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    THE NUMBER FLUX OF SNOW CRYSTALS AT THE GROUND

    Source: Monthly Weather Review:;1967:;volume( 095 ):;issue: 012::page 921
    Author:
    GUNN, K. L. S.
    DOI: 10.1175/1520-0493(1967)095<0921:TNFOSC>2.3.CO;2
    Publisher: American Meteorological Society
    Abstract: Many measurements of the snowfall rate R and the average mass per crystal m? have provided values of R/m?, the number of snow crystals reaching unit area of the surface per unit time. A typical number is 1 per cm.2 per sec. Over a whole season's data, the flux is proportional to the snowfall rate. Specifically, two-thirds of the measurements lie within a factor two of a locus R/m? (cm.?2 sec?1) = 1.5 R1,0 where R is in millimeters of water per hour. Thus the principal contribution to any increase in the snowfall rate is the formation of new crystals, rather than the growth of existing ones.
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      THE NUMBER FLUX OF SNOW CRYSTALS AT THE GROUND

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    contributor authorGUNN, K. L. S.
    date accessioned2017-06-09T15:58:35Z
    date available2017-06-09T15:58:35Z
    date copyright1967/12/01
    date issued1967
    identifier issn0027-0644
    identifier otherams-57915.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198304
    description abstractMany measurements of the snowfall rate R and the average mass per crystal m? have provided values of R/m?, the number of snow crystals reaching unit area of the surface per unit time. A typical number is 1 per cm.2 per sec. Over a whole season's data, the flux is proportional to the snowfall rate. Specifically, two-thirds of the measurements lie within a factor two of a locus R/m? (cm.?2 sec?1) = 1.5 R1,0 where R is in millimeters of water per hour. Thus the principal contribution to any increase in the snowfall rate is the formation of new crystals, rather than the growth of existing ones.
    publisherAmerican Meteorological Society
    titleTHE NUMBER FLUX OF SNOW CRYSTALS AT THE GROUND
    typeJournal Paper
    journal volume95
    journal issue12
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1967)095<0921:TNFOSC>2.3.CO;2
    journal fristpage921
    journal lastpage924
    treeMonthly Weather Review:;1967:;volume( 095 ):;issue: 012
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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