Angular Truncation Error of the Integrating Nephelometer in the Fog Droplet Size RangeSource: Journal of Applied Meteorology:;1977:;volume( 016 ):;issue: 002::page 208Author:Fitzgerald, James W.
DOI: 10.1175/1520-0450(1977)016<0210:ATEOTI>2.0.CO;2Publisher: American Meteorological Society
Abstract: Integrating 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.
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| contributor author | Fitzgerald, James W. | |
| date accessioned | 2017-06-09T17:38:58Z | |
| date available | 2017-06-09T17:38:58Z | |
| date copyright | 1977/02/01 | |
| date issued | 1977 | |
| identifier issn | 0021-8952 | |
| identifier other | ams-9238.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4232704 | |
| description abstract | Integrating 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. | |
| publisher | American Meteorological Society | |
| title | Angular Truncation Error of the Integrating Nephelometer in the Fog Droplet Size Range | |
| type | Journal Paper | |
| journal volume | 16 | |
| journal issue | 2 | |
| journal title | Journal of Applied Meteorology | |
| identifier doi | 10.1175/1520-0450(1977)016<0210:ATEOTI>2.0.CO;2 | |
| journal fristpage | 208 | |
| journal lastpage | 213 | |
| tree | Journal of Applied Meteorology:;1977:;volume( 016 ):;issue: 002 | |
| contenttype | Fulltext |