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ITF in a coupled GCM and its interannual variability related to ENSO and IOD

机译:耦合GCM中的ITF及其与ENSO和IOD相关的年际变化

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摘要

The interannual variability of the mass transport of the Indonesian Throughflow (ITF) is very possible to be connected with the El Ni(n)o-Southern Oscillation (ENSO) in the Pacific Ocean and/or the Indian Ocean Dipole (IOD). The IPSL (Institute Pierre-Simon Laplace) coupled general circulation model (CGCM) was employed to examine the interannual variability of the ITF and understand its relationship with the climatic variation in both the basins. A 1 000 a integration was conducted and an annual mean model output was utilized. The pathways of the simulated ITF are reasonable within the Indonesian seas. The major transport occurs in the upper 300 m,with an annual mean transport of 15.68×106 m3/s, among which the 13.83×106 m3/s through the Makassar Strait is the principal component. The interannual variability of the ITF transport is significant in a 2~4 a period. The relationship between sea level differences across the Indonesian seas (sites in the western Pacific north of the equator and south coast of Java, respectively) and the ITF transport is straightforward on the interannual time-scale with a simultaneous correlation of 0.82. Further investigation indicates that the preceding climatic variation in the tropical Pacific is related to the ITF transport anomaly. The ENSO-like pattern leads the extreme of ITF transport by 1 a, with the correlation between a Ni(n)o 3 SST index and the ITF transport of 0.37. It means that there tends to be an El Ni(n)o anomaly in the Pacific 1 a before a large ITF transport. The simultaneous correlation between the Ni(n)o 3 SST index and the ITF transport is -0.34. The patterns of sea surface temperature and sea surface height are, however, not the typical ENSO anomaly. The ITF transport is more related to the concurrent interannual variability over the Indian Ocean. The simultaneous correlation between the ITF transport and the dipole mode index is 0.46 and the pattern of upper layer anomaly is much like that of the IOD.
机译:印度尼西亚通量(ITF)的大规模运输的年际变化很可能与太平洋和/或印度洋偶极子(IOD)的厄尔尼诺(n)o-南方涛动(ENSO)有关。 IPSL(皮埃尔-西蒙·拉普拉斯研究所)耦合的一般环流模型(CGCM)用于检验ITF的年际变化并了解其与两个盆地气候变化的关系。进行了1000次积分,并利用了年平均模型输出。在印尼海域内,模拟ITF的路径是合理的。主要运输发生在上游300 m,年平均运输量为15.68×106 m3 / s,其中通过望加锡海峡的主要运输量为13.83×106 m3 / s。 ITF传输的年际变化在2〜4 a周期内很显着。在年际时间尺度上,印度尼西亚海域(分别位于赤道以北的西太平洋和爪哇岛南海岸的海平面)之间的海平面差异与ITF传输之间的关系是直接的,同时相关系数为0.82。进一步的调查表明,热带太平洋先前的气候变化与ITF的运输异常有关。类似于ENSO的模式将ITF传输的极限领先了1 a,Ni(n)o 3 SST指数与ITF传输的0.37之间具有相关性。这意味着在进行大规模ITF输送之前,太平洋1a中往往会出现El Ni(n)o异常。 Ni(n)o 3 SST指数与ITF传输之间的同时相关性为-0.34。但是,海面温度和海面高度的模式不是典型的ENSO异常。 ITF的运输与印度洋上同时发生的年际变化有关。 ITF传输与偶极子模式指数之间的同时相关系数为0.46,并且上层异常的模式与IOD的模式非常相似。

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  • 来源
    《海洋学报(英文版)》 |2006年第1期|32-47|共16页
  • 作者

  • 作者单位

    State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

    Laboratoire de Meteorologie Dynamique, CNRS, Universite Pierre et Marie Curie, Paris, France;

    State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 chi
  • 中图分类 海洋学;
  • 关键词

    Indonesian Throughflow; ENSO; interannual variability;

    机译:印尼流量;ENSO;年际变化;
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