YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Journal of Climate
    • View Item
    •   YE&T Library
    • AMS
    • Journal of Climate
    • View Item
    • All Fields
    • Source Title
    • Year
    • Publisher
    • Title
    • Subject
    • Author
    • DOI
    • ISBN
    Advanced Search
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Archive

    The Role of Ice–Ocean Interactions in the Variability of the North Atlantic Thermohaline Circulation

    Source: Journal of Climate:;2001:;volume( 014 ):;issue: 005::page 656
    Author:
    Holland, Marika M.
    ,
    Bitz, Cecilia M.
    ,
    Eby, Michael
    ,
    Weaver, Andrew J.
    DOI: 10.1175/1520-0442(2001)014<0656:TROIOI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The simulated influence of Arctic sea ice on the variability of the North Atlantic climate is discussed in the context of a global coupled ice?ocean?atmosphere model. This coupled system incorporates a general circulation ocean model, an atmospheric energy moisture balance model, and a dynamic?thermodynamic sea ice model. Under steady seasonal forcing, an equilibrium solution is obtained with very little variability. To induce variability in the model, daily varying stochastic anomalies are applied to the wind forcing of the Northern Hemisphere sea ice cover. These stochastic anomalies have observed spatial patterns but are random in time. Model simulations are run for 1000 yr from an equilibrium state and the variability in the system is analyzed. The sensitivity of the system to the ice?ocean coupling of both heat and freshwater is also examined. Under the stochastic forcing conditions, the thermohaline circulation (THC) responds with variability that is approximately 10% of the mean. This variability has enhanced spectral power at interdecadal timescales that is concentrated at approximately 20 yr. It is forced by fluctuations in the export of ice from the Arctic into the North Atlantic. Substantial changes in sea surface temperature and salinity are related to changes in the overturning circulation and the sea ice coverage in the northern North Atlantic. Additionally, the THC variability influences the Arctic Basin through heat transport under the ice pack. Results from sensitivity studies suggest that the freshwater exchange from the variable ice cover is the dominant process for forcing variability in the overturning. The simulated Arctic ice export appears to provide stochastic forcing to the northern North Atlantic that excites a damped oscillatory ocean-only mode. The insulating capacity of the variable sea ice has a negligible effect on the THC. Ice?ocean thermal coupling acts to damp THC variability, causing an approximately 25% reduction in the THC standard deviation.
    • Download: (612.7Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      The Role of Ice–Ocean Interactions in the Variability of the North Atlantic Thermohaline Circulation

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4197122
    Collections
    • Journal of Climate

    Show full item record

    contributor authorHolland, Marika M.
    contributor authorBitz, Cecilia M.
    contributor authorEby, Michael
    contributor authorWeaver, Andrew J.
    date accessioned2017-06-09T15:55:41Z
    date available2017-06-09T15:55:41Z
    date copyright2001/03/01
    date issued2001
    identifier issn0894-8755
    identifier otherams-5685.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4197122
    description abstractThe simulated influence of Arctic sea ice on the variability of the North Atlantic climate is discussed in the context of a global coupled ice?ocean?atmosphere model. This coupled system incorporates a general circulation ocean model, an atmospheric energy moisture balance model, and a dynamic?thermodynamic sea ice model. Under steady seasonal forcing, an equilibrium solution is obtained with very little variability. To induce variability in the model, daily varying stochastic anomalies are applied to the wind forcing of the Northern Hemisphere sea ice cover. These stochastic anomalies have observed spatial patterns but are random in time. Model simulations are run for 1000 yr from an equilibrium state and the variability in the system is analyzed. The sensitivity of the system to the ice?ocean coupling of both heat and freshwater is also examined. Under the stochastic forcing conditions, the thermohaline circulation (THC) responds with variability that is approximately 10% of the mean. This variability has enhanced spectral power at interdecadal timescales that is concentrated at approximately 20 yr. It is forced by fluctuations in the export of ice from the Arctic into the North Atlantic. Substantial changes in sea surface temperature and salinity are related to changes in the overturning circulation and the sea ice coverage in the northern North Atlantic. Additionally, the THC variability influences the Arctic Basin through heat transport under the ice pack. Results from sensitivity studies suggest that the freshwater exchange from the variable ice cover is the dominant process for forcing variability in the overturning. The simulated Arctic ice export appears to provide stochastic forcing to the northern North Atlantic that excites a damped oscillatory ocean-only mode. The insulating capacity of the variable sea ice has a negligible effect on the THC. Ice?ocean thermal coupling acts to damp THC variability, causing an approximately 25% reduction in the THC standard deviation.
    publisherAmerican Meteorological Society
    titleThe Role of Ice–Ocean Interactions in the Variability of the North Atlantic Thermohaline Circulation
    typeJournal Paper
    journal volume14
    journal issue5
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(2001)014<0656:TROIOI>2.0.CO;2
    journal fristpage656
    journal lastpage675
    treeJournal of Climate:;2001:;volume( 014 ):;issue: 005
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian