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    The Influence of Multiple Lake Interactions upon Lake-Effect Storms

    Source: Monthly Weather Review:;2002:;volume( 130 ):;issue: 006::page 1510
    Author:
    Mann, Greg E.
    ,
    Wagenmaker, Richard B.
    ,
    Sousounis, Peter J.
    DOI: 10.1175/1520-0493(2002)130<1510:TIOMLI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Mesoscale disturbances in close proximity to one another typically undergo process interactions, which ultimately may result in the formation of a disturbance on the scale of the combined mesoscale disturbances. Embedded within this combined disturbance, some semblance of the incipient individual mesoscale disturbances may be preserved, especially in instances when the individual forcing mechanisms are fixed in space, as in the case of the Great Lakes. Studies have shown that during prolonged cold air outbreaks, collective lake disturbances can originate from the organization of individual lake-scale disturbances. These collective lake disturbances may, through scale interactions, alter the behavior of the contributing individual lake-scale disturbances and the embedded lake-effect storms. Factor separation decomposition of the Great Lakes system indicates that various interactions among lake-scale processes contribute to the overall development of the regional-scale disturbance, which can modulate embedded lake-effect snowbands. Contributions from these interactions tend to offset the individual lake contributions, especially during the development of the collective lake disturbance, but vary spatially and temporally. As the regional-scale disturbance matures, lake?lake interactions then accentuate the individual lake contributions. Specifically, the modulation of lake-effect snowbands was translational, intensional, and in some instances morphological in nature. Near Lake Michigan, processes attributed to Lake Superior (upstream lake) were direct and synergistic (indirect) resulting in a time delay of maximum snowfall intensity, while processes attributed to the downstream lakes were primarily synergistic resulting in an overall decrease in snowfall intensity. Furthermore, as the collective lake disturbance matured, Lake Superior?induced processes contributed to a significant morphological change in the Lake Michigan lake-effect snowbands.
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      The Influence of Multiple Lake Interactions upon Lake-Effect Storms

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4205018
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    contributor authorMann, Greg E.
    contributor authorWagenmaker, Richard B.
    contributor authorSousounis, Peter J.
    date accessioned2017-06-09T16:14:27Z
    date available2017-06-09T16:14:27Z
    date copyright2002/06/01
    date issued2002
    identifier issn0027-0644
    identifier otherams-63958.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4205018
    description abstractMesoscale disturbances in close proximity to one another typically undergo process interactions, which ultimately may result in the formation of a disturbance on the scale of the combined mesoscale disturbances. Embedded within this combined disturbance, some semblance of the incipient individual mesoscale disturbances may be preserved, especially in instances when the individual forcing mechanisms are fixed in space, as in the case of the Great Lakes. Studies have shown that during prolonged cold air outbreaks, collective lake disturbances can originate from the organization of individual lake-scale disturbances. These collective lake disturbances may, through scale interactions, alter the behavior of the contributing individual lake-scale disturbances and the embedded lake-effect storms. Factor separation decomposition of the Great Lakes system indicates that various interactions among lake-scale processes contribute to the overall development of the regional-scale disturbance, which can modulate embedded lake-effect snowbands. Contributions from these interactions tend to offset the individual lake contributions, especially during the development of the collective lake disturbance, but vary spatially and temporally. As the regional-scale disturbance matures, lake?lake interactions then accentuate the individual lake contributions. Specifically, the modulation of lake-effect snowbands was translational, intensional, and in some instances morphological in nature. Near Lake Michigan, processes attributed to Lake Superior (upstream lake) were direct and synergistic (indirect) resulting in a time delay of maximum snowfall intensity, while processes attributed to the downstream lakes were primarily synergistic resulting in an overall decrease in snowfall intensity. Furthermore, as the collective lake disturbance matured, Lake Superior?induced processes contributed to a significant morphological change in the Lake Michigan lake-effect snowbands.
    publisherAmerican Meteorological Society
    titleThe Influence of Multiple Lake Interactions upon Lake-Effect Storms
    typeJournal Paper
    journal volume130
    journal issue6
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(2002)130<1510:TIOMLI>2.0.CO;2
    journal fristpage1510
    journal lastpage1530
    treeMonthly Weather Review:;2002:;volume( 130 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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