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Physical Envirionment Associated with Upwelling off the Southeast Coast of Korea

한국 남동해안의 용승과 관련된 물리환경

  • 이재철 (부경대학교 해양학과) ;
  • 김대현 (오션테크(주) 해양시스템연구소)
  • Received : 2018.07.13
  • Accepted : 2018.08.17
  • Published : 2018.10.31

Abstract

Data from the two bottom moorings of ADCP (acoustic doppler current profiler), coastal weather station and CTC (conductivity temperature depth) observations for 2001 were analyzed to describe the physical processes associated with upwelling off the southeast coast of Korea. Winds were favorable for upwelling during summer, but were not correlated with currents. Shoaling of isotherms toward the coast due to the baroclinic tilting of the strong East Korean Warm Current (EKWC) provided a favorable background for immediate upwelling-response of surface temperature to southerly winds. This baroclinic effect was supported by a significant inverse coherence between the upper-layer current and bottom temperature near the coast. This upwelling is similar to the Guinea Current upwelling, which is driven by remote forcing (Houghton, 1989). Persistent southward flow was observed below approximately $10^{\circ}C$ isotherm throughout the observation period.

Keywords

References

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