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    Lake Michigan Lake Breezes: Climatology, Local Forcing, and Synoptic Environment

    Source: Journal of Applied Meteorology:;2001:;volume( 040 ):;issue: 003::page 409
    Author:
    Laird, Neil F.
    ,
    Kristovich, David A. R.
    ,
    Liang, Xin-Zhong
    ,
    Arritt, Raymond W.
    ,
    Labas, Kenneth
    DOI: 10.1175/1520-0450(2001)040<0409:LMLBCL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A method was developed to identify the occurrence of lake-breeze events along the eastern, western, and both shores of Lake Michigan during a 15-yr period (1982?96). Comparison with detailed observations from May through September of 1996?97 showed that the method reasonably identified Lake Michigan lake-breeze events. The method also demonstrated the important ability to distinguish non-lake-breeze events; a problem experienced by previously developed lake-breeze criteria. Analyses of the 15-yr climatological data indicated that lake breezes tended to occur more frequently along the eastern shore of Lake Michigan than along the western shore. On average, a maximum number of lake-breeze events occurred during August at each location. This maximum is most closely associated with weaker monthly average wind speeds. Even though the air?lake temperature difference ?T provides the local forcing for the development of the lake-breeze circulation, large temperature differences are not required. Nearly 70% of all events occurred with a daytime maximum ?T ? 12°C. The evaluation of a lake-breeze index ε used in past studies and many forecasting applications showed indices computed using offshore or shore-perpendicular wind speeds (U or |U|, respectively) at inland sites resolved ≥95% of identified events based on critical ε values of 2?6. When wind speed, irrespective of wind direction, was used to calculate ε, the success of the critical indices decreased by as much as 26%. Results also showed that the lake-breeze index has a considerable tendency to overestimate the number of events. Although the possibility was suggested by previous investigations, the critical value of ε may not be appreciably affected by changes in location along the shoreline. In addition, noteworthy differences in the position of synoptic-scale sea level pressure and wind fields with respect to Lake Michigan were found to occur during eastern, western, and both-shore lake-breeze events.
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      Lake Michigan Lake Breezes: Climatology, Local Forcing, and Synoptic Environment

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4148357
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    • Journal of Applied Meteorology

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    contributor authorLaird, Neil F.
    contributor authorKristovich, David A. R.
    contributor authorLiang, Xin-Zhong
    contributor authorArritt, Raymond W.
    contributor authorLabas, Kenneth
    date accessioned2017-06-09T14:07:45Z
    date available2017-06-09T14:07:45Z
    date copyright2001/03/01
    date issued2001
    identifier issn0894-8763
    identifier otherams-12960.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148357
    description abstractA method was developed to identify the occurrence of lake-breeze events along the eastern, western, and both shores of Lake Michigan during a 15-yr period (1982?96). Comparison with detailed observations from May through September of 1996?97 showed that the method reasonably identified Lake Michigan lake-breeze events. The method also demonstrated the important ability to distinguish non-lake-breeze events; a problem experienced by previously developed lake-breeze criteria. Analyses of the 15-yr climatological data indicated that lake breezes tended to occur more frequently along the eastern shore of Lake Michigan than along the western shore. On average, a maximum number of lake-breeze events occurred during August at each location. This maximum is most closely associated with weaker monthly average wind speeds. Even though the air?lake temperature difference ?T provides the local forcing for the development of the lake-breeze circulation, large temperature differences are not required. Nearly 70% of all events occurred with a daytime maximum ?T ? 12°C. The evaluation of a lake-breeze index ε used in past studies and many forecasting applications showed indices computed using offshore or shore-perpendicular wind speeds (U or |U|, respectively) at inland sites resolved ≥95% of identified events based on critical ε values of 2?6. When wind speed, irrespective of wind direction, was used to calculate ε, the success of the critical indices decreased by as much as 26%. Results also showed that the lake-breeze index has a considerable tendency to overestimate the number of events. Although the possibility was suggested by previous investigations, the critical value of ε may not be appreciably affected by changes in location along the shoreline. In addition, noteworthy differences in the position of synoptic-scale sea level pressure and wind fields with respect to Lake Michigan were found to occur during eastern, western, and both-shore lake-breeze events.
    publisherAmerican Meteorological Society
    titleLake Michigan Lake Breezes: Climatology, Local Forcing, and Synoptic Environment
    typeJournal Paper
    journal volume40
    journal issue3
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(2001)040<0409:LMLBCL>2.0.CO;2
    journal fristpage409
    journal lastpage424
    treeJournal of Applied Meteorology:;2001:;volume( 040 ):;issue: 003
    contenttypeFulltext
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