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    Characteristics of Ozone Episodes during SCCCAMP 1985

    Source: Journal of Applied Meteorology:;1991:;volume( 030 ):;issue: 005::page 534
    Author:
    Hanna, Steven R.
    DOI: 10.1175/1520-0450(1991)030<0534:COOEDS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Extensive meteorological and air chemistry measurements were obtained along the Ventura and Santa Barbara county coastal areas in California during four 2?3 day case studies conducted during the September?October 1985 South-Central Coast Cooperative Aerometric Monitoring Program (SCCCAMP 1985). An overview of the characteristics of ozone episodes during these four case studies is given, showing that the episodes are associated with warm, high pressure systems with light winds. In the absence of easterly winds, the observed ozone in the region is primarily due to local sources. At other times, easterly wind components transport ozone and its precursors from large source regions to the east (i.e., Los Angeles County). This transport sometimes occurs in inland valleys at elevations up to 600 m, and sometimes occurs over the ocean near the surface. Local sea breezes, mesoscale eddies, and terrain-generated winds often cause complex flow patterns and recirculation of pollutants.
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      Characteristics of Ozone Episodes during SCCCAMP 1985

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4146929
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    contributor authorHanna, Steven R.
    date accessioned2017-06-09T14:03:29Z
    date available2017-06-09T14:03:29Z
    date copyright1991/05/01
    date issued1991
    identifier issn0894-8763
    identifier otherams-11675.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146929
    description abstractExtensive meteorological and air chemistry measurements were obtained along the Ventura and Santa Barbara county coastal areas in California during four 2?3 day case studies conducted during the September?October 1985 South-Central Coast Cooperative Aerometric Monitoring Program (SCCCAMP 1985). An overview of the characteristics of ozone episodes during these four case studies is given, showing that the episodes are associated with warm, high pressure systems with light winds. In the absence of easterly winds, the observed ozone in the region is primarily due to local sources. At other times, easterly wind components transport ozone and its precursors from large source regions to the east (i.e., Los Angeles County). This transport sometimes occurs in inland valleys at elevations up to 600 m, and sometimes occurs over the ocean near the surface. Local sea breezes, mesoscale eddies, and terrain-generated winds often cause complex flow patterns and recirculation of pollutants.
    publisherAmerican Meteorological Society
    titleCharacteristics of Ozone Episodes during SCCCAMP 1985
    typeJournal Paper
    journal volume30
    journal issue5
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1991)030<0534:COOEDS>2.0.CO;2
    journal fristpage534
    journal lastpage550
    treeJournal of Applied Meteorology:;1991:;volume( 030 ):;issue: 005
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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