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    The Øresund Experiment—A Nordic Mesoscale Dispersion Experiment Over a Land-Water-Land Area

    Source: Bulletin of the American Meteorological Society:;1985:;volume( 066 ):;issue: 011::page 1403
    Author:
    Gryning, Sven-Erik
    DOI: 10.1175/1520-0477(1985)066<1403:TENMDE>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The atmospheric dispersion process and the modification in the wind field across than 20-km-wide ?resund strait between Denmark and Sweden were studied in this project. The meteorological observational network extended over an 80-km-wide cross section through the ?resund. The dispersion process was investigated by carrying out SF6 tracer experiments, and the air trajectories were determined by tetroon flights. Emphasis was placed on the periods when the water surface was colder than the surrounding land, which in the experimental period typically occurred during daytime. Although the measuring program was intensified during the day, when tracer releases were carried out, a fairly large proportion of the meteorological measurements were carried out on a regular day-and-night basis throughout the whole experiments period. This yielded data for a large variety of meteorological situations. All data from the experiment will be made available for general use.
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      The Øresund Experiment—A Nordic Mesoscale Dispersion Experiment Over a Land-Water-Land Area

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4160782
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    contributor authorGryning, Sven-Erik
    date accessioned2017-06-09T14:40:21Z
    date available2017-06-09T14:40:21Z
    date copyright1985/11/01
    date issued1985
    identifier issn0003-0007
    identifier otherams-24142.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4160782
    description abstractThe atmospheric dispersion process and the modification in the wind field across than 20-km-wide ?resund strait between Denmark and Sweden were studied in this project. The meteorological observational network extended over an 80-km-wide cross section through the ?resund. The dispersion process was investigated by carrying out SF6 tracer experiments, and the air trajectories were determined by tetroon flights. Emphasis was placed on the periods when the water surface was colder than the surrounding land, which in the experimental period typically occurred during daytime. Although the measuring program was intensified during the day, when tracer releases were carried out, a fairly large proportion of the meteorological measurements were carried out on a regular day-and-night basis throughout the whole experiments period. This yielded data for a large variety of meteorological situations. All data from the experiment will be made available for general use.
    publisherAmerican Meteorological Society
    titleThe Øresund Experiment—A Nordic Mesoscale Dispersion Experiment Over a Land-Water-Land Area
    typeJournal Paper
    journal volume66
    journal issue11
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1985)066<1403:TENMDE>2.0.CO;2
    journal fristpage1403
    journal lastpage1407
    treeBulletin of the American Meteorological Society:;1985:;volume( 066 ):;issue: 011
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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