The impact of Kuroshio water on the source water of the southeastern Taiwan Strait: numerical results

The impact of Kuroshio water on the source water of the southeastern Taiwan Strait: numerical results
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黑潮水对台湾海峡东南部水源水的影响:数值结果

DOI:
10.1007/s13131-015-0720-x
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发表时间:
2015-09
影响因子:
1.4
通讯作者:
Huang Tinghsuan
Huang Tinghsuan
中科院分区:
地球科学2区
文献类型:
--
作者:
Zhang Wenzhou;Zhuang Xuefen;Chen, Chentung Arthur;Huang Tinghsuan

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利用1991 - 2008年太平洋全海盆三维物理-地球化学模式的模拟结果,研究了黑潮对台湾海峡东南部源水的影响。根据黑潮和南海海水的特征盐度,设计了黑潮影响指数(KII)来衡量黑潮对南海海水的影响程度。KII与风应力的东北-西南分量显著相关,但前者滞后于后者约两个月。两者的相关系数从0.2674增加到0.8529,滞后时间从0增加到63天。冬春季黑潮水的影响大于夏秋季。在年际时间尺度上,厄尔尼诺和拉尼娜事件在影响关键指标方面发挥着重要作用。在厄尔尼诺事件期间,台湾海峡东南部的源水来源于黑潮。相反,在拉尼娜事件期间,黑潮水对源水的贡献较少。
Model output from a Pacific basin-wide three-dimensional physical-biogeochemical model during the period of 1991 to 2008 was used to investigate the impact of Kuroshio water on the source water of the southeastern Taiwan Strait. Based on the characteristic salinities of both Kuroshio water and the South China Sea water, a Kuroshio impact index (KII) was designed to measure the degree of impact. The KII correlates significantly with the northeast-southwest component of wind stress, but the former lags the latter by approximately two months. The correlation coefficient between them increases from 0.267 4 to 0.852 9, with a lag time increasing from 0 to 63 days. The impact of Kuroshio Water is greater in winter and spring than in summer and autumn. At the interannual time scale, El Niño and La Niña events play an important role in impacting the KII. During El Niño events, more Kuroshio water contributes to the source water of the southeastern Taiwan Strait. Conversely, during La Niña events, less Kuroshio water contributes to the source water.
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