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    The Association of Low-Level Inversions with Surface Wind and Temperature at Point Arguello

    Source: Journal of Applied Meteorology:;1965:;volume( 004 ):;issue: 004::page 509
    Author:
    Baynton, Harold W.
    ,
    Bidwell, Jerold M.
    ,
    Beran, Donald W.
    DOI: 10.1175/1520-0450(1965)004<0509:TAOLLI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Inversions at Point Arguello, California, as detected in 4½ years by rawinsondes at 0400 and 1600 PST, are related to surface wind direction and speed and surface temperatures. Nocturnal inversions based below 1000 ft msl have their maximum frequency in winter and their minimum in summer. Most of them occur with downslope surface winds. Afternoon inversions are most frequent in July and least frequent in January. Nocturnal surface inversions appear to develop when the downslope drainage air from the interior is cool enough to undercut the marine layer. There is evidence that the critical surface temperature for this to take place is 9C.
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      The Association of Low-Level Inversions with Surface Wind and Temperature at Point Arguello

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4214401
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    • Journal of Applied Meteorology

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    contributor authorBaynton, Harold W.
    contributor authorBidwell, Jerold M.
    contributor authorBeran, Donald W.
    date accessioned2017-06-09T16:41:46Z
    date available2017-06-09T16:41:46Z
    date copyright1965/08/01
    date issued1965
    identifier issn0021-8952
    identifier otherams-7240.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4214401
    description abstractInversions at Point Arguello, California, as detected in 4½ years by rawinsondes at 0400 and 1600 PST, are related to surface wind direction and speed and surface temperatures. Nocturnal inversions based below 1000 ft msl have their maximum frequency in winter and their minimum in summer. Most of them occur with downslope surface winds. Afternoon inversions are most frequent in July and least frequent in January. Nocturnal surface inversions appear to develop when the downslope drainage air from the interior is cool enough to undercut the marine layer. There is evidence that the critical surface temperature for this to take place is 9C.
    publisherAmerican Meteorological Society
    titleThe Association of Low-Level Inversions with Surface Wind and Temperature at Point Arguello
    typeJournal Paper
    journal volume4
    journal issue4
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1965)004<0509:TAOLLI>2.0.CO;2
    journal fristpage509
    journal lastpage516
    treeJournal of Applied Meteorology:;1965:;volume( 004 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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