Renewal of the bottom water after the winter 2000–2001 may spin-up the thermohaline circulation in the Japan Sea

2002 ◽  
Vol 29 (7) ◽  
Author(s):  
Tomoharu Senjyu
2019 ◽  
Vol 59 (6) ◽  
pp. 1093-1096
Author(s):  
V. N. Karnaukh ◽  
A. F. Sergeev ◽  
V. B. Lobanov ◽  
P. Ya. Tishcenko

During the the 73th cruise of the RV Professor Gagarinskiy and 53th cruise of the RV Academic Oparin oceanological studies of the north-western Pacific, Japan and Okhotsk Seas were conducted. New data on the structure sea bottom, water composition as well as slope convection of the Japan Sea.


1998 ◽  
Vol 25 (5) ◽  
pp. 651-654 ◽  
Author(s):  
Yu-ichiro Kumamoto ◽  
Minoru Yoneda ◽  
Yasuyuki Shibata ◽  
Hiroshi Kume ◽  
Atsushi Tanaka ◽  
...  

2005 ◽  
Vol 61 (6) ◽  
pp. 1047-1058 ◽  
Author(s):  
Tomoharu Senjyu ◽  
Yutaka Isoda ◽  
Takafumi Aramaki ◽  
Shigeyoshi Otosaka ◽  
Shinzo Fujio ◽  
...  

2015 ◽  
Vol 71 (4) ◽  
pp. 441-447 ◽  
Author(s):  
Takeshi Matsuno ◽  
Takahiro Endoh ◽  
Toshiyuki Hibiya ◽  
Tomoharu Senjyu ◽  
Michio Watanabe

Radiocarbon ◽  
2007 ◽  
Vol 49 (2) ◽  
pp. 915-924 ◽  
Author(s):  
T Aramaki ◽  
T Senjyu ◽  
O Togawa ◽  
S Otosaka ◽  
T Suzuki ◽  
...  

Radiocarbon concentrations in the northernmost region of the Japan Sea were observed during the summer of 2002. The averaged surface δ14C (above 100 m depth) was 52 ± 8%, which is significantly higher compared with the values of the Pacific Ocean and Okhotsk Sea. The δ14C in the deep water decreased with density, and the minimum value was −70%. By analyzing 14C and other hydrographic data, we found that i) the Tsushima Warm Current Water reaches to the surface layer in the southern Tatarskiy Strait; ii) deep convection did not occur in the northernmost region, at least not after the winter of 2001–2002; and iii) the bottom water that was previously formed in this region may step down southward along the bottom slope and mix with the Japan Sea Bottom Water. Furthermore, a new water mass characterized by high salinity (>34.09 psu) was found in the subsurface layer in the area north of 46°N.


Sign in / Sign up

Export Citation Format

Share Document