• Proceedings of the Korea Committee for Ocean Resources and Engineering Conference
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• 2006.11a
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• pp.431-434
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• 2006

This study reviews the properties of coastal ocean and Seomjin River estuary spaces then define some MGIS(Marine Geographic Information System) related terminologies for clarifying the scope of MGIS boundaries. Therefore, we show the three-dimensional circulation of MGIS-based Seomjin River Estuary integrating three-dimensional POM model and observed data.

• Proceedings of the Korean Institute of Navigation and Port Research Conference
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• 2018.05a
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• pp.70-72
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• 2018

낙동강하굿둑 하구 하류역의 기존 연구결과를 살펴보면, 대부분 하천에 의한 영향을 중심으로 수행되었다. 그러나, 현재의 낙동강하굿둑 하구 하류역은 기존 연구결과와는 달리 외해쪽의 외력 영향을 받는 양상을 보이고 있다. 따라서, 금회 연구에서는 이러한 현재의 양상을 위주로 수치모델링을 수행하여 주변 해역의 매립에 따른 유속저하에 따른 퇴적우세 현상을 설명하려 한다. 또한, 부산항 신항 건설로 인한 영향이 현재의 퇴적양상에 어떤 기여를 하고 있는지를 시간적으로 역추산하였다. 이러한 현상 재현을 위하여 5개분조를 고려한 해수유동 실험을 수행하고 이에 더하여 외해파랑 영향을 추가하여 실제 현상을 재현하였다. 연구결과, 낙동강하굿둑 하구 하류역 지형변화에 주된 영향을 주는 외력조건은 파랑 인 것으로 파악되었으며, 이에 상세한 결과를 도출하기 위하여 상세조건을 추가한 실험을 수행할 계획이다.

• Journal of Korean Port Research
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• v.11 no.2
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• pp.241-255
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• 1997

Three dimensional numerical model is used to simulate the circulation patterns in the Gamcheon Bay located in Pusan, Korea and compared with the observed data. The model is forced by winds, tidal elevation at open boundaries, and warm water discharged from the outfall of power plant, Turbulence mixing coefficients are calculated according to a ${\kippa}-{\varepsilon}$ turbulence closure submodel. Temperature, salinty and current are measuted extensively and these measuted data are compared with the simulation results. Eddy-like features exist both in observed data dna simulation results. These eddies are the results of interaction with the weak tidal current, wind driven current and warm water discharges. Compensational deeects are also found to exit such that while surface current is strong, bottom current tends to weaken and vice versa.

• 대한방사선방어학회:학술대회논문집
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• 2011.04a
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• pp.176-177
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• 2011

• Proceedings of the Korean Society of Marine Engineers Conference
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• 2005.06a
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• pp.764-771
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• 2005

• Proceedings of the Korean Radioactive Waste Society Conference
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• 2006.11a
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• pp.377-378
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• 2006

• 한국해양학회지
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• v.9 no.2
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• pp.19-30
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• 1974

Current observations were carried out in Jinhae Bay area during the period of January to February 1974. The data were synthetically analyzed and the characteristics of the water movement in Jinhae Bay were studied. The water movement in Jinhae Bay area is a reversing tidal current type and the Semi- diurnal tidal current is predominant. The ebb current begins at about high water time and the strongest current occurs at about 3 hour after high water. The flood current begins at 0.2-1.0 hour before low water and the strongest current occurs at about 3-4 hour after low water. The main ebb current flows to SE direction with the maximum welocity, about 100cm/sec and the lood flows to NW with the maximum velocity, about 70cm/sec. Generally, the ebb current in Jinhae Bay is more predominat than the flood current except at the west and the north coast area of Gadeog-do where the flood current is more predominant.

• Journal of the Korean Society of Marine Environment & Safety
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• v.18 no.1
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• pp.25-32
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• 2012

To arrange effectively artificial reefs for marine afforestation, tidal currents were analyzed by numerical experiments. The numerical experiments were carried out by EFDC(Environmental Fluid Dynamics Code), and water column was vertically divided 5 layers. Tidal current patterns showed to be affected by main current at outside of study area, and circle currents of two were observed from analysis of residual currents. The calculated harmonic constants of tide and tidal current agreed well with those of observations at two stations for tide and two stations for tidal current. The model successfully reproduced the tidal current around the Geomoondo marine afforestation. It suggest that artificial reefs for marine afforestation should be installed belt zone at study area.

• Proceedings of KOSOMES biannual meeting
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• 2009.06a
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• pp.89-94
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• 2009

This study aims to examine the the characteristics if the sea water circulation in related to the change of the water exchange rate according to the the development phases of Busan Port. To clarify the characteristics, the water exchange caused by construction if new-port and river discharge conditions was examined by the numerical experiments using the Lagrangian particle tracking model based on 2-D shallow water equation. This study deals with the charge of flow field and water exchange after redevelopment using numerical simulation technique, based on the field observation and 4 rivers discharge flow. As a result if numerical simulation, Variation if current velocity in Busan North Port is almost nothing before and after construction. Water exchange of channel in area of redevelopment is a little. Futhermore, the tidal exchange had a tendency to be small both before and after redevelopment by 60%.

• Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
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• 1993.07a
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• pp.166-174
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• 1993

본 연구에서는 자유수면과 성층효과를 고려한 3차원 연안해수유동 수치모형을 개발하였다. 수치모형은 수심방향에 대해서 정규화된 좌표(c-coordinate)를 사용하며, 시간적분방법으로는 반음해법(semi-implicit)을 사용하여 계산시간의 효율성을 도모하였으며, 모드분리개념을 도입하여 내역항(Internal mode)에 대해서는 양해법을 사용하였으며, 외역항(External mode)은 수평방향 운동방정식과 연속방정식의 차분식으로부터 얻은 Poisson형태의 타도형 차분방정식을 Point-SOR법에 의하여 해석하였다. (중략)