• 한국수산과학회지
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• 제25권2호
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• pp.151-163
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• 1992

황해, 동지나해와 제주도 주변해역의 해수분포의 계절변화를 살펴본 결과 이 해역전반에 걸쳐 공통된 계절변화가 보였다. 고온고염의 해수는 겨울에 황해 쪽으로 확장되며 여름에 동지나해 쪽으로 후퇴한다. 순압모델결과는 계절풍이 이와 같은 해수분포의 계절변화를 유도할 수 있음을 보여준다. 역풍류는 이 과정에서 중요한 역할을 하는데, 모델결과에는 역풍류의 축이 중국 쪽으로 이동되어 나타난다. 역풍류 축의 이동은 황해북부의 복잡한 해안선과 얕은 해저지형에 의한 에너지손실에 기인한다. 수치모델결과에 나타난 이동된 역풍류의 길은 여름철 황해저층냉수 남하의 길과 잘 일치한다.

• 대한원격탐사학회지
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• 제37권5_2호
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• pp.1307-1315
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• 2021

매년 여름철 양자강에서 유출되는 저염분수는 동중국해 뿐만 아니라 제주도 주변 해역의 염분 변화에 큰 영향을 미치며 때때로 그 영향은 한반도 연안에 국한되지 않고 대한해협을 통과하여 동해 외해 까지 확장되기도 한다. 한반도 주변으로 확장된 양자강 유출수는 해양 물리 및 생태학적으로 많은 영향을 끼치며 어업 및 양식업에 큰 피해를 유발하기도 한다. 그러나 현장조사의 한계점 때문에 동중국해에서 확산되는 저염분수를 지속적으로 관측하기에는 현실적으로 어려움이 있다. 이러한 이유로 양자강 유출수의 확산을 실시간으로 모니터링하기 위해 인공위성을 활용한 표층 염분 산출 연구가 많이 진행되어 왔다. 본 연구에서는 시간 및 공간 해상도가 상대적으로 좋은 GOCI(Geostationary Ocean Color Imager)를 활용한 동중국해 표층 염분 산출 알고리즘을 개발하였다. 알고리즘 개발을 위해 기계학습 기법 중 하나인 MPNN(Multilayer Perceptron Neural Network)을 이용하였으며, 출력층에는 SMAP(Soil Moisture Active Passive) 위성의 표층 염분 자료를 활용하였다. 이전 연구에서 2016년 자료를 이용한 표층 염분 산출 알고리즘이 개발되었으나 본 연구에서는 연구 기간을 2015년 부터 2020년까지로 확장하여 알고리즘 성능을 개선하였다. 2011년부터 2019년까지 동중국해에서 관측된 국립수산과학원의 정선조사자료를 이용하여 알고리즘 성능을 검증한 결과로 R²는 0.61과 RMSE는 1.08 psu로 나타났다. 본 연구는 GOCI를 이용한 동중국해 표층 염분 모니터링 알고리즘 개발을 위해 수행되었으며, 향후 GOCI-II의 표층 염분 산출 알고리즘 개발에 많은 기여를 할 것으로 기대된다.

• 한국항해항만학회:학술대회논문집
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• 한국항해항만학회 2000년도 Proceeding of CIN-KIN Joint Symposium 2000 on M.E.T. Under STCW 78/95 and SINO-KOREA MARITIME CONTACT IN MID-CENTURIES
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• pp.171-183
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• 2000

Regarding the ancient Sino-Kroea sea communication as the main theme, the propagation of the China-culture in Koran Peninsula and he influence of Chinese ancient shipbuilding technique for Korea are described in the paper. Frequent sea trade resulted in the flourishing of Chinese and Korean harbours on both side of Yellow Sea. Sino-Koran sea communication is of long-standing. Korean Peninsula (KP) is just as the large arm extended to the great sea from the North-east China. It is the Chinese mainland plate-lump's extended part in the Yellow Sea. In the ancient time, the land communication between China and Korea was often not unimpeded, the contact between China and KP, such as the South-Korea, depended on the sea communication mainly, Although the friendly relationship between China and Korea rose one after another in the various historical period, but considering from the great background of people's historical development, just as the modern people benefited fro the Europe-American culture, the people of ancient time also benefited from the China-culture. All China, KP and Japan obtained the development by propagating the ancient China-culture. The seagoing ships which carried out the Sino-Korea sea communication and trade, as the friendly envoys, finished the mission linked u and developed the Sino-Korea culture contact.

• 수산경영론집
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• 제40권2호
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• pp.71-103
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• 2009

This study is designed to propose the ways of the multilateral cooperation system for effective management of fisheries resources in the various overlapping zones established by bilateral fisheries agreements between Korea, China and Japan in North East Asia as semi-enclosed sea. It is necessary to build multilateral fisheries cooperation between Korea, China and Japan in North East Asia because conservation & management of transboundary fish stocks could not be guaranted effectively by the management of fisheries resources in the area where piled up the current-fishing-pattern zone, as white zone and the various grey zone as middle zone, and the interim measures zone of bilateral fisheries agreements between Korea, China and Japan are piled up. Fisheries management in Korea, China and Japan by the bilateral fisheries agreements in North East Asia is faced with difficulties manage fisheries resources. International relationship on fisheries is maintained by bilateral fisheries agreements based on UNCLOS. However fisheries resources are over-exploited and the recovery of the fisheries resources is very slow because proper conservation and management of transboundary fish stocks which article 63(1) of UNCLOS defines have not prepared yet. Thus close cooperation among the coastal States for a proper conservation and management of transboundary fish stocks is necessary. Since the transboundary fish migrate within the EEZs of two or more coastal States, there is a need to manage the fish stocks in the region between Korea, China and Japan through a multi-lateral mechanism at ccircumference area of the current-fishing-pattern zone as white zone. Coastal States must guarantee sustainable maintenance of transboundary fish stocks through the regional cooperation for a proper conservation & management because one coastal State alone could not guarantee conservation and management of fish stocks. Thus there is a need to build multilateral fisheries cooperation between Korea, China and Japan in North East Asia. There are many successful instances including the Barents' sea for a proper conservation & management of transboundary fish stocks. The Barents' sea is one of the best research object to study the regional cooperation for a conservation & management of transboundary fish stocks in North East Asia. In conclusion, it is necessary to build a multilateral fisheries cooperation system between Korea, China and Japan in North East Asia to conserve and manage transboundary fish stocks effectively. It seems desirable that the range of the area to conserve and manage fish stocks should may be any partial area in the current-fishing-pattern zone and interim measures zone between Korea and China, Jeju middle zone between Korea and Japan, interim measures zone of bilateral fisheries agreements between China and Japan.

• 수산해양교육연구
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• 제23권4호
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• pp.772-778
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• 2011

In order to estimate the densities and composition of floating marine debris (FMD), a sighting survey was conducted from July 1st to July 14th, 2009 in the East China Sea (ECS) using a training vessel "Kaya (1,737 ton)" of Pukyong National University. The sampled zones are divided into 5 transects by observation day during the survey days and the densities and composition in each transect were calculated using the numbers of item per $km^2$. The results of distribution of FMD are as follows: 1. During the surveys, a large variety of FMD was discovered and highest densities were found in the Central East(CE) of the East China Sea(ECS) (48.2 items/$km^2$), whereas densities in the less populated transects in Okinawa(OK1, OK2) were comparatively low(3.5 ~ 4.9 items//$km^2$). 2. Among the classified 6 items, styrofoams(Styro) were most abundant and ubiquitous(10.3 items/$km^2$, 53% of the total number), except OK2 area. Next abundant item was vinyl and plastics called V & P(4.9 items/$km^2$, 25%). Above 2 items of the major proportion of FMD accounted for 78% of the total number of FMD observed through this study. 3. The percentages of manufactured plastics(Styro and V & P) found in the Seas near Korean Peninsula were varied from 87.2% to 69.8%. It was recognized that polluted level is middle value among them.

• 한국방재학회:학술대회논문집
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• 한국방재학회 2007년도 정기총회 및 학술발표대회
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• pp.327-331
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• 2007

23 tropical cyclones of tropical storm(TS) intensity or higher formed in the western North Pacific and the South China Sea in 2006. The total number is less than the 30-year $(1971{\sim}2000)$ average frequency of 26.7, Out of 23, 15 cyclones reached typhoon(TY) intensity, three severe tropical storm(STS) intensity, and five TS intensity. The tropical cyclone season in 2006 began in May with the formation of CHANCHU(0601). While convective activity was slightly inactive around the Philippines from late June to early August. In addition, subtropical high was more enhanced than normal over the south of Japan from May to early August. Consequently, most tropical cyclones formed over the sea east of the Philippines after late June, and many of them moved westwards to China. CHANCHU(0601), BILIS(0604), KAEMI(0605), PRAPIROON(0606) and SAOMI(0608) brought damage to China, the Philippines, and Vietnam. On the other hand, EWINIAR(0603) moved northwards and hit the Republic of Korea, causing damage to the country From late August to early September, convective activity was temporarily inactive over the sea east of the Philippines. However, it turned active again after late September. Subtropical high was weak over the south of Japan after late August. Therefore, most tropical cyclones formed over the sea east of the Philippines and moved northwards. WUKONG(0610) and SHANSHAN(0613) hit Japan to bring damage to the country. On the other hand, XANGSANE(0615) and CIMARON(0619) moved westwards in the South China Sea, causing damage to the Philippines, Thailand, and Vietnam. In addition, IOKE(0612) was the first namded cyclone formed in the central North Pacific and moved westwards across longitude 180 degrees east after HUKO(0224).

• Ocean and Polar Research
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• 제33권2호
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• pp.135-147
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• 2011

Zooplankton is an important constituent in assessing ecosystem responses to global warming. The northern East China Sea is an important ecosystem for carbon cycling with a net sink of carbon dioxide. Despite their importance as a major component in carbon cycling, relatively little is known about zooplankton biomass structure and its regulating factors in the northern East China Sea. This study examined zooplankton biomass distribution pattern in the region from multiple cruises encompassing various seasons between 2004 and 2009. Results showed that zooplankton biomass exhibits less cross-shelf gradient in general with declining biomass to the eastern shelf towards the Tsushima Current Water. Size-fractionated biomass showed that the 1.0~2.0 mm size group, mostly copepods, dominated zooplankton biomass, comprising 38 to 48% of total biomass. Smaller zooplankton (0.2~1.0 mm) biomass, consisting mainly of Paracalanus spp, a particle eating herbivorous copepod, was positively related to chlorophyll-a concentration, but no relationship was established for larger zooplankton (1.0~5.0 mm). Spatially-averaged mean total zooplankton biomass was also highly related to chlorophyll-a concentration. These result suggest that the long-term trend of zooplankton biomass increase in this region is partly accounted for by the increases of phytoplankton biomass and productivity underway in the region. However, the underlying mechanisms of how sea surface warming in the study area leads to increased phytoplankton biomass and productivity remains unclear.

• 환경생물
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• 제22권1호
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• pp.192-199
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• 2004

2002년 가을에 제주도를 중심으로한 동중국해 18개 정점에서 그랩으로 채니한 표층 퇴적물 속의 와편모조류시스트 분포 특성을 조사하였다 현미경 잔찰시 해상력을 좋게 하기 위하여 퇴적물을 HCl과 HF로 처리하여 그 속의 시스트를 관찰하였다 총 13속 21종의 와편모조류시스트가 출현하였는데, Spiniferites bulloideus가 우점종을 차지하고 있었다. 임의로 나눈 제주도 북부 해역인 Part 1정점들에서의 평균 시스트 농도(1,144 cysts $g^{-1}$)가 그 남쪽 해역인 Part 2 (183 cysts $g^{-1}$)에서 보다 6배 이상 높은 값을 나타내고 있었다. 본 연구 결과는 이제까지 동중국해의 본 조사 정점 부근 해역에서 실시된 와편모조류 시스트 분포 조사 결과들과 비슷한 분포 경향을 보이고 있었다.

• 한국정보통신학회:학술대회논문집
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• 한국해양정보통신학회 2001년도 추계종합학술대회
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• pp.290-294
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• 2001

Satellite data, with Sea Surface Temperature(SST) by NOAA and Sea Level(SL) by Topex/poseidon, are used to estimate characteristics on the variations and correlations of SST and SL in the East Asian Seas from January 1993 through May 1998. In the oceanic climate, the variations of SL shown the high values in the main current of Kuroshio and the variations of SST shown not the remarkable seasonal variations because of the continuos compensation of warm current by Kuroshio. In the continental climate, SL shown high variations in the estuaries(the Yellow River, the Yangtze River) with the mixing the fresh water in the mouth of estuaries of the saline water in the coasts of continent and SST shown highly the seasonal variations due to the climatic effect of continents. In the steric variations in summer, the eastern sea of Japan, the East China Sea and the western sea of Korea shown the increment of sea level with 10~20cm. But the Bohai bay in China shown relatively the high values of 20~30cm due to the continental climate. Generally the trends of SST and SL increased during all periods. That is say, the slopes of SST and SL presented 0.29$^{\circ}C$/year and 0.84cm/year, respectively. The annual and semi-annual amplitudes shown a remarkable variations in the western sea of Korea and the eastern sea of Japan.

• Fisheries and Aquatic Sciences
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• 제3권1호
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• pp.8-13
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• 2000

Monthly mean chlorophyll concentration in the East Sea was estimated from the ocean color observed by the Coastal Zone Color Scanner (CZCS) on Nimbus-7 satellite which had performed various remote sensing missions from 1979 to 1986. The areas of high chlorophyll concentration were found in the sea between Siberia coast and Sakhalin Island, in the Donghan Bay and in the Ulleung Basin. In the southwestern East Sea, especially in the area near Ulleung Island, the yearly maximum chlorophyll concentration occurred in December. The chlorophyll concentration in Ulleung Basin in December was about two times higher than during spring bloom in April. The early winter bloom occurred in the warm side of the front that was formed between warm water from the East China Sea and nutrition rich cold water from the northern East Sea.