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    A NEW METHOD FOR THE DETERMINATION OF THE VERTICAL DISTRIBUTION OF OZONE FROM A GROUND STATION

    Source: Journal of Meteorology:;1956:;volume( 013 ):;issue: 004::page 319
    Author:
    Epstein, Edward S.
    ,
    Osterberg, Charles
    ,
    Adel, Arthur
    DOI: 10.1175/1520-0469(1956)013<0319:ANMFTD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A new method for determining the vertical distribution of ozone, utilizing only surface observations, has been developed. Infrared and ultraviolet observations are used to complement one another. The theoretical background of the method is discussed in detail, and the techniques of its application are described. Also presented are the results of applying the method to data collected in the seven months beginning February 1955 (124 days' observations). There are definite seasonal trends in the distributions, which are not related in any simple way to the total amount of ozone. The ozone is lowest at times of passages of troughs aloft. Ozone densities at low levels are greatest when surface pressure is lowest.
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      A NEW METHOD FOR THE DETERMINATION OF THE VERTICAL DISTRIBUTION OF OZONE FROM A GROUND STATION

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4149818
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    • Journal of Meteorology

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    contributor authorEpstein, Edward S.
    contributor authorOsterberg, Charles
    contributor authorAdel, Arthur
    date accessioned2017-06-09T14:11:29Z
    date available2017-06-09T14:11:29Z
    date copyright1956/08/01
    date issued1956
    identifier issn0095-9634
    identifier otherams-14275.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149818
    description abstractA new method for determining the vertical distribution of ozone, utilizing only surface observations, has been developed. Infrared and ultraviolet observations are used to complement one another. The theoretical background of the method is discussed in detail, and the techniques of its application are described. Also presented are the results of applying the method to data collected in the seven months beginning February 1955 (124 days' observations). There are definite seasonal trends in the distributions, which are not related in any simple way to the total amount of ozone. The ozone is lowest at times of passages of troughs aloft. Ozone densities at low levels are greatest when surface pressure is lowest.
    publisherAmerican Meteorological Society
    titleA NEW METHOD FOR THE DETERMINATION OF THE VERTICAL DISTRIBUTION OF OZONE FROM A GROUND STATION
    typeJournal Paper
    journal volume13
    journal issue4
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1956)013<0319:ANMFTD>2.0.CO;2
    journal fristpage319
    journal lastpage334
    treeJournal of Meteorology:;1956:;volume( 013 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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