrations exceeding 500 cm?3. The most common coincidence error is one that arises when a droplet within the sample volume of the FSSP is rejected or sized incorrectly because of the coincident passage of another droplet outside that sample volume. Droplet spectra are measured to be too broad, and to contain too many large but too few small droplets, as a result of this effect. Some implications for past and future studies using this probe are discussed. | |
publisher | American Meteorological Society | |
title | Effects of Coincidence on Measurements with a Forward Scattering Spectrometer Probe | |
type | Journal Paper | |
journal volume | 5 | |
journal issue | 6 | |
journal title | Journal of Atmospheric and Oceanic Technology | |
identifier doi | 10.1175/1520-0426(1988)005<0823:EOCOMW>2.0.CO;2 | |
journal fristpage | 823 | |
journal lastpage | 832 | |
tree | Journal of Atmospheric and Oceanic Technology:;1988:;volume( 005 ):;issue: 006 | |
contenttype | Fulltext |