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    THE ELECTRIFICATION OF CLOUD DROPLETS IN NON-PRECIPITATING CUMULI

    Source: Journal of Meteorology:;1952:;volume( 009 ):;issue: 006::page 397
    Author:
    Gunn, Ross
    DOI: 10.1175/1520-0469(1952)009<0397:TEOCDI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The magnitude and character of the electrification of natural cloud-droplets have been investigated. Measurements of the electric field at the surface of non-precipitating clouds show that, as a whole, they are electrically neutral to a good approximation. New airborne apparatus was designed and built to reveal the detailed electrical distribution by separating the electricity carried by the larger droplets from that on the surrounding small particles or air. Measurements in different types of clouds show that the electric charges carried by the cloud elements are large. In warm swelling cumuli at 4,500 feet, the measurements show the following distribution of charge: a. On large cloud-drops centrifuged out and estimated greater than 10 microns diameter Charge usually positive, approximately +3.8 ? 10?6 e.s.u. cm?3. b. On air and tiny drops collected by ion collector, drops estimated less than 10?2 microns diameter Charge usually negative, approximately ?6.1 ? 10?6 e.s.u. cm?3. c. On small cloud-drops missed by both centrifuge and ion collector, estimated to lie between 10?2 and 10 microns diameter. Charge taken as algebraic sum of items (a) and (b), since electric field measurements show cloud is neutral; +2.3 ? 1O?6 e.s.u. cm?3. From these data, the average charge on each of the larger cloud-droplets was estimated to approximate 32 elementary positive units. The centrifuge and the ion filter of the new cloud-analyzer usually capture charges of opposite sign. The measurements emphasize the fundamental electrical character of natural clouds and suggest their stability may be related to electrification.
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      THE ELECTRIFICATION OF CLOUD DROPLETS IN NON-PRECIPITATING CUMULI

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    contributor authorGunn, Ross
    date accessioned2017-06-09T14:10:38Z
    date available2017-06-09T14:10:38Z
    date copyright1952/12/01
    date issued1952
    identifier issn0095-9634
    identifier otherams-13941.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149447
    description abstractThe magnitude and character of the electrification of natural cloud-droplets have been investigated. Measurements of the electric field at the surface of non-precipitating clouds show that, as a whole, they are electrically neutral to a good approximation. New airborne apparatus was designed and built to reveal the detailed electrical distribution by separating the electricity carried by the larger droplets from that on the surrounding small particles or air. Measurements in different types of clouds show that the electric charges carried by the cloud elements are large. In warm swelling cumuli at 4,500 feet, the measurements show the following distribution of charge: a. On large cloud-drops centrifuged out and estimated greater than 10 microns diameter Charge usually positive, approximately +3.8 ? 10?6 e.s.u. cm?3. b. On air and tiny drops collected by ion collector, drops estimated less than 10?2 microns diameter Charge usually negative, approximately ?6.1 ? 10?6 e.s.u. cm?3. c. On small cloud-drops missed by both centrifuge and ion collector, estimated to lie between 10?2 and 10 microns diameter. Charge taken as algebraic sum of items (a) and (b), since electric field measurements show cloud is neutral; +2.3 ? 1O?6 e.s.u. cm?3. From these data, the average charge on each of the larger cloud-droplets was estimated to approximate 32 elementary positive units. The centrifuge and the ion filter of the new cloud-analyzer usually capture charges of opposite sign. The measurements emphasize the fundamental electrical character of natural clouds and suggest their stability may be related to electrification.
    publisherAmerican Meteorological Society
    titleTHE ELECTRIFICATION OF CLOUD DROPLETS IN NON-PRECIPITATING CUMULI
    typeJournal Paper
    journal volume9
    journal issue6
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1952)009<0397:TEOCDI>2.0.CO;2
    journal fristpage397
    journal lastpage402
    treeJournal of Meteorology:;1952:;volume( 009 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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