제주도-고오또 열도 사이를 통과하는 대마난류 = Tsushima Warm Current Passing though Cheju-Goto Channel

다국어 초록 (Multilingual Abstract)

Main route of Tsushima Warm Current (TWC) and a roundabout flow near Goto Islands were examined by water mass analysis and geostrophic calcualtion with hydrographic data observed in the sea between Cheju and Gotto Islands in winter, spring, 1998 and summer. 1994. Most of warm and saline waters which distribute in the center of Cheju-Gotto channel in winter link with waters from the southwest but not to link with waters from the southeast of Gotto Islands. Warm and saline waters near Gotto Islands seems to turn around the islands and to go southward along the iso-bath line. Geostrphic calculation shows that volume transports passing through Cheju-Gotto channel is about 26.9 Sv in winter. 16.4 Sv in spring and summer. But volume transport in the depths of 100-150m is a little larger in summer than in winter. which supports the fact that transport volume passing the western channel of Korean Straits is two times larger in summer than in winter.

목차 (Table of Contents)

• 서론 = 91
• 대마난류의 주축은 제주도-고오또 사이에서 어디로 통과하는가? = 93
• 체적수송량의 계절 변동 = 93
• 대마난류수와 남해연안수의 경계 = 100
• 결론 및 토의 = 102
• 요약 = 103
• 사사 = 104
• <참고문헌> = 104