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What is Tide-Induced Residual Current?
Publisher: American Meteorological Society
Abstract: We carried out a numerical experiment to study the velocity field of a two-dimensional tidal current in a simple model basin with a narrow strait. It was found that the tide-induced transient eddy (TITE) originated from ...
A Numerical Experiment on Water and Salt Exchange through the Akashi and the Naruto Straits
Publisher: American Meteorological Society
Abstract: To study the relation between the water-volume exchange rates Ev and the salt-exchange rates Ez of the Akashi and the Naruto Straits in the Seto Inland Sea of Japan, we use an observed salt distribution near the straits, ...
An Event in Water Exchange between Continental Shelf and the Kuroshio off Southern Japan: Lagrangian Tracking of a Low-Salinity Water Mass on the Kuroshio
Publisher: American Meteorological Society
Abstract: Low-salinity water masses were occasionally observed in spring and summer on the surface of the Kuroshio, south of Japan. Many of the masses were accompanied by excessive discharge of fresh water from major rivers in ...
Numerical Study of Shelf Water Motion Driven by the Kuroshio: Barotropic Model
Publisher: American Meteorological Society
Abstract: The barotropic response of the shelf and coastal regions south of Japan to short-term variations in the Kuroshio was studied numerically with an inflow?outflow model. The onshore?offshore movements of the stream axis of ...
Tidal Exchange through a Strait: A Numerical Experiment Using a Simple Model Basin
Publisher: American Meteorological Society
Abstract: In order to investigate the mechanism of tidal exchange through a strait, we numerically track the Lagrangian movement of water particles over a full cycle of the M2 tide. As a result, it is found that the spatially rapid ...
A Numerical Study of a Shallow Sea Front Generated by Buoyancy Flux: Generation Mechanism
Publisher: American Meteorological Society
Abstract: We studied numerically the frontogenesis of shallow sea fronts such as are observed in the Kii Channel, Japan, during winter, under conditions of sea surface cooling and buoyancy influx from coast and open ocean. Numerical ...