Contribution of Kuroshio Recirculation to Nutrient Transport Along the Kuroshio South of Japan

Author(s):  
Xinyu Guo ◽  
Yingying Hu ◽  
Yoshikazu Sasai
2013 ◽  
Vol 838-841 ◽  
pp. 2361-2365
Author(s):  
Yu Long ◽  
Xiao Hua Zhu ◽  
Xin Yu Guo

To confirm Spatial variations of Kuroshio nutrient transport from the East China Sea to South of Japan, we apply an inverse method to hydrographic data from sections across the Kuroshio path from the East China Sea (Sections PN and TK) to south of Japan (Sections ASUKA and 137E) to get absolute geostrophic velocity, then the nutrient flux (velocity times concentration) and nutrient transport (integration of flux over a section) were calculated. In addition, Section OK east of the Ryukyu Islands was also examined. The nitrate flux during winter of 2009 shows a subsurface maximum core with a value of 11, 15, 7, 19,and 10 mol m-2s-1at Sections PN, TK, OK, ASUKA and 137E, respectively. The depth of subsurface maximum core is about 280, 470, 800, 200, and 470 m at Sections PN, TK, OK, ASUKA and 137E, respectively. The eastward nitrate transport is 248.6,213.3,97.7,804.3,879.0 k mol s-1at Sections PN, TK, OK, ASUKA and 137E, respectively. Comparisons between nitrate transport through Section ASUKA and the sum of transports through Sections TK and OK and nitrate transport of Section 137E, suggest that the Kuroshio recirculation south of Shikoku can significantly intensify the eastward nitrate transport by the Kuroshio and therefore plays an important role in the nitrate transport in the Kuroshio region.


2006 ◽  
Vol 56 (5-6) ◽  
pp. 607-623 ◽  
Author(s):  
Norihisa Usui ◽  
Hiroyuki Tsujino ◽  
Yosuke Fujii ◽  
Masafumi Kamachi

2001 ◽  
Vol 28 (1) ◽  
pp. 17-20 ◽  
Author(s):  
Shiro Imawaki ◽  
Hiroshi Uchida ◽  
Hiroshi Ichikawa ◽  
Masao Fukasawa ◽  
Shin-ichiro Umatani ◽  
...  

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