

FOLLOWUS
1.School of Marine Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China
2.Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
3.Function Laboratory for Ocean Dynamics and Climate, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266000, China
4.Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China
YANG Dezhou, E-mail: yangdezhou@qdio.ac.cn
收稿:2020-01-14,
录用:2020-3-16,
网络首发:2021-04-01,
纸质出版:2021-03
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Numerical study on interaction between eddies and the Kuroshio Current east of Taiwan, China[J]. 海洋湖沼学报(英文), 2021,39(2):388-402.
Yunlong SHI, Dezhou YANG, Yijun HE. Numerical study on interaction between eddies and the Kuroshio Current east of Taiwan, China[J]. Journal of Oceanology and Limnology, 2021, 39(2): 388-402.
Numerical study on interaction between eddies and the Kuroshio Current east of Taiwan, China[J]. 海洋湖沼学报(英文), 2021,39(2):388-402. DOI: 10.1007/s00343-020-0010-0.
Yunlong SHI, Dezhou YANG, Yijun HE. Numerical study on interaction between eddies and the Kuroshio Current east of Taiwan, China[J]. Journal of Oceanology and Limnology, 2021, 39(2): 388-402. DOI: 10.1007/s00343-020-0010-0.
We investigated the interaction between mesoscale eddies and the Kuroshio Current east of Taiwan
China
using a fine-resolution regional general circulation model. Mesoscale eddies are injected into a region east of Taiwan
China
according to the quasi-geostrophic theory of stratified fluids. Modeled eddies propagated westward at the velocity of the first baroclinic mode Rossby wave. When eddies collide with the Kuroshio Current east of Taiwan
China
the spatial structure and volume transport of the Kuroshio Current shows a significant variation. The upper 600 m of the anticyclonic eddy cannot cross the Kuroshio Current to reach the region west of the Kuroshio Current; rather
these waters flow northward along the eastern side of the Kuroshio Current. The upper water carried by the anticyclonic eddies cannot reach the shelf of the East China Sea (ECS). In contrast
the waters in the upper layer of the cyclonic eddy reach the western side of the Kuroshio Current and then flow northward. The dynamic mechanism analysis shows that the interaction between the Kuroshio Current and the cyclonic (anticyclonic) eddy decrease (increase) the horizontal potential vorticity (PV) gradient
or PV barrier
whereby the cyclonic (anticyclonic) eddy can (cannot) cross the Kuroshio Current. This study implies that the continental shelf could potentially be influenced by cyclonic eddies in the open ocean
which can transport heat and material from the upper open ocean across the Kuroshio Current to the shelf waters.
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