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    Time-to-Detect Trends in Precipitable Water Vapor with Varying Measurement Error

    Source: Journal of Climate:;2014:;volume( 027 ):;issue: 021::page 8259
    Author:
    Roman, Jacola
    ,
    Knuteson, Robert
    ,
    Ackerman, Steve
    DOI: 10.1175/JCLI-D-13-00736.1
    Publisher: American Meteorological Society
    Abstract: his study determined the theoretical time-to-detect (TTD) global climate model (GCM) precipitable water vapor (PWV) 100-yr trends when realistic measurement errors are considered. Global trends ranged from 0.055 to 0.072 mm yr?1 and varied minimally from season to season. Global TTDs with a 0% measurement error ranged from 3.0 to 4.8 yr, while a 5% measurement error increased the TTD by almost 6 times, ranging from 17.6 to 22.0 yr. Zonal trends were highest near the equator; however, zonal TTDs were nearly independent of latitude when 5% measurement error was included. Zonal TTDs are significantly reduced when the trends are analyzed by season. Regional trends (15° ? 30°) show TTDs close to those in the 15° latitude zones (15° ? 360°). Detailed case study analysis of four selected regions with high population density?eastern United States, Europe, China, and India?indicated that trend analysis on regional spatial scales may provide the most timely information regarding highly populated regions when comparing detection time scales to global and zonal analyses.
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      Time-to-Detect Trends in Precipitable Water Vapor with Varying Measurement Error

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4223244
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    contributor authorRoman, Jacola
    contributor authorKnuteson, Robert
    contributor authorAckerman, Steve
    date accessioned2017-06-09T17:09:43Z
    date available2017-06-09T17:09:43Z
    date copyright2014/11/01
    date issued2014
    identifier issn0894-8755
    identifier otherams-80361.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4223244
    description abstracthis study determined the theoretical time-to-detect (TTD) global climate model (GCM) precipitable water vapor (PWV) 100-yr trends when realistic measurement errors are considered. Global trends ranged from 0.055 to 0.072 mm yr?1 and varied minimally from season to season. Global TTDs with a 0% measurement error ranged from 3.0 to 4.8 yr, while a 5% measurement error increased the TTD by almost 6 times, ranging from 17.6 to 22.0 yr. Zonal trends were highest near the equator; however, zonal TTDs were nearly independent of latitude when 5% measurement error was included. Zonal TTDs are significantly reduced when the trends are analyzed by season. Regional trends (15° ? 30°) show TTDs close to those in the 15° latitude zones (15° ? 360°). Detailed case study analysis of four selected regions with high population density?eastern United States, Europe, China, and India?indicated that trend analysis on regional spatial scales may provide the most timely information regarding highly populated regions when comparing detection time scales to global and zonal analyses.
    publisherAmerican Meteorological Society
    titleTime-to-Detect Trends in Precipitable Water Vapor with Varying Measurement Error
    typeJournal Paper
    journal volume27
    journal issue21
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-13-00736.1
    journal fristpage8259
    journal lastpage8275
    treeJournal of Climate:;2014:;volume( 027 ):;issue: 021
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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