Generation Mechanism of Tidally-driven Whirlpools at A Narrow Strait in An Estuary. Issue 1 (December 2021)

• Record Type: Journal Article
• Authors: Uchiyama, Yusuke; Zhang, Xu; Yanase, Shota
• Is Part Of: IOP conference series. Volume 945:Issue 1(2021)
• Publication Date: 2021-12
• Subjects: Tidal Strait -- Tidal Current -- Sub-mesoscale Eddies -- Whirlpools -- Ocean Circulation Model; Earth sciences -- Periodicals; Environmental sciences -- Congresses; Environmental sciences -- Periodicals; 550.5
• DOI: 10.1088/1755-1315/945/1/012028
• Languages: English
• ISSNs: 1755-1307

Abstract

Abstract: This study investigates the generation mechanism and influence of the whirlpools in the Naruto Strait on the surrounding marine environment using state-of-the-art high-resolution numerical ocean circulation modeling in a quadruple nested configuration. The Naruto whirlpools is recognized as an extraordinary seascape that the local governments and the citizens seek to register as a world natural heritage site. We found that the pronounced pressure gradient force associated with the meridional surface elevation difference was induced by a phase difference of two bifurcating major tidal waves. These waves originate from the Kitan Strait, and ultimately produce intense tidal currents at the Naruto Strait. One branch of the tidal waves propagates counter-clockwise along Awaji Island through the Akashi Strait, while the other occurs directly from the Kii Channel. As such, the whirlpool emerges as a large number of sub-mesoscale eddies, primarily due to the horizontal shear instability of tidal currents energized at the narrow topography between two headlands that extend into the strait. A dipole of overturning vertical circulations appears underneath the whirlpools with convergent downward transport at the strongest tidal current near the center of the strait; this causes efficient vertical mixing. This three-dimensional non-linear mixing promotes a time-averaged southeastward mass transport that extracts water and materials from the Harima-nada Sea into the Kii Channel.