Interannual Climate Variability over the Tropical Pacific Ocean Induced by the Indian Ocean Dipole through the Indonesian Throughflow
Interannual Climate Variability over the Tropical Pacific Ocean Induced by the Indian Ocean Dipole through the Indonesian Throughflow
复制标题
印度洋偶极子通过印度尼西亚穿流引起的热带太平洋气候年际变化
DOI：
10.1175/jcli-d-12-00117.1
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发表时间：
2013-04
影响因子：
4.9
通讯作者：
Zhao, Xia
中科院分区：
文献类型：
--
作者：
Yuan, Dongliang;Zhou, Hui;Zhao, Xia
作者先前的动力学研究表明，通过印度尼西亚贯穿流的输送变化，印度洋和太平洋的年际气候变化之间存在联系。在这项研究中，这种海洋通道联系与……的一致性
The authors' previous dynamical study has suggested a link between the Indian and Pacific Ocean interannual climate variations through the transport variations of the Indonesian Throughflow. In this study, the consistency of this oceanic channel link with observations is investigated using correlation analyses of observed ocean temperature, sea surface height, and surface wind data. The analyses show significant lag correlations between the sea surface temperature anomalies (SSTA) in the southeastern tropical Indian Ocean in fall and those in the eastern Pacific cold tongue in the following summer through fall seasons, suggesting potential predictability of ENSO events beyond the period of 1 yr. The dynamics of this teleconnection seem not through the atmospheric bridge, because the wind anomalies in the far western equatorial Pacific in fall have insignificant correlations with the cold tongue anomalies at time lags beyond one season. Correlation analyses between the sea surface height anomalies (SSHA) in the southeastern tropical Indian Ocean and those over the Indo-Pacific basin suggest eastward propagation of the upwelling anomalies from the Indian Ocean into the equatorial Pacific Ocean through the Indonesian Seas. Correlations in the subsurface temperature in the equatorial vertical section of the Pacific Ocean confirm the propagation. In spite of the limitation of the short time series of observations available, the study seems to suggest that the ocean channel connection between the two basins is important for the evolution and predictability of ENSO.
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印度洋偶极子对热带太平洋年际变化的强迫：印度尼西亚通流的作用
影响因子：
4.9
作者：
Yuan, Dongliang;Wang, Jing;Xu, Tengfei;Xu, Peng;Hui, Zhou;Zhao, Xia;Luan, Yihua;Zheng, Weipeng;Yu, Yongqiang
通讯作者：
Yu, Yongqiang
影响因子：
3.1
作者：
K. Trenberth;Shyh-C. Chen
通讯作者：
K. Trenberth;Shyh-C. Chen
影响因子：
64.8
作者：
Saji, NH;Goswami, BN;Yamagata, T
通讯作者：
Yamagata, T
影响因子：
0.5
作者：
K. Pujiana;A. Gordon;J. Sprintall;Dwi Susanto
通讯作者：
K. Pujiana;A. Gordon;J. Sprintall;Dwi Susanto
影响因子：
--
作者：
J. Sprintall;A. Gordon;R. Murtugudde;R. Susanto
通讯作者：
J. Sprintall;A. Gordon;R. Murtugudde;R. Susanto