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  • Wiley  (2)
  • English  (2)
  • 2010-2014  (2)
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  • Wiley  (2)
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  • English  (2)
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  • 2010-2014  (2)
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  • 1
    Online Resource
    Online Resource
    Wiley ; 2011
    In:  International Journal of Climatology Vol. 31, No. 10 ( 2011-08), p. 1567-1572
    In: International Journal of Climatology, Wiley, Vol. 31, No. 10 ( 2011-08), p. 1567-1572
    Abstract: Using the climate change experiments generated for the Fourth Assessment of the Intergovernmental Panel on Climate Change, a possible mechanism for the El Niño‐like warming in response to the greenhouse warming is suggested. From the coupled global climate model (CGCM) simulations with climate change scenario, it is found that the Bjerknes air–sea coupled process is a dominant contributor to the tropical Pacific response. However, it is revealed that most CGCMs commonly simulate the off‐equatorial maximum of precipitation change. It is suggested here that the off‐equatorial precipitation and the associated equatorial westerlies play a seeding role in triggering an El Niño‐like warming response. Atmospheric GCM (AGCM) experiments show that even uniform sea‐surface temperature (SST) warming leads to off‐equatorial increase in precipitation which brings equatorial westerlies, implying that these non‐uniform (off‐equatorial) responses can play a seeding role for the El Niño‐like warming pattern. Copyright © 2010 Royal Meteorological Society
    Type of Medium: Online Resource
    ISSN: 0899-8418 , 1097-0088
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2011
    detail.hit.zdb_id: 1491204-1
    SSG: 14
    Location Call Number Limitation Availability
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  • 2
    Online Resource
    Online Resource
    Wiley ; 2010
    In:  Quarterly Journal of the Royal Meteorological Society Vol. 136, No. 653 ( 2010-10), p. 2051-2060
    In: Quarterly Journal of the Royal Meteorological Society, Wiley, Vol. 136, No. 653 ( 2010-10), p. 2051-2060
    Abstract: In this study, a new Ensemble Kalman Filter (EnKF) algorithm called EnKF with growing‐error correction (EnKF‐GEC) is developed for minimizing the growing component of the forecast error; for this purpose, prospective observations are assimilated using empirical singular vectors (ESVs). Unlike the Ensemble Kalman Smoother (EnKS) or four‐dimensional EnKF (4DEnKF), the EnKF‐GEC is designed to reduce the analysis error at the last analysis time (errors of initial condition for prediction). By performing assimilation experiments using the CZ‐SPEEDY coupled model within a perfect model framework, it is shown that the analysis errors obtained using the EnKF‐GEC are significantly reduced as compared to those obtained using the conventional EnKF until the last analysis time as well as during the middle of analysis time. This indicates that the new algorithm is beneficial for prediction. Seasonal prediction results show that the prediction skill when initial conditions are generated by the EnKF‐GEC is superior to when initial conditions are generated by the conventional EnKF or EnKS, particularly during the early forecast lead month. For example, correlation skill improvement with 16 ensemble members is about 0.1 for a 3‐month lead forecast. In addition, it is shown that the new EnKF algorithm is more effective for unpredictable regions, where the value of the unstable singular vector is robust. Copyright © 2010 Royal Meteorological Society
    Type of Medium: Online Resource
    ISSN: 0035-9009 , 1477-870X
    URL: Issue
    RVK:
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2010
    detail.hit.zdb_id: 3142-2
    detail.hit.zdb_id: 2089168-4
    SSG: 14
    Location Call Number Limitation Availability
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