Along the southwest coast of the Kii Peninsula, a bifurcation current is regularly observed. By using ADCP data taken on board the R/V Wakayama of the Wakayama Prefectural Fisheries Experimental Station, characteristics of this bifurcation current are analyzed. The occurrence frequency of the bifurcation current reaches about 70 % in the period from 1988 to 1996. The bifurcation point appears to be changeable and occurs almost evenly between Cape Ichie and Cape Shionomisaki. The current divergence in the alongshore direction was also investigated. Positive divergence values dominated in the whole analyzed area, and an onshore current appears to be dominant along the southwest coast of the Kii Peninsula, except in 1990 when the Kuroshio flow...
The sectional structures of current in the western channel of the Tsushima/Korea Strait were repeate...
The relationship between the variations of the Tsushima Current at the entrance of the East Sea and ...
Oyashio water flowing into the Mixed Water Region (MWR) and the Kuroshio Ex-tension region that form...
The Kii Bifurcation Current is often found along the southwest coast of the Kii Pe-ninsula, and its ...
mapped since fall 2000 using a pair of SeaSonde long-range HF radars. During September 2000 through ...
The shallow coastal water of the Enshu-Nada Sea (ENSW) recirculates regardless of whether the Kurosh...
In the two decades following 1975, the Kuroshio path south of Japan was observed to oscillate intera...
The sea level difference between Kushimoto and Uragami, located to the west and east of the southern...
Several long-term current records, which were obtained from the mooring systems settled in the south...
An analytical model of the branching of an inertial current partly afloat incident upon a step fall ...
Since the Intermediate Oyashio Water (IOW) gradually accumulates in Sagami Bay, it can reasonably be...
⋅ conditions for large meander, ⋅ eddy interaction, ⋅ current axis curvature, ⋅ current velocity, ⋅ ...
The distributions and conditions of surface currents are described on the basis of the data obtained...
The Kuroshio is the western boundary current of the North Pacific mid-latitude gyre. An observationa...
This paper reports on the strength and structure of the Kuroshio Extension and its recirculation gyr...
The sectional structures of current in the western channel of the Tsushima/Korea Strait were repeate...
The relationship between the variations of the Tsushima Current at the entrance of the East Sea and ...
Oyashio water flowing into the Mixed Water Region (MWR) and the Kuroshio Ex-tension region that form...
The Kii Bifurcation Current is often found along the southwest coast of the Kii Pe-ninsula, and its ...
mapped since fall 2000 using a pair of SeaSonde long-range HF radars. During September 2000 through ...
The shallow coastal water of the Enshu-Nada Sea (ENSW) recirculates regardless of whether the Kurosh...
In the two decades following 1975, the Kuroshio path south of Japan was observed to oscillate intera...
The sea level difference between Kushimoto and Uragami, located to the west and east of the southern...
Several long-term current records, which were obtained from the mooring systems settled in the south...
An analytical model of the branching of an inertial current partly afloat incident upon a step fall ...
Since the Intermediate Oyashio Water (IOW) gradually accumulates in Sagami Bay, it can reasonably be...
⋅ conditions for large meander, ⋅ eddy interaction, ⋅ current axis curvature, ⋅ current velocity, ⋅ ...
The distributions and conditions of surface currents are described on the basis of the data obtained...
The Kuroshio is the western boundary current of the North Pacific mid-latitude gyre. An observationa...
This paper reports on the strength and structure of the Kuroshio Extension and its recirculation gyr...
The sectional structures of current in the western channel of the Tsushima/Korea Strait were repeate...
The relationship between the variations of the Tsushima Current at the entrance of the East Sea and ...
Oyashio water flowing into the Mixed Water Region (MWR) and the Kuroshio Ex-tension region that form...