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Sources of water in the Taiwan Strait

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Abstract

The conveyor of the source water that feeds into the Taiwan Strait (TS), particularly from the south, is investigated using historical CTD (Conductivity-Temperature-Depth) data and a North Pacific Ocean and East Asian seas coupled model. The modeled currents and drifter trajectories suggest that the Kuroshio Branch Water (KBW) rarely flows directly into the TS from the Luzon Strait (LS) in winter; instead the massive westward movement of the Kuroshio conveys high salinity water to the southeastern TS through a loop-like route. In summer, the modeled flow fields suggest that the Kuroshio surface currents hardly intrude into the TS directly from the LS. Observations and model results show that the monsoon-driven northeastwardflowing currents in the northern South China Sea transport relatively low salinity water through the entire TS.

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Authors and Affiliations

  1. Institute of Hydrological and Oceanic Sciences, National Central University, 300 Jung-da Rd., Jung-li, 32001, Taiwan, R.O.C.

    Sen Jan

  2. Department of Atmospheric Science, National Taiwan University, 1, Sec. 4, Roosevelt Rd., Taipei, 10617, Taiwan, R.O.C.

    Yu-Heng Tseng & David E. Dietrich

  3. AcuSea, Inc., 8450-101 Via Sonoma, La Jolla, CA, 92037, USA

    David E. Dietrich

  4. Institute of Oceanography, National Taiwan University, 1, Sec. 4, Roosevelt Rd., Taipei, 10617, Taiwan, R.O.C.

    Sen Jan

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  1. Sen Jan
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  2. Yu-Heng Tseng
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  3. David E. Dietrich
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Correspondence to Sen Jan.

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Jan, S., Tseng, YH. & Dietrich, D.E. Sources of water in the Taiwan Strait. J Oceanogr 66, 211–221 (2010). https://doi.org/10.1007/s10872-010-0019-7

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