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    Unexplained Discontinuity in the U.S. Radiosonde Temperature Data. Part II: Stratosphere

    Source: Journal of Atmospheric and Oceanic Technology:;2004:;volume( 021 ):;issue: 008::page 1133
    Author:
    Redder, Christopher R.
    ,
    Luers, Jim K.
    ,
    Eskridge, Robert E.
    DOI: 10.1175/1520-0426(2004)021<1133:UDITUR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The second part of this two-part article discusses the differences between observations taken at 0000 and 1200 UTC, particularly in the stratosphere, by the Vaisala RS80-57H radiosondes that are integrated within the National Weather Service's (NWS's) Micro-ART system. There are large maxima in the horizontal distributions of the monthly time means of the 0000/1200 UTC temperature and height differences over the central United States that are absent over Canada. These maxima are as large as 5 K and 150 m at 10 hPa. Data analysis shows that the 0000/1200 UTC differences are largely artificial, especially over the central United States. They originate in the postprocessing software at observing stations, thus confirming the findings in Part I. Special flight data from the NWS test facility at Sterling, Virginia, have been used to deduce the bias correction applied by Vaisala's postprocessing system. By analyzing the correction data, it has been shown that the inconsistencies with non-U.S. Vaisala RS80 data, as well as most of the large 0000/1200 UTC differences over the United States, can be accounted for by multiplying the reported time since radiosonde launch by a factor of 5/3, which is incorrectly applied by the Vaisala postprocessing software. After being presented with the findings in this paper, Vaisala further isolated the source of the inconsistencies to a software coding error in the radiation bias correction scheme. The error affects only the software installed at NWS stations.
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      Unexplained Discontinuity in the U.S. Radiosonde Temperature Data. Part II: Stratosphere

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4159945
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    contributor authorRedder, Christopher R.
    contributor authorLuers, Jim K.
    contributor authorEskridge, Robert E.
    date accessioned2017-06-09T14:38:29Z
    date available2017-06-09T14:38:29Z
    date copyright2004/08/01
    date issued2004
    identifier issn0739-0572
    identifier otherams-2339.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159945
    description abstractThe second part of this two-part article discusses the differences between observations taken at 0000 and 1200 UTC, particularly in the stratosphere, by the Vaisala RS80-57H radiosondes that are integrated within the National Weather Service's (NWS's) Micro-ART system. There are large maxima in the horizontal distributions of the monthly time means of the 0000/1200 UTC temperature and height differences over the central United States that are absent over Canada. These maxima are as large as 5 K and 150 m at 10 hPa. Data analysis shows that the 0000/1200 UTC differences are largely artificial, especially over the central United States. They originate in the postprocessing software at observing stations, thus confirming the findings in Part I. Special flight data from the NWS test facility at Sterling, Virginia, have been used to deduce the bias correction applied by Vaisala's postprocessing system. By analyzing the correction data, it has been shown that the inconsistencies with non-U.S. Vaisala RS80 data, as well as most of the large 0000/1200 UTC differences over the United States, can be accounted for by multiplying the reported time since radiosonde launch by a factor of 5/3, which is incorrectly applied by the Vaisala postprocessing software. After being presented with the findings in this paper, Vaisala further isolated the source of the inconsistencies to a software coding error in the radiation bias correction scheme. The error affects only the software installed at NWS stations.
    publisherAmerican Meteorological Society
    titleUnexplained Discontinuity in the U.S. Radiosonde Temperature Data. Part II: Stratosphere
    typeJournal Paper
    journal volume21
    journal issue8
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(2004)021<1133:UDITUR>2.0.CO;2
    journal fristpage1133
    journal lastpage1144
    treeJournal of Atmospheric and Oceanic Technology:;2004:;volume( 021 ):;issue: 008
    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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