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    The Mesoscale and Microscale Structure and Organization of Clouds and Precipitation in Midlatitude Cyclones. I: A Case Study of a Cold Front

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 003::page 568
    Author:
    Hobbs, Peter V.
    ,
    Matejka, Thomas J.
    ,
    Herzegh, Paul H.
    ,
    Locatelli, John D.
    ,
    Houze, Robert A.
    DOI: 10.1175/1520-0469(1980)037<0568:TMAMSA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Detailed information is deduced on the mesoscale organization of precipitation, the structures of the clouds, the air flows associated with mesoscale rainbands, and the precipitation efficiencies and the mechanisms producing precipitation in the rainbands associated with a cold front. Measurements were obtained with quantitative reflectivity and Doppler radars, two instrumented aircraft, serial rawinsondes and a network of ground stations. The regions of heaviest precipitation were organized into a complex mesoscale rainband in the warm-sector air ahead of the front, a narrow band of precipitation at the surface cold front, and four wide cold-frontal rainbands. The wide cold-frontal rainbands and the smaller mesoscale areas of precipitation within them moved with the velocities of the winds between ?3?6 km. The narrow rainband, which was produced by strong convergence and convection in the boundary layer, moved with the speed of the cold front at the surface. A coupled updraft and downdraft was probably responsible for the heavy precipitation on the cold front being organized, on the small mesoscale, into ellipsoidal areas with similar orientations. The precipitation efficiencies in the warm-sector and narrow cold-frontal rainbands were ?40?50% and ?30?50%, respectively. One of the wide cold-frontal rainbands, in which there was a steady production of ice panicles in the main updraft, had a precipitation efficiency of at least 80%, whereas another wide cold-frontal band, in which some precipitation evaporated before reaching the surface, had a precipitation efficiency of ?20%. Ice particles from shallow convective cells aloft played important roles in the production of precipitation in the wide cold-frontal rainbands and in some regions of the warm-sector rainband. These ?seed? ice particles grew by aggregation and by the deposition of vapor as they fell through lower level ?feeder? clouds. About 20% of the mass of the precipitation reaching the ground in the wide cold-frontal rainbands originated in the upper level ?seeder? zones and ?80% in the ?feeder? zones.
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      The Mesoscale and Microscale Structure and Organization of Clouds and Precipitation in Midlatitude Cyclones. I: A Case Study of a Cold Front

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4153808
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    contributor authorHobbs, Peter V.
    contributor authorMatejka, Thomas J.
    contributor authorHerzegh, Paul H.
    contributor authorLocatelli, John D.
    contributor authorHouze, Robert A.
    date accessioned2017-06-09T14:21:19Z
    date available2017-06-09T14:21:19Z
    date copyright1980/03/01
    date issued1980
    identifier issn0022-4928
    identifier otherams-17867.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153808
    description abstractDetailed information is deduced on the mesoscale organization of precipitation, the structures of the clouds, the air flows associated with mesoscale rainbands, and the precipitation efficiencies and the mechanisms producing precipitation in the rainbands associated with a cold front. Measurements were obtained with quantitative reflectivity and Doppler radars, two instrumented aircraft, serial rawinsondes and a network of ground stations. The regions of heaviest precipitation were organized into a complex mesoscale rainband in the warm-sector air ahead of the front, a narrow band of precipitation at the surface cold front, and four wide cold-frontal rainbands. The wide cold-frontal rainbands and the smaller mesoscale areas of precipitation within them moved with the velocities of the winds between ?3?6 km. The narrow rainband, which was produced by strong convergence and convection in the boundary layer, moved with the speed of the cold front at the surface. A coupled updraft and downdraft was probably responsible for the heavy precipitation on the cold front being organized, on the small mesoscale, into ellipsoidal areas with similar orientations. The precipitation efficiencies in the warm-sector and narrow cold-frontal rainbands were ?40?50% and ?30?50%, respectively. One of the wide cold-frontal rainbands, in which there was a steady production of ice panicles in the main updraft, had a precipitation efficiency of at least 80%, whereas another wide cold-frontal band, in which some precipitation evaporated before reaching the surface, had a precipitation efficiency of ?20%. Ice particles from shallow convective cells aloft played important roles in the production of precipitation in the wide cold-frontal rainbands and in some regions of the warm-sector rainband. These ?seed? ice particles grew by aggregation and by the deposition of vapor as they fell through lower level ?feeder? clouds. About 20% of the mass of the precipitation reaching the ground in the wide cold-frontal rainbands originated in the upper level ?seeder? zones and ?80% in the ?feeder? zones.
    publisherAmerican Meteorological Society
    titleThe Mesoscale and Microscale Structure and Organization of Clouds and Precipitation in Midlatitude Cyclones. I: A Case Study of a Cold Front
    typeJournal Paper
    journal volume37
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1980)037<0568:TMAMSA>2.0.CO;2
    journal fristpage568
    journal lastpage596
    treeJournal of the Atmospheric Sciences:;1980:;Volume( 037 ):;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
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