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contributor authorFitzgerald, James W.
date accessioned2017-06-09T17:38:58Z
date available2017-06-09T17:38:58Z
date copyright1977/02/01
date issued1977
identifier issn0021-8952
identifier otherams-9238.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232704
description abstractIntegrating nephelometers have an inherent error, known as the angular truncation error, which arises from the fact that they integrate scattered light intensity over a truncated angular range from ?1 > 0° to ?2 < 180°. Typically, ?1 is between 5° and 10°. Since the proportion of light scattered in the extreme forward direction increases as scatterer size increases, this error can become sizeable for measurements made in fogs. Correction factors ?(α) for angular truncation are computed for spherical water droplets having values of the size parameter α (= πd/?) in the range 3?200, for values of ?1 of 6°?9° and for ?2 = 170°. If monochromatic light of wavelength 0.55 ?m is assumed, this range of α corresponds to droplet diameters between 0.53 and 35 ?m. The magnitude of ?(α) increases nonmonotonically from a value between 1.03 and 1.07 (depending on ?1) for α = 3 to a value between 2.0 and 2.14 for α = 100. In the range 100 < α ≤ 200, ?(α) varies by less than 7%. Angular truncation correction factors applicable to the MRI model 1580 Fog Visinmeter are also computed.
publisherAmerican Meteorological Society
titleAngular Truncation Error of the Integrating Nephelometer in the Fog Droplet Size Range
typeJournal Paper
journal volume16
journal issue2
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1977)016<0210:ATEOTI>2.0.CO;2
journal fristpage208
journal lastpage213
treeJournal of Applied Meteorology:;1977:;volume( 016 ):;issue: 002
contenttypeFulltext


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