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

    Instability Characteristics of Radar-Derived Mesoscale Organization Modes within Cool-Season Precipitation near Portland, Oregon

    Source: Monthly Weather Review:;2014:;volume( 142 ):;issue: 005::page 1738
    Author:
    Cunningham, Jeffrey G.
    ,
    Yuter, Sandra E.
    DOI: 10.1175/MWR-D-13-00133.1
    Publisher: American Meteorological Society
    Abstract: he instability characteristics associated with different radar-derived mesoscale organization modes are examined using six cool seasons of operational scanning radar data near Portland, Oregon, and operational sounding data from Salem, Oregon. Additionally, several years of Microwave Rain Radar Ka-band vertically pointing radar data from Portland and Merwin, Washington, are used to characterize the nature and occurrence of generating cells and fall streaks. The combination of a new metric, convective-stratiform intermittency, with the classification of radar reflectivity maps into convective and stratiform precipitation types was applied to periods when the freezing level was >1.4-km altitude. This method distinguishes periods with embedded convective within stratiform mesoscale organization from those that were mostly convective or mostly stratiform. Mesoscale organization occurs in a continuum of states with predominantly stratiform structure occurring most frequently. Generating cells in the snow layer are common in cool-season storms and are primarily associated with potential instability aloft. For mostly stratiform and embedded convective within stratiform 3-h periods, the vertically pointing radar data showed nearly ubiquitous fall streaks in the snow layer originating above 3-km altitude. Stronger generating cells enhanced reflectivity in the rain layer consistent with a seeder mechanism. Stronger generating cells were more common during embedded convection within stratiform than in mostly stratiform periods. Nearly all embedded periods have active or latent (potential) instability. Hydrostatic instability more typically occurred at higher altitudes for embedded convective within stratiform periods compared to mostly convective periods. The occurrence of vertical wind shear instability was primary below 2-km altitude and was not typically associated with levels with generating cells.
    • Download: (2.335Mb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      Instability Characteristics of Radar-Derived Mesoscale Organization Modes within Cool-Season Precipitation near Portland, Oregon

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4230209
    Collections
    • Monthly Weather Review

    Show full item record

    contributor authorCunningham, Jeffrey G.
    contributor authorYuter, Sandra E.
    date accessioned2017-06-09T17:31:12Z
    date available2017-06-09T17:31:12Z
    date copyright2014/05/01
    date issued2014
    identifier issn0027-0644
    identifier otherams-86630.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4230209
    description abstracthe instability characteristics associated with different radar-derived mesoscale organization modes are examined using six cool seasons of operational scanning radar data near Portland, Oregon, and operational sounding data from Salem, Oregon. Additionally, several years of Microwave Rain Radar Ka-band vertically pointing radar data from Portland and Merwin, Washington, are used to characterize the nature and occurrence of generating cells and fall streaks. The combination of a new metric, convective-stratiform intermittency, with the classification of radar reflectivity maps into convective and stratiform precipitation types was applied to periods when the freezing level was >1.4-km altitude. This method distinguishes periods with embedded convective within stratiform mesoscale organization from those that were mostly convective or mostly stratiform. Mesoscale organization occurs in a continuum of states with predominantly stratiform structure occurring most frequently. Generating cells in the snow layer are common in cool-season storms and are primarily associated with potential instability aloft. For mostly stratiform and embedded convective within stratiform 3-h periods, the vertically pointing radar data showed nearly ubiquitous fall streaks in the snow layer originating above 3-km altitude. Stronger generating cells enhanced reflectivity in the rain layer consistent with a seeder mechanism. Stronger generating cells were more common during embedded convection within stratiform than in mostly stratiform periods. Nearly all embedded periods have active or latent (potential) instability. Hydrostatic instability more typically occurred at higher altitudes for embedded convective within stratiform periods compared to mostly convective periods. The occurrence of vertical wind shear instability was primary below 2-km altitude and was not typically associated with levels with generating cells.
    publisherAmerican Meteorological Society
    titleInstability Characteristics of Radar-Derived Mesoscale Organization Modes within Cool-Season Precipitation near Portland, Oregon
    typeJournal Paper
    journal volume142
    journal issue5
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR-D-13-00133.1
    journal fristpage1738
    journal lastpage1757
    treeMonthly Weather Review:;2014:;volume( 142 ):;issue: 005
    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