Characteristics of the Kuroshio in the vicinity of the Izu Ridge

1985 ◽  
Vol 41 (6) ◽  
pp. 441-451 ◽  
Author(s):  
Kazuyuki Otsuka
Keyword(s):  
The Kuroshio ◽  
Izu Ridge

Velocity fluctuations of the Kuroshio near the Izu Ridge and their relationship to current path

1981 ◽  
Vol 28 (10) ◽  
pp. 1187-1197 ◽  
Author(s):  
Keisuke Taira ◽  
Toshihiko Teramoto
Keyword(s):  
Velocity Fluctuations ◽  
Current Path ◽  
The Kuroshio ◽  
Izu Ridge

Eduction of hydrodynamical processes from cross-channel electric-potential differences in the Kuroshio area around the Izu Ridge

1994 ◽  
Vol 50 (3) ◽  
pp. 339-363 ◽  
Author(s):  
Toshihiko Teramoto ◽  
Hirobumi Kojima
Keyword(s):  
Electric Potential ◽  
The Kuroshio ◽  
Izu Ridge

scholarly journals Bedforms produced by the Kuroshio Current over the Izu Ridge: Side-scan sonar surveys around Kozu Sima, Nii-jima and Miyake Sima Islands, central Japan.

2002 ◽  
Vol 108 (2) ◽  
pp. 103-113 ◽  
Author(s):  
Yu'suke Kubo ◽  
Wonn Soh ◽  
Hideaki Machiyama ◽  
Hidekazu Tokuyama
Keyword(s):  
Kuroshio Current ◽  
Central Japan ◽  
Side Scan Sonar ◽  
The Kuroshio ◽  
Izu Ridge

scholarly journals Blocking of the Kuroshio Large Meander by Baroclinic Interaction with the Izu Ridge

2006 ◽  
Vol 36 (11) ◽  
pp. 2042-2059 ◽  
Author(s):  
Humio Mitsudera ◽  
Bunmei Taguchi ◽  
Takuji Waseda ◽  
Yasushi Yoshikawa
Keyword(s):  
Rossby Waves ◽  
Western Slope ◽  
Large Meander ◽  
Kuroshio Large Meander ◽  
Topographic Rossby Waves ◽  
The Kuroshio ◽  
Izu Ridge ◽  
Sloping Bottom

Abstract This paper discusses the role of the Izu Ridge in blocking the Kuroshio large meander from propagating eastward across the ridge. It is shown that a combination of the sloping bottom with baroclinicity in the Kuroshio flow is important for blocking of the large meander. It produces a cyclonic torque over the western slope of the ridge when the large meander impinges upon it. That is, the cyclonic torque is formed ahead of the large meander, which results in blocking and amplification of the meander upstream of the Izu Ridge. The baroclinicity of the Kuroshio over the ridge is caused by baroclinic topographic Rossby waves generated when the large meander encounters the ridge.

Temperature structure and mixed layer in the Kuroshio Region over the Izu Ridge

1988 ◽  
Vol 46 (4) ◽  
pp. 683-700 ◽  
Author(s):  
Kimio Hanawa ◽  
Izumi Hoshino
Keyword(s):  
Mixed Layer ◽  
Temperature Structure ◽  
The Kuroshio ◽  
Izu Ridge ◽  
Kuroshio Region

Enhanced vertical turbulent nitrate flux in the Kuroshio across the Izu Ridge

2018 ◽  
Vol 75 (2) ◽  
pp. 195-203 ◽  
Author(s):  
T. Tanaka ◽  
D. Hasegawa ◽  
I. Yasuda ◽  
H. Tsuji ◽  
S. Fujio ◽  
...  
Keyword(s):  
Nitrate Flux ◽  
The Kuroshio ◽  
Izu Ridge

Bedforms produced by the Kuroshio Current passing over the northern Izu Ridge

2004 ◽  
Vol 24 (1) ◽  
pp. 1-7 ◽  
Author(s):  
Hidekazu Tokuyama ◽  
Yu'suke Kubo ◽  
Wonn Soh ◽  
Hideaki Machiyama
Keyword(s):  
Kuroshio Current ◽  
Current Passing ◽  
The Kuroshio ◽  
Izu Ridge

Biophysical variability in the Kuroshio Extension from altimeter and SeaWiFS

OCEANS 2009 ◽  
2009 ◽  
Author(s):  
Peter C. Chu ◽  
Yu-heng Kuo
Keyword(s):  
Kuroshio Extension ◽  
The Kuroshio

Cold air outbreak over the Kuroshio extension region

OCEANS 2009 ◽  
2009 ◽  
Author(s):  
T. G. Jensen ◽  
T. Campbell ◽  
T. A. Smith ◽  
R. J. Small ◽  
R. Allard
Keyword(s):  
Kuroshio Extension ◽  
Cold Air ◽  
Cold Air Outbreak ◽  
The Kuroshio ◽  
Kuroshio Extension Region
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