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    Mean and Variability of the Tropical Atlantic Ocean in the CCSM4

    Source: Journal of Climate:;2012:;volume( 025 ):;issue: 014::page 4860
    Author:
    Muñoz, Ernesto
    ,
    Weijer, Wilbert
    ,
    Grodsky, Semyon A.
    ,
    Bates, Susan C.
    ,
    Wainer, Ilana
    DOI: 10.1175/JCLI-D-11-00294.1
    Publisher: American Meteorological Society
    Abstract: his study analyzes important aspects of the tropical Atlantic Ocean from simulations of the fourth version of the Community Climate System Model (CCSM4): the mean sea surface temperature (SST) and wind stress, the Atlantic warm pools, the principal modes of SST variability, and the heat budget in the Benguela region. The main goal was to assess the similarities and differences between the CCSM4 simulations and observations. The results indicate that the tropical Atlantic overall is realistic in CCSM4. However, there are still significant biases in the CCSM4 Atlantic SSTs, with a colder tropical North Atlantic and a hotter tropical South Atlantic, that are related to biases in the wind stress. These are also reflected in the Atlantic warm pools in April and September, with its volume greater than in observations in April and smaller than in observations in September. The variability of SSTs in the tropical Atlantic is well represented in CCSM4. However, in the equatorial and tropical South Atlantic regions, CCSM4 has two distinct modes of variability, in contrast to observed behavior. A model heat budget analysis of the Benguela region indicates that the variability of the upper-ocean temperature is dominated by vertical advection, followed by meridional advection.
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      Mean and Variability of the Tropical Atlantic Ocean in the CCSM4

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4221748
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    contributor authorMuñoz, Ernesto
    contributor authorWeijer, Wilbert
    contributor authorGrodsky, Semyon A.
    contributor authorBates, Susan C.
    contributor authorWainer, Ilana
    date accessioned2017-06-09T17:04:34Z
    date available2017-06-09T17:04:34Z
    date copyright2012/07/01
    date issued2012
    identifier issn0894-8755
    identifier otherams-79014.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4221748
    description abstracthis study analyzes important aspects of the tropical Atlantic Ocean from simulations of the fourth version of the Community Climate System Model (CCSM4): the mean sea surface temperature (SST) and wind stress, the Atlantic warm pools, the principal modes of SST variability, and the heat budget in the Benguela region. The main goal was to assess the similarities and differences between the CCSM4 simulations and observations. The results indicate that the tropical Atlantic overall is realistic in CCSM4. However, there are still significant biases in the CCSM4 Atlantic SSTs, with a colder tropical North Atlantic and a hotter tropical South Atlantic, that are related to biases in the wind stress. These are also reflected in the Atlantic warm pools in April and September, with its volume greater than in observations in April and smaller than in observations in September. The variability of SSTs in the tropical Atlantic is well represented in CCSM4. However, in the equatorial and tropical South Atlantic regions, CCSM4 has two distinct modes of variability, in contrast to observed behavior. A model heat budget analysis of the Benguela region indicates that the variability of the upper-ocean temperature is dominated by vertical advection, followed by meridional advection.
    publisherAmerican Meteorological Society
    titleMean and Variability of the Tropical Atlantic Ocean in the CCSM4
    typeJournal Paper
    journal volume25
    journal issue14
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-11-00294.1
    journal fristpage4860
    journal lastpage4882
    treeJournal of Climate:;2012:;volume( 025 ):;issue: 014
    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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