Skip to main content
Log in

Slope-Current fluctuations northeast of Taiwan winter 1990

  • Published:
Journal of the Oceanographical Society of Japan Aims and scope Submit manuscript

Abstract

During the winter of 1990, two current-meter moorings were deployed in the outer shelf region across a canyon northeast of Taiwan. The data indicate that a steady flow exists in the southward, along-slope direction, opposite to the nearby northward-flowing Kuroshio current. Tides run transverse to the mean flow. Fluctuations in subtidal current mostly occur on the south side of the canyon, concentrated in the synoptic (2–4 days) band and oriented in the cross-slope direction. From the nearby winds and coastal sea-level observations, it is clear that the rotating-wind field associated with the passage of winter cold front is responsible for generating the observed energetic fluctuations. The northeasterly monsoon wind is very effective in piling up water against the northern coast of Taiwan and establishing an out-flowing geostrophic current. Trailing wind behind the high-pressure system has exactly the opposite effect. The investigation suggests that due to the winter-weather pattern, the area northeast of Taiwan is an important region for water exchange between the East China Sea and the Kuroshio.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Institutional subscriptions

Similar content being viewed by others

References

  • Chao, S.-Y. (1990): Circulation of the East China Sea, a numerical study. J. Oceanogr. Soc. Japan,46, 273–295.

    Article  Google Scholar 

  • Chern, C.-S. (1982): A preliminary study on the response of Taiwan Strait to winter monson. Acta Oceanogr. Taiwanica,13, 124–139.

    Google Scholar 

  • Chern, C.-S., J. Wang, and D.-P. Wang (1990): The exchange of Kuroshio and East China Sea shelf water. J. Geophys. Res.,95, 16017–16023.

    Google Scholar 

  • Chuang, W.-S. (1985): Dynamics of subtidal flow in Taiwan Strait. J. Oceanogr. Soc. Japan,41, 65–72.

    Article  Google Scholar 

  • Chuang, W.-S. (1986): A note on the driving mechanisms of current in the Taiwan Strait. J. Oceanogr. Soc. Japan,42, 355–361.

    Article  Google Scholar 

  • Guan, B. (1984): Major features of the shallow water hydrography in the East China Sea and Huanghai Sea. p. 1–13. In: Ocean Hydrodynamics of the Japan and East China Seas, ed. by T. Ichiye, Elsevier, New York.

    Google Scholar 

  • Hsueh, Y., R. D. Romea and P. W. deWitt (1986): Wintertime winds and coastal sea-level fluctuations in the Northeast China Sea. Part II: Numerical model. J. Phys. Oceanogr.,16, 241–261.

    Article  Google Scholar 

  • Hsueh, Y. and J. H. Tinsman (1987): A comparison between geostrophic and observed winds at a Japan Meteorological Agency buoy in the East China Sea. J. Oceanogr. Soc. Japan,43, 251–257.

    Article  Google Scholar 

  • Kundu, P. K., and J. S. Allen (1976): Some three-dimensional characteristics of low-frequency current fluctuations near the Oregon coast. J. Phys. Oceanogr.,6, 181–199.

    Google Scholar 

  • Nakamura Y., K. Miyaji, K. Tamai, and Y. Zheng (1990): On the characteristics of the oceanic front in the East China sea from the viewpoint of oceanic currents. p. 84–98. In: Proceedings of Japan-China Joint Symposium of the Cooperative Study on the Kuroshio, November 14–16, 1989, Tokyo.

  • Nitani, H. (1972): Beginning of the Kuroshio. p. 129–163. In: Kuroshio, Its Physical Aspects, ed. by H. Stommel and K. Yoshida, Univ. Tokyo Press, Tokyo.

    Google Scholar 

  • Noble M. and B. Butman (1989): The structure of subtidal currents within and around Lydonia Canyon: Evidence for enhanced cross-shelf fluctuations over the mouth of the Canyon. J. Geophys. Res.,94, 8091–8110.

    Google Scholar 

  • Pu, Y., Y. Su, and X. Xu (1987): Some features of the current field in the south of the East China Sea (in Chinese with English abstract). p. 33–43. In: Essays on the Investigation of Kuroshio, ed. by X. Sun, Ocean Press, Beijing.

    Google Scholar 

  • Sun, X. (1987): Analysis of the surface path of the Kuroshio in the East China Sea (in Chinese with English abstract). p. 1–14. In: Essays on the Investigation of Kuroshio, ed. by X. Sun, Ocean Press, Beijing.

    Google Scholar 

  • Uda, M. and A. Kishi (1974): Cyclonic cold eddies along the edge of the Kuroshio current in relation to the genesis and passage of cyclones, I. Waters north of Taiwan. p. 199–218. In: The Kuroshio III, Proceedings of the 3rd Symposium, Bangkok, Thailand, 1972.

  • Zhang, M., J. Yao, and J. Chen (1987): Preliminary analysis of meteorological features during the survey of Kuroshio in the East China Sea (in Chinese with English abstract). p. 247–255. In: Essays on the Investigation of Kuroshio, ed. by X. Sun, Ocean Press, Beijing.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Chuang, WS., Wu, CK. Slope-Current fluctuations northeast of Taiwan winter 1990. Journal of the Oceanographical Society of Japan 47, 185–193 (1991). https://doi.org/10.1007/BF02310034

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02310034

Keywords

Navigation