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    INVERSIONS OVER THE TROPICAL EASTERN PACIFIC OCEAN

    Source: Monthly Weather Review:;1968:;volume( 096 ):;issue: 003::page 177
    Author:
    HARAGUCHI, PAUL Y.
    DOI: 10.1175/1520-0493(1968)096<0177:IOTTEP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Two definite levels of subsidence inversions were found over the tropical Eastern Pacific Ocean during the winter of 1964; both were mainly persistent and continuous. The existence of the lower inversion has been known, but that of the upper inversion at a mean height of 550 mb. has not. It is hypothesized that the upper inversion is caused and maintained by the subsidence in the warm ?dynamic? anticyclone centered over Central America during winter. Both inversions appear to act as ?lids? on cloud height development.
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      INVERSIONS OVER THE TROPICAL EASTERN PACIFIC OCEAN

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4198338
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    contributor authorHARAGUCHI, PAUL Y.
    date accessioned2017-06-09T15:58:39Z
    date available2017-06-09T15:58:39Z
    date copyright1968/03/01
    date issued1968
    identifier issn0027-0644
    identifier otherams-57946.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198338
    description abstractTwo definite levels of subsidence inversions were found over the tropical Eastern Pacific Ocean during the winter of 1964; both were mainly persistent and continuous. The existence of the lower inversion has been known, but that of the upper inversion at a mean height of 550 mb. has not. It is hypothesized that the upper inversion is caused and maintained by the subsidence in the warm ?dynamic? anticyclone centered over Central America during winter. Both inversions appear to act as ?lids? on cloud height development.
    publisherAmerican Meteorological Society
    titleINVERSIONS OVER THE TROPICAL EASTERN PACIFIC OCEAN
    typeJournal Paper
    journal volume96
    journal issue3
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1968)096<0177:IOTTEP>2.0.CO;2
    journal fristpage177
    journal lastpage185
    treeMonthly Weather Review:;1968:;volume( 096 ):;issue: 003
    contenttypeFulltext
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