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    Sea Ice in the Canadian Arctic Archipelago: Modeling the Past (1950–2004) and the Future (2041–60)

    Source: Journal of Climate:;2009:;volume( 022 ):;issue: 008::page 2181
    Author:
    Sou, Tessa
    ,
    Flato, Gregory
    DOI: 10.1175/2008JCLI2335.1
    Publisher: American Meteorological Society
    Abstract: Considering the recent losses observed in Arctic sea ice and the anticipated future warming due to anthropogenic greenhouse gas emissions, sea ice retreat in the Canadian Arctic Archipelago (CAA) is expected and indeed is already being observed. As most global climate models do not resolve the CAA region, a fine-resolution ice?ocean regional model is developed and used to make a projection of future changes in the CAA sea ice. Results from a historical run (1950?2004) are used to evaluate the model. The model does well in representing observed sea ice spatial and seasonal variability, but tends to underestimate summertime ice cover. The model results for the future (2041?60) show little change in wintertime ice concentrations from the past, but summertime ice concentrations decrease by 45%. The ice thickness is projected to decrease by 17% in the winter and by 36% in summer. Based on this study, a completely ice-free CAA is unlikely by the year 2050, but the simulated ice retreat suggests that the region could support some commercial shipping.
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      Sea Ice in the Canadian Arctic Archipelago: Modeling the Past (1950–2004) and the Future (2041–60)

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4208562
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    • Journal of Climate

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    contributor authorSou, Tessa
    contributor authorFlato, Gregory
    date accessioned2017-06-09T16:23:55Z
    date available2017-06-09T16:23:55Z
    date copyright2009/04/01
    date issued2009
    identifier issn0894-8755
    identifier otherams-67147.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208562
    description abstractConsidering the recent losses observed in Arctic sea ice and the anticipated future warming due to anthropogenic greenhouse gas emissions, sea ice retreat in the Canadian Arctic Archipelago (CAA) is expected and indeed is already being observed. As most global climate models do not resolve the CAA region, a fine-resolution ice?ocean regional model is developed and used to make a projection of future changes in the CAA sea ice. Results from a historical run (1950?2004) are used to evaluate the model. The model does well in representing observed sea ice spatial and seasonal variability, but tends to underestimate summertime ice cover. The model results for the future (2041?60) show little change in wintertime ice concentrations from the past, but summertime ice concentrations decrease by 45%. The ice thickness is projected to decrease by 17% in the winter and by 36% in summer. Based on this study, a completely ice-free CAA is unlikely by the year 2050, but the simulated ice retreat suggests that the region could support some commercial shipping.
    publisherAmerican Meteorological Society
    titleSea Ice in the Canadian Arctic Archipelago: Modeling the Past (1950–2004) and the Future (2041–60)
    typeJournal Paper
    journal volume22
    journal issue8
    journal titleJournal of Climate
    identifier doi10.1175/2008JCLI2335.1
    journal fristpage2181
    journal lastpage2198
    treeJournal of Climate:;2009:;volume( 022 ):;issue: 008
    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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