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    Persistence of Wintertime 500 mb Height Anomalies over the Central Pacific

    Source: Monthly Weather Review:;1985:;volume( 113 ):;issue: 011::page 2043
    Author:
    Horel, John D.
    DOI: 10.1175/1520-0493(1985)113<2043:POWMHA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The persistence of daily 500 mb geopotential height anomalies during the 17 winters from 1966 to 1982 is documented for a region over the central Pacific that is noted for its frequent blocking activity. Persistence is expressed here in terms of the degree to which a height value remains constant during the next several days. For a 9 grid-point region centered on 50°N, 165°W, blocks (large positive geopotential height anomalies) tend to be less persistent than negative height anomalies between ?100 and ?200 m. The greater persistence of negative height anomalies in this region is related to periods of stronger than normal zonal flow centered near 40°N (high zonal index). These periods of stronger than normal zonal flow are more persistent than expected of a first-order autoregressive process.
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      Persistence of Wintertime 500 mb Height Anomalies over the Central Pacific

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4201435
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    contributor authorHorel, John D.
    date accessioned2017-06-09T16:05:34Z
    date available2017-06-09T16:05:34Z
    date copyright1985/11/01
    date issued1985
    identifier issn0027-0644
    identifier otherams-60732.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4201435
    description abstractThe persistence of daily 500 mb geopotential height anomalies during the 17 winters from 1966 to 1982 is documented for a region over the central Pacific that is noted for its frequent blocking activity. Persistence is expressed here in terms of the degree to which a height value remains constant during the next several days. For a 9 grid-point region centered on 50°N, 165°W, blocks (large positive geopotential height anomalies) tend to be less persistent than negative height anomalies between ?100 and ?200 m. The greater persistence of negative height anomalies in this region is related to periods of stronger than normal zonal flow centered near 40°N (high zonal index). These periods of stronger than normal zonal flow are more persistent than expected of a first-order autoregressive process.
    publisherAmerican Meteorological Society
    titlePersistence of Wintertime 500 mb Height Anomalies over the Central Pacific
    typeJournal Paper
    journal volume113
    journal issue11
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1985)113<2043:POWMHA>2.0.CO;2
    journal fristpage2043
    journal lastpage2048
    treeMonthly Weather Review:;1985:;volume( 113 ):;issue: 011
    contenttypeFulltext
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