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1998 년 춘계 제주도 북서쪽해역에 출현하는 저밀도수의 거동 특성
김상현(Sang Hyun Kim),노홍길(Hong Kil Rho),송야건(Takeshi Matsuno) 한국수산과학회 2002 한국수산과학회지 Vol.35 No.1
N/A The low temperature, low salinity and low density sea water which was originated from the southern part of the Yellow Sea and distributed from the surface to 20 m depth was transported by the northwesterly wind during the period from the middle of March to the beginning of April, 1998 and had an influence on the northern coastal sea area of Cheju Island. Accordingly, this kind of accumulated data may supply the fundamental data for the realtime monitoring of oceanographic conditions and may improve degree of the forecasting accuracy of fishing and oceanographic conditions.
On the Origin of the Tsushima Current ( Ⅰ ) : Barotropic Case
방익찬 ( Ig Chan Pang ),김태희 ( Tae Hee Kim ),송야건 ( Takeshi MATSUNO ),노홍길 ( Hong Kil Rho ) 한국수산과학회 1993 한국수산과학회지 Vol.26 No.6
The Tsushima Current has been known to branch out from the Kuroshio west of Kyushu and to flow north to the Korea Strait. Then, it has to flow across the isobaths and so needs some driving forces. As the forces, sea level difference between the Korea and Tsugaru Straits, Reynolds stress west of Kyushu and density differences have been suggested, In this paper, their roles have been numerically studied in the barotropic case. Model results show that the Tsushima Current is possible without any above force. The flows just follow isobaths over the East China Sea. They seem to be driven by their own dynamics without any external force. The mechanism is just like outflows from a gap. Model results also show that the flows in this area could be significantly affected by the external forces such as Reynolds Stress. Then the dynamics and flows in real ocean might be complicated. However, the barotropic study tells us that the Tsuahima Currents is basically driven by geostrophic adjustment.