Dietary overlap and optimal prey environments of larval and juvenile sardine and anchovy in the mixed water region of the western North Pacific

2019 ◽  
Vol 630 ◽  
pp. 149-160
Author(s):  
Y Okazaki ◽  
K Tadokoro ◽  
H Kubota ◽  
Y Kamimura ◽  
K Hidaka
Keyword(s):  
North Pacific ◽  
Western North Pacific ◽  
Dietary Overlap ◽  
Mixed Water Region ◽  
Water Region ◽  
Mixed Water

North Pacific Intermediate Water in the Kuroshio/Oyashio Mixed Water Region

1995 ◽  
Vol 25 (4) ◽  
pp. 475-501 ◽  
Author(s):  
Lynne D. Talley ◽  
Yukata Nagata ◽  
Masahiko Fujimura ◽  
Takanori Iwao ◽  
Tokihiro Kono ◽  
...  
Keyword(s):  
North Pacific ◽  
Intermediate Water ◽  
North Pacific Intermediate Water ◽  
Mixed Water Region ◽  
Water Region ◽  
The Kuroshio ◽  
Mixed Water

scholarly journals Effect of Decadal Kuroshio Extension Jet and Eddy Variability on the Modification of North Pacific Intermediate Water

2011 ◽  
Vol 41 (3) ◽  
pp. 503-515 ◽  
Author(s):  
Bo Qiu ◽  
Shuiming Chen
Keyword(s):  
North Pacific ◽  
North Pacific Ocean ◽  
Kuroshio Extension ◽  
Mesoscale Eddy ◽  
Dynamic State ◽  
Intermediate Water ◽  
North Pacific Intermediate Water ◽  
Mixed Water Region ◽  
Water Region ◽  
Mixed Water

Abstract Salinity modifications in the North Pacific Intermediate Water (NPIW) core layer of 26.7–26.8 σθ in the western North Pacific Ocean are investigated using temperature–salinity data from available profiling float and hydrographic measurements in 2002–09. During 2002–05, when the Kuroshio Extension (KE) jet was intense and zonally elongated, coherent positive salinity anomalies appeared along the inflow KE jet southeast of Japan and in the downstream Mixed Water region east of 152°E. Broad-scale negative salinity anomalies were detected south of the KE jet and in the upstream Mixed Water region west of 152°E. The signs of these observed salinity anomalies were reversed in 2006–09, when the KE jet transitioned to a weakened and zonally contracted dynamic state. By adopting an isopycnal advection–diffusion model and conducting model runs with the time-dependent advective field inferred from the eddy-resolving satellite altimeter sea surface height data, it is found that the observed salinity anomalies are oscillatory in nature and are determined not only by the decadally varying KE jet itself but also by mesoscale eddy signals that modulate temporally and longitudinally along the path of the KE jet.

Congruence between euphausiid community and water region in the northwestern Pacific: particularly in the Oyashio–Kuroshio Mixed Water Region

2012 ◽  
Vol 69 (1) ◽  
pp. 71-85 ◽  
Author(s):  
Sayaka Sogawa ◽  
Hiroya Sugisaki ◽  
Hiroaki Saito ◽  
Yuji Okazaki ◽  
Shinji Shimode ◽  
...  
Keyword(s):  
Northwestern Pacific ◽  
Mixed Water Region ◽  
Water Region ◽  
Mixed Water

Transport of subarctic large copepods from the Oyashio area to the mixed water region by the coastal Oyashio intrusion

2009 ◽  
Vol 18 (5) ◽  
pp. 312-327 ◽  
Author(s):  
YUGO SHIMIZU ◽  
KAZUTAKA TAKAHASHI ◽  
SHIN-ICHI ITO ◽  
SHIGEHO KAKEHI ◽  
HIROAKI TATEBE ◽  
...  
Keyword(s):  
Mixed Water Region ◽  
Water Region ◽  
Mixed Water

Transport of Oyashio Water across the Subarctic Front into the Mixed Water Region and Formation of NPIW

2003 ◽  
Vol 59 (6) ◽  
pp. 855-869 ◽  
Author(s):  
Masachika Masujima ◽  
Ichiro Yasuda ◽  
Yutaka Hiroe ◽  
Tomowo Watanabe
Keyword(s):  
Mixed Water Region ◽  
Subarctic Front ◽  
Oyashio Water ◽  
Water Region ◽  
Mixed Water
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