Frontiers in Marine Science (Nov 2023)

Numerical study of tidal effect on the water flux across the Korea/Tsushima Strait

  • Wenxin Jiang,
  • Wenxin Jiang,
  • Wenxin Jiang,
  • Wenxin Jiang,
  • Wenxin Jiang,
  • Dezhou Yang,
  • Dezhou Yang,
  • Dezhou Yang,
  • Dezhou Yang,
  • Dezhou Yang,
  • Lingjing Xu,
  • Lingjing Xu,
  • Lingjing Xu,
  • Lingjing Xu,
  • Zhiwei He,
  • Zhiwei He,
  • Zhiwei He,
  • Zhiwei He,
  • Xuan Cui,
  • Xuan Cui,
  • Xuan Cui,
  • Xuan Cui,
  • Baoshu Yin,
  • Baoshu Yin,
  • Baoshu Yin,
  • Baoshu Yin,
  • Baoshu Yin

DOI
https://doi.org/10.3389/fmars.2023.1287611
Journal volume & issue
Vol. 10

Abstract

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Tremendous amounts of materials and energy are transported from the East China Sea (ECS) to the East/Japan Sea (EJS) through the Korea/Tsushima Strait (KTS). Tides undoubtedly play an important role in regulating ocean circulation on the broad continental shelf of the ECS, while the effects of tides on the water exchange between the ECS and EJS remain unclear. Using a three-dimensional Regional Oceanic Modeling System (ROMS) circulation model, we conducted numerical experiments with tides, without tides, and only barotropic tides. The results showed that the water flux across the KTS can increase by up to 13% (in summer) when excluding tides from the numerical simulation. To understand how tidal forcing regulates the KTS water flux, we performed a dynamic diagnostic analysis and revealed that the variation in sea surface height under tidal effect is the main reason for the water flux variation across the KTS. The tidal effect can adjust the sea surface height, weaken the pressure gradient and reduce the water flux across the KTS, which affect the intensity of water exchange between the ECS and EJS. The tidal effect can alter sea level difference between the Taiwan Strait and the KTS, which influences the KTS water flux. Tides can also influence the KTS water flux by altering the sea surface height through interaction with topography and stratification. We also found that tidal effect weakens the northward intrusion of the Yellow Sea Warm Current in winter and in turn enhances the water flux across the KTS according to volume conservation. These modeling results imply that tides must be considered when simulating the ocean environment of the northwestern Pacific Ocean.

Keywords