• Proceedings of the KSRS Conference
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• 2006.03a
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• pp.91-94
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• 2006

China Coastal Waters (CCW) usually appears in the seas surrounding Jeju Island annually(June to October) and is very pronounced in August. Generally, low-salinity water appears to the western seas of Jeiu Island from June through October and gradually propagates to the eastern seas, where CCW meets the Tsushima Current. Empirical orthogonal function (EOF) analysis of SLAs and SSTs indicated that the valiance in SLAs and SSTs was 95.05%(the first mode to third mode) and 98.09%(the first mode), respectively The PSD of the western waters for the first mode of EOF analysis of SLAs was stronger than that of the eastern waters because of the influence of CCW. The PSD for the EOF analysis of SSTs was similar in all areas (the Yangtze Estuary and the seas to the west and east of Jeju Island), with a period of approximately 260 days.

• Proceedings of the Korean Society of Fisheries Technology Conference
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• 2001.10a
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• pp.200-201
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• 2001

제주도 연안 천해역 환경은 대마난류수, 한국남해연안수, 중국대륙연안수, 황해 저층냉수 등의 외해에 분포하고 있는 여러 수괴에 의해 영향을 받고 있지만 이외에도 제주도의 강수량, 기온, 북서계절풍 등과 같은 기상상태나 육수유입, 파랑, 조석상태 등에 의해서도 크게 영향을 받아 시ㆍ공간적 차가 생길 것으로 판단된다. (중략)

• Korean Journal of Remote Sensing
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• v.21 no.6
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• pp.469-482
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• 2005

China Coastal Waters (CCW) usually appears in the seas surrounding Jeju Island annually(June to October) and is very pronounced in August. Generally, low-salinity water appears to the western seas of Jeju Island from June through October and gradually propagates to the eastern seas, where CCW meets the Tsushima Current. Empirical orthogonal function (EOF) analysis of SLAs and SSTs indicated that the variance in SLAs and SSTs was $95.01\%$(the first mode to third mode) and $98.09\%$(the first mode), respectively. The PSD of the western waters for the first mode of EOF analysis of SLAs was stronger than that of the eastern waters because of the influence of CCW. The PSD for the EOF analysis of SSTs was similar in all areas (the Yangtze Estuary and the seas to the west and east of Jeju Island), with a period of approximately 260 days.

• Proceedings of the Korean Society of Fisheries Technology Conference
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• 2000.10a
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• pp.125-126
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• 2000

제주도 주변해역은 대마난류수, 황해난류수, 중국대륙연안수, 한국남해안연안수, 혼합수 등(노ㆍ평야, 1983; 노ㆍ김, 1983, 노, 1985; 조, 1988, 김ㆍ노, 1994)의 이질수괴가 출현하고, 이들 이질수괴의 경계역에는 계절에 따라 복잡한 수온전선을 형성(양 등, 1998)하고 있다. 또한 제주해협내에서는 12월부터 익년 4월까지 연직적으로 균질한 동계해황(김ㆍ노, 1997)을 나타내고, 5월부터 춘계해황이 시작되는 특성을 나타내나 아직까지 그 구체적이고 광역에 대한 조사가 이루어지지 않았다. (중략)

• Proceedings of the Korean Society of Fisheries Technology Conference
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• 2001.05a
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• pp.246-247
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• 2001

대마난류수, 황해난류수, 황해냉수, 중국대륙연안수, 한국남해안연안수, 혼합수등(노ㆍ平野, 1983; 노ㆍ김, 1983, 노, 1985; 조, 1988, 김ㆍ노, 1994)의 이질수괴가 출현하고 있는 제주도 주변해역은 산업적으로 중요한 어종(조기, 갈치, 고등어, 전갱이, 오징어 등)의 산란ㆍ생육ㆍ섭이장이 되는 어업적으로 상당히 중요한 해역 이며, 또한 이들 수괴들의 경계 역에서의 SST 전선과 고등어 선망어장과의 관계는 연관성이 높은 것으로 나타났다(양 등, 1999). (중략)

• Korean Journal of Fisheries and Aquatic Sciences
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• v.27 no.5
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• pp.515-528
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• 1994

China Coastal Water(CCW) appeared in the neighbouring seas of Cheju Island has been analyzed and the results are as follows: The water with salinity below $32.20\%0$ in the neighbouring seas of Cheju Island in summer is thought CCW. During the period from April 1985 to August 1986, salinity of more than $34.00\%0$ was appeared in the Cheju Strait during January to mid May, but it decreased gradually from late May. CCW with salinity below $32.20\%0$ appeared in the Cheju Strait in early July and disappeared in October. The mean thickness of CCW in the Cheju Strait was about 25m and CCW had an influence of up to about 50m depth. And stratification structure of the Cheju Strait in summer was halocline between the surface and 50m depth and homogeneous salinity layer below 50m depth. It seems that although CCW appears in the wide area of neighbouring seas surface of Cheju Island in summer, the core of this CCW which has the lowest salinity flows into the Cheju Strait from the western seas of Cheju Island. This CCW flows out the east through the central part of the Cheju Strait and then seems to be transported further in the form of eddy.

• Proceedings of the Korean Society of Fisheries Technology Conference
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• 2001.10a
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• pp.39-40
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• 2001

제주도 주변해역은 계절에 따라 다양한 이질수괴(대마난류계수, 황해지층냉수계수, 중국대륙연안수, 한국남해연안수 등)가 출현하고 있으며 이들 여러수괴의 분포상태에 따라 고등어, 전갱이, 방어, 삼치 등과 같은 여러 회유성 어종이 시기별 출현상황이 달라지고 있다(노, 1985; Nakao, 1977; 김ㆍ노, 1994; 김, 1995). 그중 방어(Yellow tail, Seriola quinqueradiata, TEMMINCK et SCHL-ECEL)는 제주도 주변해역에는 추ㆍ동계가 되면 제주도 북서쪽 추자도 주변어장을 시작으로 제주해협의 화도(속칭:관탈도)를 거쳐 제주도 남서부 마라도로 연결되는 방어어장이 매년 형성되며 특히, l1∼12월 사이의 어획량은 전국 방어 채낚기어업의 어획량의 대부분을 차지하고 있을 정도로 그 규모가 매우크다. (중략)

• Proceedings of the Korean Society of Fisheries Technology Conference
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• 2002.10a
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• pp.133-134
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• 2002

제주해협에 접해 있는 한국남해연안역은 대체로 50m미만의 천해로써 제주해협에 비해 계절별로 하계에 저온ㆍ고염분수, 동계에 저온ㆍ저염분수가 출현해 해협내 연중 전선을 형성하는 해역으로서 특히, 한국 남해연안역에 위치해 있는 추자도 주변해역은 지형적 특성상 대마난류수, 한국 남해연안수와 중국대륙연안수, 황해저층냉수 등 이러한 이질수괴들이 시기와 계절별로 서로 상접하여 복잡한 해황을 형성하는 해역이다(Rho, 1985, 최, 1989, 김ㆍ노, 1994, Yoon, 1986, Rhoㆍ평야, 1983). (중략)

• Proceedings of the Korean Society of Fisheries Technology Conference
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• 2003.05a
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• pp.138-139
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• 2003

한국 남해역은 계절에 따라 대마난류, 황해저증 냉수괴 및 중국대륙연안수 등 다양한 수괴가 세력권을 달리하고 있어 다양한 해양환경 특성을 나타낸다. 따라서 본 연구에서는 수온전선역이 형성(국립수산진흥원, 2000)되는 해역을 대상으로 해수의 수온, 염분, 밀도 및 표층적물중의 IL, COD, Phaeopigment등에 의한 표층퇴적 환경과 와편모조류 cyst 군집으로부터 이 지역의 해양환경 특성을 파악해 보고자 한다. (중략)

• Proceedings of the Korean Institute of Information and Commucation Sciences Conference
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• v.9 no.1
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• pp.383-386
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• 2005

CCW(China Coastal Water) is different each year. It appears clearly from June to October in the neighboring sea of Jeju island. It appears in June, and it's strong most in August, after tat disappears in October. CCW appeared clearly at 1996 and 1999 during investigation period(1995 to 1999). SLA and SST appear annual variations(about 365day), semi-annual variations(about 180day) from power spectral density. After PCA(Principal component analysis), it's different. PCA of SLA shows 43day variations and PCA of SST shows 259day variations. SLA and SST appear annual variation, semi-annual variation and seasonal variation from power spectral density. SLA appeared that summer and fall of 1996 and 1999 is higher than other years. It seem to be being the relationship which is close with the severe rain strom. Temperature distribution of sea surface according to season is different, but clearly water temperature boundary divides this area into Yellow Sea and East China Sea. It considered that CCW follow according to boundary of temperature. The variation which it follows at time of SLA and SST is faster about one month to three month at Yangtz.