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    Recent Trends in Land Surface Temperature on the Tibetan Plateau

    Source: Journal of Climate:;2006:;volume( 019 ):;issue: 012::page 2995
    Author:
    Oku, Yuichiro
    ,
    Ishikawa, Hirohiko
    ,
    Haginoya, Shigenori
    ,
    Ma, Yaoming
    DOI: 10.1175/JCLI3811.1
    Publisher: American Meteorological Society
    Abstract: The diurnal, seasonal, and interannual variations in land surface temperature (LST) on the Tibetan Plateau from 1996 to 2002 are analyzed using the hourly LST dataset obtained by Japanese Geostationary Meteorological Satellite 5 (GMS-5) observations. Comparing LST retrieved from GMS-5 with independent precipitation amount data demonstrates the consistent and complementary relationship between them. The results indicate an increase in the LST over this period. The daily minimum has risen faster than the daily maximum, resulting in a narrowing of the diurnal range of LST. This is in agreement with the observed trends in both global and plateau near-surface air temperature. Since the near-surface air temperature is mainly controlled by LST, this result ensures a warming trend in near-surface air temperature.
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      Recent Trends in Land Surface Temperature on the Tibetan Plateau

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4220929
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    contributor authorOku, Yuichiro
    contributor authorIshikawa, Hirohiko
    contributor authorHaginoya, Shigenori
    contributor authorMa, Yaoming
    date accessioned2017-06-09T17:02:05Z
    date available2017-06-09T17:02:05Z
    date copyright2006/06/01
    date issued2006
    identifier issn0894-8755
    identifier otherams-78278.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4220929
    description abstractThe diurnal, seasonal, and interannual variations in land surface temperature (LST) on the Tibetan Plateau from 1996 to 2002 are analyzed using the hourly LST dataset obtained by Japanese Geostationary Meteorological Satellite 5 (GMS-5) observations. Comparing LST retrieved from GMS-5 with independent precipitation amount data demonstrates the consistent and complementary relationship between them. The results indicate an increase in the LST over this period. The daily minimum has risen faster than the daily maximum, resulting in a narrowing of the diurnal range of LST. This is in agreement with the observed trends in both global and plateau near-surface air temperature. Since the near-surface air temperature is mainly controlled by LST, this result ensures a warming trend in near-surface air temperature.
    publisherAmerican Meteorological Society
    titleRecent Trends in Land Surface Temperature on the Tibetan Plateau
    typeJournal Paper
    journal volume19
    journal issue12
    journal titleJournal of Climate
    identifier doi10.1175/JCLI3811.1
    journal fristpage2995
    journal lastpage3003
    treeJournal of Climate:;2006:;volume( 019 ):;issue: 012
    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
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