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    A Theoretical Study of the St. Louis Heat Island: The Wind and Temperature Distribution

    Source: Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 005::page 417
    Author:
    Vukovich, Fred M.
    ,
    Dunn, J. W.
    ,
    Crissman, Bobby W.
    DOI: 10.1175/1520-0450(1976)015<0417:ATSOTS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A three-dimensional primitive equation model was used to study the St. Louis heat island. In this paper, the influence of synoptic wind speed and wind direction on the heat island is presented. With respect to the synoptic wind speed, it was found that the temperature and wind distribution associated with the St. Louis heat island changed markedly as the wind speed increased. When the synoptic wind speed was small, the intensity of the heat island was independent of the wind direction. However, for large synoptic wind speeds, the intensity of the heat island changed, and the change was dependent on the wind direction. These changes were due to the influence of the local topography.
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      A Theoretical Study of the St. Louis Heat Island: The Wind and Temperature Distribution

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4232514
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    • Journal of Applied Meteorology

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    contributor authorVukovich, Fred M.
    contributor authorDunn, J. W.
    contributor authorCrissman, Bobby W.
    date accessioned2017-06-09T17:38:34Z
    date available2017-06-09T17:38:34Z
    date copyright1976/05/01
    date issued1976
    identifier issn0021-8952
    identifier otherams-9067.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232514
    description abstractA three-dimensional primitive equation model was used to study the St. Louis heat island. In this paper, the influence of synoptic wind speed and wind direction on the heat island is presented. With respect to the synoptic wind speed, it was found that the temperature and wind distribution associated with the St. Louis heat island changed markedly as the wind speed increased. When the synoptic wind speed was small, the intensity of the heat island was independent of the wind direction. However, for large synoptic wind speeds, the intensity of the heat island changed, and the change was dependent on the wind direction. These changes were due to the influence of the local topography.
    publisherAmerican Meteorological Society
    titleA Theoretical Study of the St. Louis Heat Island: The Wind and Temperature Distribution
    typeJournal Paper
    journal volume15
    journal issue5
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1976)015<0417:ATSOTS>2.0.CO;2
    journal fristpage417
    journal lastpage440
    treeJournal of Applied Meteorology:;1976:;volume( 015 ):;issue: 005
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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