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    Flow Mechanism for the Long-Range Transport of Air Pollutants by the Sea Breeze Causing Inland Nighttime High Oxidants

    Source: Journal of Applied Meteorology:;1988:;volume( 027 ):;issue: 002::page 182
    Author:
    Ueda, Hiromasa
    ,
    Mitsumoto, Shigeki
    ,
    Kurita, Hidemi
    DOI: 10.1175/1520-0450(1988)027<0182:FMFTLR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Flow mechanism causing nighttime smog was investigated by analyzing 1) continuous records of meteorological data and concentration of Oxidants (Ox) for 15 days and 2) aircraft data along the transportation route of a polluted air mass. It was found that an air mass which passed over the large emission sources along the coastline was transported inland as a sea breeze in the form of a gravity current. A high concentration layer was created in the upper part of the gravity current. It descended at the rear edge of a gravity-current head due to the internal circulation within the head, thus yielding the highest concentration of Ox near the ground there.
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      Flow Mechanism for the Long-Range Transport of Air Pollutants by the Sea Breeze Causing Inland Nighttime High Oxidants

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4146510
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    contributor authorUeda, Hiromasa
    contributor authorMitsumoto, Shigeki
    contributor authorKurita, Hidemi
    date accessioned2017-06-09T14:02:11Z
    date available2017-06-09T14:02:11Z
    date copyright1988/02/01
    date issued1988
    identifier issn0894-8763
    identifier otherams-11298.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146510
    description abstractFlow mechanism causing nighttime smog was investigated by analyzing 1) continuous records of meteorological data and concentration of Oxidants (Ox) for 15 days and 2) aircraft data along the transportation route of a polluted air mass. It was found that an air mass which passed over the large emission sources along the coastline was transported inland as a sea breeze in the form of a gravity current. A high concentration layer was created in the upper part of the gravity current. It descended at the rear edge of a gravity-current head due to the internal circulation within the head, thus yielding the highest concentration of Ox near the ground there.
    publisherAmerican Meteorological Society
    titleFlow Mechanism for the Long-Range Transport of Air Pollutants by the Sea Breeze Causing Inland Nighttime High Oxidants
    typeJournal Paper
    journal volume27
    journal issue2
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1988)027<0182:FMFTLR>2.0.CO;2
    journal fristpage182
    journal lastpage187
    treeJournal of Applied Meteorology:;1988:;volume( 027 ):;issue: 002
    contenttypeFulltext
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