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    On Recent Trends in Atmospheric and Limnological Variables in Lake Ontario

    Source: Journal of Climate:;2012:;volume( 025 ):;issue: 017::page 5807
    Author:
    Huang, Anning
    ,
    Rao, Yerubandi R.
    ,
    Zhang, Weitao
    DOI: 10.1175/JCLI-D-11-00495.1
    Publisher: American Meteorological Society
    Abstract: he surface air and water temperatures increased at all seasonal and annual time scales during the last 40 yr in Lake Ontario. The annual mean air and surface water temperatures have increased by 1.43° ±0.39° and 1.26° ±0.32°C, respectively, over 1970?2009. The air temperature increased at a faster rate than the surface water temperature in winter and autumn, whereas in spring and summer the surface water temperature warmed faster than the air temperature. The length of summer stratified season has increased by 12 ± 2 days since the early 1970s due to the increase in water temperature. The decline of surface wind speed over Lake Ontario resulted in a shallower surface mixed layer and enhanced the summer thermal stratification, which increased the summer surface water temperature more rapidly than the air temperature.
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      On Recent Trends in Atmospheric and Limnological Variables in Lake Ontario

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4221910
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    contributor authorHuang, Anning
    contributor authorRao, Yerubandi R.
    contributor authorZhang, Weitao
    date accessioned2017-06-09T17:05:10Z
    date available2017-06-09T17:05:10Z
    date copyright2012/09/01
    date issued2012
    identifier issn0894-8755
    identifier otherams-79161.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4221910
    description abstracthe surface air and water temperatures increased at all seasonal and annual time scales during the last 40 yr in Lake Ontario. The annual mean air and surface water temperatures have increased by 1.43° ±0.39° and 1.26° ±0.32°C, respectively, over 1970?2009. The air temperature increased at a faster rate than the surface water temperature in winter and autumn, whereas in spring and summer the surface water temperature warmed faster than the air temperature. The length of summer stratified season has increased by 12 ± 2 days since the early 1970s due to the increase in water temperature. The decline of surface wind speed over Lake Ontario resulted in a shallower surface mixed layer and enhanced the summer thermal stratification, which increased the summer surface water temperature more rapidly than the air temperature.
    publisherAmerican Meteorological Society
    titleOn Recent Trends in Atmospheric and Limnological Variables in Lake Ontario
    typeJournal Paper
    journal volume25
    journal issue17
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-11-00495.1
    journal fristpage5807
    journal lastpage5816
    treeJournal of Climate:;2012:;volume( 025 ):;issue: 017
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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