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    Improved Prediction of the Indian Ocean Dipole Mode by Use of Subsurface Ocean Observations

    Source: Journal of Climate:;2017:;volume( 030 ):;issue: 019::page 7953
    Author:
    Doi, Takeshi;Storto, Andrea;Behera, Swadhin K.;Navarra, Antonio;Yamagata, Toshio
    DOI: 10.1175/JCLI-D-16-0915.1
    Publisher: American Meteorological Society
    Abstract: AbstractThe numerical seasonal prediction system using the Scale Interaction Experiment?Frontier version 1 (SINTEX-F) ocean?atmosphere coupled model has so far demonstrated a good performance for prediction of the Indian Ocean dipole mode (IOD) despite the fact that the system adopts a relatively simple initialization scheme based on nudging only the sea surface temperature (SST). However, it is to be expected that the system is not sufficient to capture in detail the subsurface oceanic precondition. Therefore, the authors have introduced a new three-dimensional variational ocean data assimilation (3DVAR) method that takes three-dimensional observed ocean temperature and salinity into account. Since the new system has successfully improved IOD predictions, the present study is showing that the ocean observational efforts in the tropical Indian Ocean are decisive for improvement of the IOD predictions and may have a large impact on important socioeconomic activities, particularly in the Indian Ocean rim countries.
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      Improved Prediction of the Indian Ocean Dipole Mode by Use of Subsurface Ocean Observations

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4246195
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    contributor authorDoi, Takeshi;Storto, Andrea;Behera, Swadhin K.;Navarra, Antonio;Yamagata, Toshio
    date accessioned2018-01-03T11:01:30Z
    date available2018-01-03T11:01:30Z
    date copyright7/26/2017 12:00:00 AM
    date issued2017
    identifier otherjcli-d-16-0915.1.pdf
    identifier urihttp://138.201.223.254:8080/yetl1/handle/yetl/4246195
    description abstractAbstractThe numerical seasonal prediction system using the Scale Interaction Experiment?Frontier version 1 (SINTEX-F) ocean?atmosphere coupled model has so far demonstrated a good performance for prediction of the Indian Ocean dipole mode (IOD) despite the fact that the system adopts a relatively simple initialization scheme based on nudging only the sea surface temperature (SST). However, it is to be expected that the system is not sufficient to capture in detail the subsurface oceanic precondition. Therefore, the authors have introduced a new three-dimensional variational ocean data assimilation (3DVAR) method that takes three-dimensional observed ocean temperature and salinity into account. Since the new system has successfully improved IOD predictions, the present study is showing that the ocean observational efforts in the tropical Indian Ocean are decisive for improvement of the IOD predictions and may have a large impact on important socioeconomic activities, particularly in the Indian Ocean rim countries.
    publisherAmerican Meteorological Society
    titleImproved Prediction of the Indian Ocean Dipole Mode by Use of Subsurface Ocean Observations
    typeJournal Paper
    journal volume30
    journal issue19
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-16-0915.1
    journal fristpage7953
    journal lastpage7970
    treeJournal of Climate:;2017:;volume( 030 ):;issue: 019
    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
    yabeshDSpacePersian