• Proceedings of the Korean Institute of Navigation and Port Research Conference
• /
• 2006.06b
• /
• pp.185-190
• /
• 2006

Damages such as beach erosion, seawall destruction and difficulty of cargo working due to rolling of ship result from shipwave. In addition, high speed operations of motor boat and passenger ship respectively jeopardize sea bathers and anglers' safety. In general, shipwaves in shallow water have worse effect on coastal facilities and working people there than those in deepwater. This study aims to investigate the characteristics of shipwaves which occurred and propagated in shallowwater experimentally and theoretically.

• Korean Journal of Ichthyology
• /
• v.8 no.1
• /
• pp.9-13
• /
• 1996

To study on the growth of young stage Acanthopagrus schlegelii, samples were collected from the shallow waters off Kunsan, Korea from July to December, 1995. The planctonic larvae of Acanthopagrus schlegelii were collected in early June. The young fish of 12.7~26.6 mm in total length began to appear in the shallow water in late June. They grew up 19.9~51.4 mm in middle July, 24.8~75.0 mm in late July, 63.3~79.6mm in middle August. A. schlegelii disappear from the shallow water after middle August, and began to be collected in the outer bay off Kokunsan Isls. by long back net. This species that had spawned from Kunsan coast in late June to middle August grew up to 100mm in total length in December of that year.

• Journal of Korean Society of Coastal and Ocean Engineers
• /
• v.20 no.2
• /
• pp.148-156
• /
• 2008

WAM(WAve Model), deep water wave model has been extended to the region of shallow water, incorporating wave breaking, and triad wave interaction. To verify this model, two numerical simulations for hydraulic experiments of Chawla et al.(1998) and Beji and Battjes(1993) are performed. The computed results show good agreements with measured ones. To identify its applicability to real sea, it is applied to storm wave modelling for typhoon Maemi. Numerical results compared with measured ones at Geoje, Busan and Ulsan show reasonable wave height estimations.

• Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
• /
• 1996.10a
• /
• pp.38-41
• /
• 1996

심해에서 풍파의 형성은 주로 바람에 의한 마찰력과 파와 파간의 상호간섭 그리고 white capping 현상등에 의한 1차 에너지 손실에 의하여 이루어지며, 파의 변이는 주로 이상의 세 가지 물리현상에 좌우된다. 이러한 심해역에서의 파의 변이를 해석할 때 굴절, 회절 및 마찰손실 등에 의한 천해역 현상은 무시할 수 있으며 풍파의 형성은 주로 바람 조건에 좌우된다. 그러나 파도가 일단 심해역에서 천해역으로 들어오게 되면, 천수, 굴절, 회절 및 마찰손실 등에 의하여 급격하게 변이한다. (중략)

• Journal of Korean Society of Coastal and Ocean Engineers
• /
• v.27 no.5
• /
• pp.364-371
• /
• 2015

This study is aimed to develop the dynamic analysis technique for a floating aquaculture in a shallow water region under the harsh sea condition. In case of the installation region to transform from a coastal area to the offshore area, the influence of sea bed with sea waves on the mooring lines was announced to be significant by other authors. In this study, the numerical tool was developed to solve dynamic behavior of the floating barge coupled with mooring lines in a shallow zone of the sea considering the influence of sea bed on the floating system.

• Proceedings of the Korea Committee for Ocean Resources and Engineering Conference
• /
• 2004.11a
• /
• pp.149-153
• /
• 2004

본 연구에서는 태풍의 천애역 내습시 태풍의 풍역이동과 위험반경내의 풍향 풍속 변화를 해안지형의 특성에 따라 파랑이 충분히 발달할 수 있는 해역을 대상으로 발생가능한 풍향별 취송거리 및 관측된 풍향 풍속으로 천해설계파를 산정하기 위한 한가지 수치해석기법을 소개한다. 이를 통해 구조물 전면에서의 파고계산을 위해서는 구역을 결정할 때 해역의 개방 정도 및 폐쇄성과 태풍중심 이동경로가 천해설계파 산정시 중요함을 강조 할 수 있다. 실시간 해석기법에 대해서 부가적인 재해석 절차가 필요한 상황이지만 본 연구의 해석기법은 연안 해안지역의 천해설계파를 추정함에 있어 태풍의 천해역 통과시 풍역의 변화특성과 이를 고려한 파랑의 불획 정성을 극복하고 보완 할 수 있는 천해설계파 산정을 위한 기초적 연구로서 활용될 수 있을 것이라 판단된다.

• Journal of Korean Society of Coastal and Ocean Engineers
• /
• v.19 no.6
• /
• pp.511-520
• /
• 2007

WAM(WAve Model), deep water wave model has been extended to the region of shallow water, incorporating wave breaking, and triad wave interaction. To verify the model, numerical simulation of waves in Youngil bay, Pohang is performed and the simulated results show good agreements with measured wave data sets, one station at the mouth of bay and two stations inside the bay. As waves propagate toward the shore, wave height gradually diminishes by bottom friction and wave breaking, and wave direction, initially NE changes normal to the shore due to depth refraction.

• Journal of Korean Port Research
• /
• v.14 no.1
• /
• pp.97-105
• /
• 2000

This paper presents an automatic mesh generation considering water depth, which is based on the depth interpolation. The key feature of this method is that the position of a mesh on any depth in the shallow water area can be generated. The Examples are carried out, and the results are shown to be good. This method is shown to be a useful and powerful tool for the flow calculation for the seabed topography.

• Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
• /
• 2002.08a
• /
• pp.35-41
• /
• 2002

천해역에서 관찰되는 장주기파는 발생 기구에 따라서 surf beat, setdown wave, locked wave, 또는 Far-infra-gravity wave 등으로 다양하게 불리 우며, 모두 0.5-수 분대의 주기를 갖는다. 이들은 정의에 따라 약간씩 다르기는 하지만 모두 계류된 선박의 동요뿐만 아니라 해안선 침식과도 밀접한 관련이 있다는 것이 일반적으로 인정되고있다(가등 등, 1989). (중략)

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