Effects of mesoscale eddies on the volume transport and branch pattern of the Kuroshio east of Taiwan
Effects of mesoscale eddies on the volume transport and branch pattern of the Kuroshio east of Taiwan
复制标题
中尺度涡旋对台湾东部黑潮体积输送及分支格局的影响
DOI:
10.1002/2016jc012038
复制
发表时间:
2016
期刊:
影响因子:
--
通讯作者:
Zhang Linlin
中科院分区:
文献类型:
--
作者:
Yan Xiaomei;Zhu Xiao-Hua;Pang Chongguang;Zhang Linlin
Using satellite altimeter data and a long-term altimetric transport index for the Kuroshio inflow northeast of Taiwan, the effects of mesoscale eddies on the Kuroshio volume transport (KVT) at the East Taiwan Channel and the branching pattern of the Kuroshio east of Taiwan are investigated at scales from those of individual events to interannual timescales. Both anticyclonic and cyclonic eddies are found to be able either to strengthen or weaken the KVT, depending on the relative strength of mass convergence and divergence produced upstream and downstream of the eddies. The major factor influencing the intensity of the Kuroshio inflow is the meridional location of the eddies. For single eddy events, the KVT is significantly correlated with the latitude of the eddy's center, the correlations being 0.44 and -0.48 for anticyclonic and cyclonic eddies, respectively. For dipole eddy events, when the direction angle falls in the interval 40°-150° (240°-300°), the KVT anomaly tends to be positive (negative). Furthermore, low KVT events generally correspond to the formation of the Ryukyu Current branch, which is also generated from strong mass divergence produced by the eddies. In addition, on interannual time scales, the variation of KVT is closely related to the relative number of anticyclonic to cyclonic eddies west of 125°E, with a correlation of 0.5. This article is protected by copyright. All rights reserved.