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    In Situ Aircraft Measurements of the Vertical Distribution of Liquid and Ice Water Content in Midlatitude Mixed-Phase Clouds

    Source: Journal of Applied Meteorology and Climatology:;2012:;volume( 052 ):;issue: 001::page 269
    Author:
    Noh, Yoo-Jeong
    ,
    Seaman, Curtis J.
    ,
    Vonder Haar, Thomas H.
    ,
    Liu, Guosheng
    DOI: 10.1175/JAMC-D-11-0202.1
    Publisher: American Meteorological Society
    Abstract: he vertical distribution of liquid and ice water content and their partitioning is studied using 34 cases of in situ measured microphysical properties in midlatitude mixed-phase clouds, with liquid water path ranging from near zero to ~248 g m?2, total water path ranging from near zero to ~562 g m?2, and cloud-top temperature ranging from ?2° to ?38°C. The 34 profiles were further divided into three cloud types depending on their vertical extents and altitudes. It is found that both the vertical distribution of liquid water within a cloud and the liquid water fraction (of total condensed water) as a function of temperature or relative position in a cloud layer are cloud-type dependent. In particular, it is found that the partitioning between liquid and ice water for midlevel shallow clouds is relatively independent on the vertical position within the cloud while it clearly depends on cloud mean temperature. For synoptic snow clouds, however, liquid water fraction increases with the decrease of altitude within the cloud. While the liquid water fraction in synoptic clouds also decreases with lowering temperature, its magnitude is only about 50% near 0°C.
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      In Situ Aircraft Measurements of the Vertical Distribution of Liquid and Ice Water Content in Midlatitude Mixed-Phase Clouds

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4216836
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    contributor authorNoh, Yoo-Jeong
    contributor authorSeaman, Curtis J.
    contributor authorVonder Haar, Thomas H.
    contributor authorLiu, Guosheng
    date accessioned2017-06-09T16:48:47Z
    date available2017-06-09T16:48:47Z
    date copyright2013/01/01
    date issued2012
    identifier issn1558-8424
    identifier otherams-74594.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4216836
    description abstracthe vertical distribution of liquid and ice water content and their partitioning is studied using 34 cases of in situ measured microphysical properties in midlatitude mixed-phase clouds, with liquid water path ranging from near zero to ~248 g m?2, total water path ranging from near zero to ~562 g m?2, and cloud-top temperature ranging from ?2° to ?38°C. The 34 profiles were further divided into three cloud types depending on their vertical extents and altitudes. It is found that both the vertical distribution of liquid water within a cloud and the liquid water fraction (of total condensed water) as a function of temperature or relative position in a cloud layer are cloud-type dependent. In particular, it is found that the partitioning between liquid and ice water for midlevel shallow clouds is relatively independent on the vertical position within the cloud while it clearly depends on cloud mean temperature. For synoptic snow clouds, however, liquid water fraction increases with the decrease of altitude within the cloud. While the liquid water fraction in synoptic clouds also decreases with lowering temperature, its magnitude is only about 50% near 0°C.
    publisherAmerican Meteorological Society
    titleIn Situ Aircraft Measurements of the Vertical Distribution of Liquid and Ice Water Content in Midlatitude Mixed-Phase Clouds
    typeJournal Paper
    journal volume52
    journal issue1
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/JAMC-D-11-0202.1
    journal fristpage269
    journal lastpage279
    treeJournal of Applied Meteorology and Climatology:;2012:;volume( 052 ):;issue: 001
    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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