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    Predicted Changes in the Frequency of Extreme Precipitable Water Vapor Events

    Source: Journal of Climate:;2015:;volume( 028 ):;issue: 018::page 7057
    Author:
    Roman, Jacola
    ,
    Knuteson, Robert
    ,
    Ackerman, Steve
    ,
    Revercomb, Hank
    DOI: 10.1175/JCLI-D-14-00679.1
    Publisher: American Meteorological Society
    Abstract: high amount of precipitable water vapor (PWV) is a necessary requirement for heavy precipitation and extreme flooding events. This study determined the predicted shift in extreme PWV from a set of CMIP5 global climate models using the highest emission scenario over three different spatial resolutions (global, zonal, and regional) and four different case regions (India, China, Europe, and eastern United States). For the globe, the frequency of the extreme 1% of PWV events between 2006 and 2030 was predicted to increase by a median factor (herein called an X factor) of 9 by 2075?99. Areas of high PWV, like the tropics, tended toward higher factors. The annual median X factor for India, China, central Europe, and the eastern United States was 24, 17, 15, and 16, respectively. For India, the minimum median X factor was 10 during December?February (DJF) and the maximum was 48 during June?August (JJA). In China, the minimum median X factor (8) occurred during DJF, and the maximum was 42 in JJA. For Europe, DJF and September?November (SON) had the smallest median X factor of 15, whereas JJA had the largest median X factor of 30. The smallest median X factor for the eastern United States (11) occurred during March?May (MAM), whereas the largest median X factor (32) occurred in JJA. Regional X factors were significantly larger than global (1.5?2 times larger), illustrating the importance of regional assessments of extreme PWV. The mean trend in the extreme PWV was approximately linear for all regions with a slope of about 3% decade?1. Observations for 10 (20) years are needed for the extreme PWV to change by an amount that exceeds a 3% (5%) measurement error.
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      Predicted Changes in the Frequency of Extreme Precipitable Water Vapor Events

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4223774
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    • Journal of Climate

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    contributor authorRoman, Jacola
    contributor authorKnuteson, Robert
    contributor authorAckerman, Steve
    contributor authorRevercomb, Hank
    date accessioned2017-06-09T17:11:28Z
    date available2017-06-09T17:11:28Z
    date copyright2015/09/01
    date issued2015
    identifier issn0894-8755
    identifier otherams-80838.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4223774
    description abstracthigh amount of precipitable water vapor (PWV) is a necessary requirement for heavy precipitation and extreme flooding events. This study determined the predicted shift in extreme PWV from a set of CMIP5 global climate models using the highest emission scenario over three different spatial resolutions (global, zonal, and regional) and four different case regions (India, China, Europe, and eastern United States). For the globe, the frequency of the extreme 1% of PWV events between 2006 and 2030 was predicted to increase by a median factor (herein called an X factor) of 9 by 2075?99. Areas of high PWV, like the tropics, tended toward higher factors. The annual median X factor for India, China, central Europe, and the eastern United States was 24, 17, 15, and 16, respectively. For India, the minimum median X factor was 10 during December?February (DJF) and the maximum was 48 during June?August (JJA). In China, the minimum median X factor (8) occurred during DJF, and the maximum was 42 in JJA. For Europe, DJF and September?November (SON) had the smallest median X factor of 15, whereas JJA had the largest median X factor of 30. The smallest median X factor for the eastern United States (11) occurred during March?May (MAM), whereas the largest median X factor (32) occurred in JJA. Regional X factors were significantly larger than global (1.5?2 times larger), illustrating the importance of regional assessments of extreme PWV. The mean trend in the extreme PWV was approximately linear for all regions with a slope of about 3% decade?1. Observations for 10 (20) years are needed for the extreme PWV to change by an amount that exceeds a 3% (5%) measurement error.
    publisherAmerican Meteorological Society
    titlePredicted Changes in the Frequency of Extreme Precipitable Water Vapor Events
    typeJournal Paper
    journal volume28
    journal issue18
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-14-00679.1
    journal fristpage7057
    journal lastpage7070
    treeJournal of Climate:;2015:;volume( 028 ):;issue: 018
    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