• Journal of the korean society of oceanography
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• 제34권3호
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• pp.133-143
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• 1999

We carried out simultaneous and long-time observations of currents across the western channel of the Korea Strait during the period of May, 1994 to September, 1996 in order to understand the spatial and temporal variability of tidal and nontidal currents in the Strait. Results show that currents in the Strait are quite variable in space and time, and they largely consist of mean current and diurnal and semidiurnal tidal currents of about equal magnitudes. The mean currents include the Tsushima Current and the Korea Strait Undercurrent at the center of the channel. The former occupies the upper two-thirds and the latter the lower one-third of the water column. The semidiurnal and diurnal currents are largely rectilinear in the direction of NE-SW and their amplitude variation across the channel appears to be small. However, the diurnal currents at some locations show rotational characteristics with significant nontidal effects. The station close to the Korean coast leads the phase and the phase difference of the semidiurnal current across the channel appears to be less than half an hour while that of the diurnal current is over five hours.

• 한국해양학회지
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• 제28권1호
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• pp.35-46
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• 1993

알라스카만 명태 산란장에서의 해수의 성질과 해류의 흐름을 규명하기 위하여, 쉘 리코프 해협에서의 CTD 조사 결과와 해류계 자료가 분석되었다. 쉘리코프해협에서는 3개의 수괴가 구분되었다. 첫 번째 수괴는 Cook 내만으로부터 유래된 적은 양의 차갑고 염분이 낮은 ($<{\;}3^{\circ}C,{\;}<{\;}31.5\textperthousand$) 표층수로서 알라스카 반도 해안에 바짝 붙어서 남서쪽을 향하여 흐르고 있다. 둘째의 수괴는 알라스카 해안류 (ACC)의 가지로서 해협의 북종쪽 입구로 들어와 남서쪽을 향해 흐르며, 해협내에서는 중층과 표층의 대부분을 차지하고 있다. 해협의 가장 깊은 골의 상부층에 가장 빠른 흐름이 존재하며, 그들은 Semidi섬과 Chirikof섬 사이의 남서쪽 계곡을 통하여 해협에서 빠져나간다. 세 번째의 수괴는 비교적 느리고, 따뜻하고 염분이 높은 ($>{\;}5^{circ}C,{\;}>{\;}32\textperthousand$) 대륙사면으로부터 남서쪽 입구의 저층을 통하여 해협으로 들어온 저층수인데 이들은 북동쪽을 향해 흐르며 해협 저층의 대부분을 차지한다.

• 한국수산과학회지
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• 제16권4호
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• pp.299-304
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• 1983

제주해협 동쪽 입구에는 주년 대마난류 수괴인 설상 난수가 존재한다. 그러므로 이 설상 난수 때문에 동 해협 서쪽에서 유입하는 해수의 유향이 이 해협내에서 변화되 한국 남해 연안쪽을 향할 수 있어 제주해협내의 중, 저층수는 한국 남해 연안수 형성에 중요한 영향을 미칠 수 있다. 이 설상 난수는 동계에 강하고 하계에 약하므로 대마난류는 하계 보다 동계에 한국 남해 연안에 접근하며, 이 난류의 북쪽 경계도 거문도와 소리도 연안까지 자주 접근하고 있다.

• 한국항해항만학회:학술대회논문집
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• 한국항해항만학회 2006년도 추계학술대회 논문집(제2권)
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• pp.13-17
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• 2006

Almost every day close passage or near miss events happens in south part of Istanbul Strait between the vessel runs in the local area and pass strait transit. The vessels run in the local area pass close bow or aft of transit vessel or come close and wait for transit vessel because of inexperienced or incompetent skipper or because of time limitation or failure in technical equipment or lack of technical equipment or old equipment. This close passages create profound dangers for the surroundings. By the this research has been aimed to point out mentioned dangers by the concrete as number. For this purpose has been utilized JMS Ship Handling Simulator which has been settled in ITU Maritime Faculty and Environmental Stress Model which has been built up and improved in Inoue Laboratory. Has been put in the senarios which been played during simulation implementations transferred to the numerical risk occured during passage of South Part of Istanbul Strait by the Environmental Stress Model . Thus so, the riskwhich Istanbul Strait face everyday has been expressed as numerical and concrete.

• 한국수산과학회지
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• 제30권6호
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• pp.1021-1032
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• 1997

Satellite-tracked drifters deployed in the East Sea since 1991 are used to study the Tsushima Current (TC). It is found that the TC is a steady current with a mean speed of 10 cm/s before it enters the East Sea. Only during the summer, the TC flows along Honshu Island with a mean speed of $30\~40\;cm/s$ and then exits through the Tsugaru Strait. In fall and winter, the TC does not follow the coast along Honshu Island but it enters into the interior of the East Sea before it reaches the Tsugaru Strait. The water that passes the West Channel of the Korea Strait mostly comes from the western East China Sea and spreads into the interior of the East Sea. It also forms the large eddies in the southern East Sea. The outflow through the Tsugaru Strait comes from the interior of the East Sea in all seasons except summer. The mean speed of the Tsugaru Strait outflow is about 60 cm/s. The largest current variability is found in the eastern central area of the East Sea, south of sub-polar front.

• 해양환경안전학회지
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• 제21권1호
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• pp.25-33
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• 2015

말라카해협의 해상교통 안전 확보는 우리나라를 비롯하여 중국, 일본을 포함한 극동아시아의 경제 발전에 직접적인 영향을 미치므로 세계적으로 중요한 해역이다. 이러한 의미에서 이 해역의 해상교통안전을 분석하는 것은 중요한 의미가 있다. 이 연구에서는 말라카해협을 대상으로 TOAIS 프로그램에 의한 선박 AIS 데이터를 1개월 동안 수집하였고, EasyFit 프로그램을 이용하여 해상교통의 통항분포를 통계적으로 분석하였다. 그 결과, 현재까지 해상교통공학 분야에서 선박통항의 분포는 정규분포라고 알려져 사용되고 있었지만, 말라카해협의 해상교통조사 결과 그 통항분포가 정규분포와 상이하다는 것을 확인하였다. 이러한 상이한 해상교통 분포 모델을 적용한 IWRAP모델을 이용하여 이 해역을 평가하였고, 그 결과 추월과 횡단상황이 가장 위험한 것으로 분석되었다. 또한 말라카해협의 충돌위험이 가장 높은 해역은 말라카해협과 포트클랑 해협 간 횡단지점으로 분석되었다.

• 수산해양기술연구
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• 제34권2호
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• pp.117-134
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• 1998

The study on the Assembling Mechanism of the Hairtail, Trichiurus lenpturus, at the Fishing Grounds of the Cheju Strait had been investigated by analyzing the relationship of the oceanographic conditions and the fishing ground of the Hairtail in the Cheju Strait. 1. The fishing grounds of the hairtail at the Cheju Strait are formed at the bottom of a high temperature of the tidal front at the coast. area of northern Cheju Island, the tip of the linguiform is high in salinity at the eastern and western entrances of Cheju Island, low salinity eddy on the surface and its surrounding front, various water masses in the Strait and coastal waters of the South Sea in Korea. 2. The fishing grounds of the Hairtail at the Cheju Strait begins with the sea surface temperature higher than $15^{\circ}C$ and the incoming of low salinity water now from the East China Sea. 3. Estimation of optimum temperature and salinity per season based upon analysis for relationship between temperature of water and salinity of the bottom layer and the catch is : 15.2~$16.4^{\circ}C$, 34.20~34.40${\textperthousand}$ in spring(June); 14.4~ $17.0^{\circ}C$, 33.70~34.30${\textperthousand}$ in summer(July~September); and 15.7~ $18.6^{\circ}C$, 33.70~34.50$\textperthousand$ in autumn(October~December). Hairtail are mostly caught at the Yellow Sea Warm Current and Tsushima Current with temperature over $14.5^{\circ}C$ and salinity over 33.70${\textperthousand}$ at the bottom layers of the Cheju Strait. 4. Considering the relationship between the amount of hairtail catch and the water temperature of bottom layer, when the bottom water being above $14.0^{\circ}C$ flowed into Cheju Strait through the western entrance of the strait in summer, the ca-h appears to have been abundant. In contrast, the catch has been poor when the temperature of such water was recorded to be below $13^{\circ}C$ Therefore, distribution patterns of water at the bottom layer can be used as a forecast index whether the catch of a certain year will be good or poor.

• 한국항해항만학회지
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• 제34권9호
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• pp.687-692
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• 2010

This study is to improve the marine traffic environment along the west coast of the Korean peninsular so as to prevent the traffic accidents of the dangerous cargo carriers. The most used routes of the vessels were investigated from GICOMS database and the questionnaire survey. Gwanjanghang Sudo strait and Maenggol Sudo strait were considered to have some potential risks to the vessels. In this study, the alternative routes were developed to substitute the current routes near Gwanjanghang Sudo strait and the new boundary line of The Traffic Prohibited Area for Tanker was suggested to contain the Maenggol Sudo strait.

• 한국항해학회지
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• 제8권1호
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• pp.49-70
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• 1984

Spatial and temporal variations of hydrography and currents are investigated in the Southeastern Sea of Korea during October 1982. The distribution of the water mass of high salinity (>34.40${\textperthousand}$) and low dissolved oxygen concentration (<5.0ml/l) indicates that the Tsushima current flows northward as it passes the Western Channel of the Korea Strait. The cold water (<$6.0^{\circ}c$) with low salinity (<$34.20{\textperthousand}$) and high dissolved oxygen concentration (>6.0ml/l) reaches the bottom of the western channel of the Korea Strait after flowing southward leaning against the slope rather than following the deepest part of the Channel. Repeated sections in the Korea Strait show a remarkable change of hydrographic structure over a period of 4 days ; both warn and cold waters are intensified, particularly in the eastern part of the strait toward the Tsushima Island.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume II
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• pp.943-945
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• 2006

The experiment on study of ambient nose generated by large-amplitude internal waves in Luzon Strait is analyzed. Simultaneous observations of internal waves and characteristics of ambient noise generated by them were carried out. Fast 50-m solitary internal wave propagated to the northwest direction with speed more than 3 m/s was observed. It was revealed an enhancing of ambient noise level (at frequency range 1-2 kHz) at a time of passing the face side of the solitary wave.