YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Monthly Weather Review
    • View Item
    •   YE&T Library
    • AMS
    • Monthly Weather Review
    • View Item
    • All Fields
    • Source Title
    • Year
    • Publisher
    • Title
    • Subject
    • Author
    • DOI
    • ISBN
    Advanced Search
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Archive

    ANALYSIS OF A CASPIAN SEA VORTEX

    Source: Monthly Weather Review:;1965:;volume( 093 ):;issue: 010::page 613
    Author:
    SHENK, WILLIAM E.
    DOI: 10.1175/1520-0493(1965)093<0613:AOACSV>2.3.CO;2
    Publisher: American Meteorological Society
    Abstract: The origin of a small, tight cloud vortex located over the Caspian Sea as viewed by TIROS VII in late November 1963 was investigated. Charts at the mandatory levels from the surface to 500 mb. at 12-hr. intervals were examined. Possible causes of formation that were investigated included upper air circulation effects, mechanical effects induced by the Caucasus Mountains, surface heating from the sea, and association with a cold front. Evidence is presented that the cloud vortex was associated with a frontless circulation. A well-defined upper-level wind circulation is believed to be the major cause for the formation of the cloud spiral.
    • Download: (1.599Mb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      ANALYSIS OF A CASPIAN SEA VORTEX

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4198018
    Collections
    • Monthly Weather Review

    Show full item record

    contributor authorSHENK, WILLIAM E.
    date accessioned2017-06-09T15:57:57Z
    date available2017-06-09T15:57:57Z
    date copyright1965/10/01
    date issued1965
    identifier issn0027-0644
    identifier otherams-57658.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198018
    description abstractThe origin of a small, tight cloud vortex located over the Caspian Sea as viewed by TIROS VII in late November 1963 was investigated. Charts at the mandatory levels from the surface to 500 mb. at 12-hr. intervals were examined. Possible causes of formation that were investigated included upper air circulation effects, mechanical effects induced by the Caucasus Mountains, surface heating from the sea, and association with a cold front. Evidence is presented that the cloud vortex was associated with a frontless circulation. A well-defined upper-level wind circulation is believed to be the major cause for the formation of the cloud spiral.
    publisherAmerican Meteorological Society
    titleANALYSIS OF A CASPIAN SEA VORTEX
    typeJournal Paper
    journal volume93
    journal issue10
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1965)093<0613:AOACSV>2.3.CO;2
    journal fristpage613
    journal lastpage617
    treeMonthly Weather Review:;1965:;volume( 093 ):;issue: 010
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian