• 베이커리
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• no.7 s.372
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• pp.74-75
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• 1999

• Proceedings of the Korea Water Resources Association Conference
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• 2004.05b
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• pp.468-473
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• 2004

본 연구에서는 기존의 ㅡ자형, ㄴ자형, ㄷ자형 조파시스템이 경사진 방향으로 가동될 때 발생되는 에너지의 불연속성으로 인한 회절철상이나 구조물에서 반사된 파가 조파판에서 발생하는 재 반사 철상의 단점을 보완할 수 있도록 곡선형태의 조파판을 배치하여 수치실험을 행하였다. 조파판을 곡선형으로 배치시켜 실험 대상물에서부터 반사된 파가 가능한 조파판에 직각으로 부딪치도록 유도하였다. 편미분 격자생성기법을 도입하여 구성된 곡선형 격자망에서 Copeland(1985)의 완경사 방정식을 이용하여 수치해석 하였다. 우선, 1차원 실험영역에서 파를 생성하여 대상구조물에서 반사되어 돌아온 반사파 성분을 조파판에서 흡수하면서 입사파를 생성하는 현상을 재현하였다. 그 후, 실험영역을 2차원으로 확장시켜 조파판을 곡선형으로 배치하여 수치 실험하여 진행파와 회절파의 중첩으로 고안된 해석해와 수치 해를 비교하려다. 그 결과, 기존의 조파시스템에 비하여 에너지 불연속선에서의 회절 현상도 발생하지 않고 반사파 성분을 효율적으로 흡수하는데 효과적임을 알아냈다.

• Korean Journal of Fisheries and Aquatic Sciences
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• v.31 no.5
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• pp.695-706
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• 1998

SST (Sea Surface. Temperature) fronts which were found in the South-West Sea of Korea and the northern area of the East China Sea were examined in order to clarify their positions, shapes, seasonal changes and the formation mechanism, For this study used SST data rearranged from the SST IR image during 1991 to 1996 and oceanographical data obtained by National Fisheries Research and Development Institute. Temperature front in the Cheju Strait was analyzed by the data obtained from a fisheries guidance ship of Cheju Provincial Government, The coastal frontal zone in the South-West Sea of Korea and the offshore frontal zone in the northern area of the East China Sea can be divided into several types (Type of Winter, Summer, Spring, Autumn and late Autumn), Short term variations of SST fronts have a tendency not to move to any Bleat extent for several days. The location of the frontal zone in the southwestern sea of Cheju Island changes on a much large scale than that of the one in the southern coast of Korea, The frontal Tone, formed every year in the southern sea of Korea approaches closer to the coastal area in winter, and moves closer to the south in spring and autumn. The frontal zone of the southwestern sea of Cheju Island moves in a westerly direction from the east, and reaches its most westerly point in the winter and its most easterly point in the summer related to the seasonal change of the Tsushima Current. Additionally, the frontal zone of the southwestern sea of Korea becomes extremely weak in March, April and November. SST fronts are formed every year around the line connecting Cheju Island to Yeoseo Island or to Chungsan Island in the Cheju Strait. A Ring-shaped tidal mixing front appears along the coastal area of Cheju Island throughout the year except during the months from November to January. Especially, in May and October fronts are formed between the coastal waters of Cheju Island and the Tsushima currents connecting the frontal zone of the coastal region in the southern sea of Korea with that of the southwestern sea of Cheju Island.