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    A Readout Technique for the Laser Fog Disdrometer

    Source: Journal of Applied Meteorology:;1966:;volume( 005 ):;issue: 003::page 343
    Author:
    Thompson, Brian J.
    ,
    Parrent, Georgy B.
    ,
    Ward, John H.
    ,
    Justii, Bruce
    DOI: 10.1175/1520-0450(1966)005<0343:ARTFTL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Recently a new instrument termed the laser fog disdrometer was introduced by Silverman, Thompson and Ward. As implied by the name, the function of the instrument is the determination of the size distribution of fog droplets. In design, operation and analysis this instrument represents a significant departure from the customary approaches to the problem. The basic principle of the instrument may be summarized as follows: by suitably storing the diffraction pattern associated with a droplet, both the precise size and location of the droplet may be determined. This principle can be utilized to obtain size distributions without disturbing the statistics of the sample, i.e., finite volumes may be sampled without dilution. Originally, the data were read directly from the diffraction pattern. This type of readout is subject to two fundamental difficulties: 1) the geometry of droplets is difficult to ascertain except for simple structures; 2) if several droplets are relatively near each other in the sample volume, the resultant diffraction pattern is difficult to interpret. This first consideration does not represent a severe limitation for this application; however, it would be a serious limitation in other applications where non-spherical droplets exist. Both of these restrictions, however, are removed by the present readout technique. Physically, the new readout is based on the realization that the diffraction patterns stored by the instrument are, in fact, a new kind of hologram. Hence, the stored diffraction pattern can be used to create a real three-dimensional image of the sample volume. Since the image is fixed in time, the volume may be explored at will and the size and shape of each particle as well as its position relative to the other particles in the sample may be determined. In the present paper the concept and design of the disdrometer is reviewed and the new readout technique is discussed from both a theoretical and experimental point of view. Typical experimental results are also illustrated.
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      A Readout Technique for the Laser Fog Disdrometer

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4215523
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    • Journal of Applied Meteorology

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    contributor authorThompson, Brian J.
    contributor authorParrent, Georgy B.
    contributor authorWard, John H.
    contributor authorJustii, Bruce
    date accessioned2017-06-09T16:44:56Z
    date available2017-06-09T16:44:56Z
    date copyright1966/06/01
    date issued1966
    identifier issn0021-8952
    identifier otherams-7341.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4215523
    description abstractRecently a new instrument termed the laser fog disdrometer was introduced by Silverman, Thompson and Ward. As implied by the name, the function of the instrument is the determination of the size distribution of fog droplets. In design, operation and analysis this instrument represents a significant departure from the customary approaches to the problem. The basic principle of the instrument may be summarized as follows: by suitably storing the diffraction pattern associated with a droplet, both the precise size and location of the droplet may be determined. This principle can be utilized to obtain size distributions without disturbing the statistics of the sample, i.e., finite volumes may be sampled without dilution. Originally, the data were read directly from the diffraction pattern. This type of readout is subject to two fundamental difficulties: 1) the geometry of droplets is difficult to ascertain except for simple structures; 2) if several droplets are relatively near each other in the sample volume, the resultant diffraction pattern is difficult to interpret. This first consideration does not represent a severe limitation for this application; however, it would be a serious limitation in other applications where non-spherical droplets exist. Both of these restrictions, however, are removed by the present readout technique. Physically, the new readout is based on the realization that the diffraction patterns stored by the instrument are, in fact, a new kind of hologram. Hence, the stored diffraction pattern can be used to create a real three-dimensional image of the sample volume. Since the image is fixed in time, the volume may be explored at will and the size and shape of each particle as well as its position relative to the other particles in the sample may be determined. In the present paper the concept and design of the disdrometer is reviewed and the new readout technique is discussed from both a theoretical and experimental point of view. Typical experimental results are also illustrated.
    publisherAmerican Meteorological Society
    titleA Readout Technique for the Laser Fog Disdrometer
    typeJournal Paper
    journal volume5
    journal issue3
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1966)005<0343:ARTFTL>2.0.CO;2
    journal fristpage343
    journal lastpage348
    treeJournal of Applied Meteorology:;1966:;volume( 005 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian