YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Journal of Climate
    • View Item
    •   YE&T Library
    • AMS
    • Journal of Climate
    • 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

    Cloud Liquid Water Climatology from the Special Sensor Microwave/Imager

    Source: Journal of Climate:;1997:;volume( 010 ):;issue: 005::page 1086
    Author:
    Weng, Fuzhong
    ,
    Grody, Norman C.
    ,
    Ferraro, Ralph
    ,
    Basist, Alan
    ,
    Forsyth, David
    DOI: 10.1175/1520-0442(1997)010<1086:CLWCFT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A Special Sensor Microwave/Imager (SSM/I) algorithm is developed to measure both cloud liquid water path (LWP) and cloud frequency (CF) over the oceans. For climate analysis, the LWP and CF parameters are computed on pentad and monthly timescales. Comparisons are made between cloud frequencies obtained from microwave and visible/infrared measurements. It is shown that the SSM/I CF correlates with International Satellite Cloud Climatology Program low- and middle-level cloudiness. Interannual variations of monthly LWP are found to be strongly correlated with El Niño and La Niña events. In general, positive LWP anomalies are associated with positive SST anomalies. However, positive LWP anomalies may also occur in regions of negative SST anomalies. This is probably due to an increase in warm top rain clouds, produced from low-level convergence. When pentads of outgoing longwave radiation data are compared to the LWP, they both show the detailed structure for atmospheric intraseasonal oscillations at 30?60-day periods. However, there are some interesting differences. Finally, as an important application, the monthly LWP is compared with simulations from a general circulation model. While the simulation captures the locations of observed maxima and minima, there is a large discrepancy between the model and measurement for the Northern Hemisphere in summer.
    • Download: (1.462Mb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      Cloud Liquid Water Climatology from the Special Sensor Microwave/Imager

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4187000
    Collections
    • Journal of Climate

    Show full item record

    contributor authorWeng, Fuzhong
    contributor authorGrody, Norman C.
    contributor authorFerraro, Ralph
    contributor authorBasist, Alan
    contributor authorForsyth, David
    date accessioned2017-06-09T15:34:57Z
    date available2017-06-09T15:34:57Z
    date copyright1997/05/01
    date issued1997
    identifier issn0894-8755
    identifier otherams-4774.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4187000
    description abstractA Special Sensor Microwave/Imager (SSM/I) algorithm is developed to measure both cloud liquid water path (LWP) and cloud frequency (CF) over the oceans. For climate analysis, the LWP and CF parameters are computed on pentad and monthly timescales. Comparisons are made between cloud frequencies obtained from microwave and visible/infrared measurements. It is shown that the SSM/I CF correlates with International Satellite Cloud Climatology Program low- and middle-level cloudiness. Interannual variations of monthly LWP are found to be strongly correlated with El Niño and La Niña events. In general, positive LWP anomalies are associated with positive SST anomalies. However, positive LWP anomalies may also occur in regions of negative SST anomalies. This is probably due to an increase in warm top rain clouds, produced from low-level convergence. When pentads of outgoing longwave radiation data are compared to the LWP, they both show the detailed structure for atmospheric intraseasonal oscillations at 30?60-day periods. However, there are some interesting differences. Finally, as an important application, the monthly LWP is compared with simulations from a general circulation model. While the simulation captures the locations of observed maxima and minima, there is a large discrepancy between the model and measurement for the Northern Hemisphere in summer.
    publisherAmerican Meteorological Society
    titleCloud Liquid Water Climatology from the Special Sensor Microwave/Imager
    typeJournal Paper
    journal volume10
    journal issue5
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(1997)010<1086:CLWCFT>2.0.CO;2
    journal fristpage1086
    journal lastpage1098
    treeJournal of Climate:;1997:;volume( 010 ):;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