Journal cover Journal topic
Ocean Science An interactive open-access journal of the European Geosciences Union

Journal metrics

  • IF value: 2.985 IF 2.985
  • IF 5-year<br/> value: 2.790 IF 5-year
    2.790
  • CiteScore<br/> value: 2.70 CiteScore
    2.70
  • SNIP value: 1.191 SNIP 1.191
  • SJR value: 1.885 SJR 1.885
  • IPP value: 2.589 IPP 2.589
  • h5-index value: 25 h5-index 25
Ocean Sci., 5, 303-312, 2009
http://www.ocean-sci.net/5/303/2009/
doi:10.5194/os-5-303-2009
© Author(s) 2009. This work is distributed
under the Creative Commons Attribution 3.0 License.
 
03 Aug 2009
The Kuroshio exchange with the South and East China Seas
T. Matsuno1, J.-S. Lee2, and S. Yanao3 1Research Institute for Applied Mechanics, Kyushu University, Japan
2Ocean Research Team, National Fisheries Research & Development Institute, Korea
3Department of Earth System Science and Technology, Kyushu University, Japan
Abstract. The Kuroshio flows along the edges of the marginal East Asian seas such as the South China Sea (SCS) and East China Sea (ECS). Exchanges of materials and energy between the Kuroshio and the marginal seas partly control the environments of the marginal seas. In particular, saline water from the Kuroshio maintains certain salinity in the shelf water in the ECS. Nutrients from the subsurface of the Kuroshio may influence primary production on the shelf. We summarize how the Kuroshio comes into contact with the shelf water or marginal seas, describing phenomena related to the exchange between the Kuroshio and the ECS along with the SCS, using reports in the literature along with original data. The Kuroshio tends to intrude into the SCS through the Luzon Strait in various manners such as direct intrusion, associated with eddies and as a loop current. The Kuroshio intrusion into the shelf region of the ECS has distinct seasonal variation and the Taiwan Warm Current plays a significant role in the determination of water properties in the outer shelf associated with the Kuroshio intrusion. We then examine physical processes related to the interaction between the Kuroshio and shelf water. Interaction between the Kuroshio and the bottom topography is an important process in the control of the exchange around the shelf break. Vertical mixing and frontal eddies are also important factors that control the water exchange and formation of water masses in the outer shelf. Wind stress plays a significant role in the exchange with a rather event-like manner. To determine the source of the water masses, chemical tracers could be powerful tools and it is suggested that a significant part of the shelf water consists of Kuroshio intermediate water.

Citation: Matsuno, T., Lee, J.-S., and Yanao, S.: The Kuroshio exchange with the South and East China Seas, Ocean Sci., 5, 303-312, doi:10.5194/os-5-303-2009, 2009.
Publications Copernicus
Download
Share