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    Vertical Wind Component Estimates up to 1.2 km above Ground

    Source: Journal of Applied Meteorology:;1970:;volume( 009 ):;issue: 001::page 64
    Author:
    Rider, Laurence J.
    ,
    Armendariz, Manuel
    DOI: 10.1175/1520-0450(1970)009<0064:VWCEUT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Vertical wind components were computed up to 1.2 km from 37 wintertime and 10 summertime balloon observations between 0900 and 1200 local time utilizing the accurate and high-resolution cinetheodolite/Jimsphere system. The mean ascent rate of the Jimsphere was computed from all observations taken on a particular day. The ascent rate was found to be 5.16 m sec?1 for the winter and 5.10 m sec?1 for the summer months. The individual variations of a given observation from the mean ascent rate were assumed to be the vertical component. Variations in balloon ascent caused by variation in drag, anomalous variation in atmospheric density, balloon response to the wind, and aerodynamically induced motions are discussed. Vertical wind components ranged from 10?25 cm sec?1 in a stable atmosphere and 55?100 cm sec?1 under unstable conditions depending on wind speed.
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      Vertical Wind Component Estimates up to 1.2 km above Ground

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4222233
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    contributor authorRider, Laurence J.
    contributor authorArmendariz, Manuel
    date accessioned2017-06-09T17:06:17Z
    date available2017-06-09T17:06:17Z
    date copyright1970/02/01
    date issued1970
    identifier issn0021-8952
    identifier otherams-7945.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4222233
    description abstractVertical wind components were computed up to 1.2 km from 37 wintertime and 10 summertime balloon observations between 0900 and 1200 local time utilizing the accurate and high-resolution cinetheodolite/Jimsphere system. The mean ascent rate of the Jimsphere was computed from all observations taken on a particular day. The ascent rate was found to be 5.16 m sec?1 for the winter and 5.10 m sec?1 for the summer months. The individual variations of a given observation from the mean ascent rate were assumed to be the vertical component. Variations in balloon ascent caused by variation in drag, anomalous variation in atmospheric density, balloon response to the wind, and aerodynamically induced motions are discussed. Vertical wind components ranged from 10?25 cm sec?1 in a stable atmosphere and 55?100 cm sec?1 under unstable conditions depending on wind speed.
    publisherAmerican Meteorological Society
    titleVertical Wind Component Estimates up to 1.2 km above Ground
    typeJournal Paper
    journal volume9
    journal issue1
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1970)009<0064:VWCEUT>2.0.CO;2
    journal fristpage64
    journal lastpage71
    treeJournal of Applied Meteorology:;1970:;volume( 009 ):;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
    yabeshDSpacePersian