• 한국해안해양공학회:학술대회논문집
• /
• 한국해안해양공학회 2002년도 한국해안해양공학발표논문집 Proceedings of Coastal and Ocean Engineering in Korea
• /
• pp.191-197
• /
• 2002

The prediction of the dynamic behaviors of buoyant water discharges into a large volume of water bodies, the flows of water accompanying the density differences due to temperature differences and sometimes also to salinity differences, have attracted great concern over several decades. Heated water surface discharges from power plants and freshwater discharges in estuaries are typical examples of the buoyant flows. (omitted)

• International Journal of Ocean Engineering and Technology Speciallssue:Selected Papers
• /
• 제6권1호
• /
• pp.15-21
• /
• 2003

A common feature in the three-dimensional numerical model experiments of coastal discharge with simplified model and idealized external forcings is investigated. The velocity fields due to the buoyancy and flaw flux, are spreaded radiately and the surface velocites are much greater than the homegeneous discharges. The coastal dischargd due to the Coriolis force and flaw flux are shaped a anticyclical gyre (clockwise) and determined the scale of the gyre in the coastal zone, respectively. The bottom topography restricts a outward extention of the coastal fronts and it accelerates a southward flow.

• 한국해양공학회지
• /
• 제20권4호
• /
• pp.50-57
• /
• 2006

The effect of discharges from the Seomjin River on the dispersion of thermal effluent from the Hadong Power Plant, located along the south coast of Korea, was investigatedusing intensive field observation and three-dimensinal Princeton Ocean Model simulations. A POM and observed CTD data was used to predict the mixing behaviour of the Summer freshet, during the July 2005 intensive observing period. The dispersal of the river discharge anomaly, associated with the Seomjin River plume, was seen to be highly responsive to tidal currents and river flows during the spring tide.

• Ocean and Polar Research
• /
• 제22권1호
• /
• pp.45-56
• /
• 2000

Hydrodynamic mixing characteristics of submerged effluent discharges into Masan Bay were investigated by both field observations and numerical model simulations. CORMIX model, a length-scale mixing model, was adopted to obtain the near-field dilution and wastefield characteristics of the effluent discharges into Masan Bay. Model predictions of the near-field dilution rates were in a good agreement with field observations in summer and winter seasons. Seasonal variations in the dilution rates showed that the highest dilution rate was obtained in winter while the lowest dilution rate was in summer. As the effluent discharges are increased with the treatment capacity expansion to be completed by 2011, the dilution rates are expected to be much reduced and the near-field stability of the wastefields will become unstable due to the increased effluent discharges.

• 한국해양공학회지
• /
• 제17권2호
• /
• pp.1-7
• /
• 2003

A common feature in the three-dimensional numerical model experiments of coastal discharge with simplifed model and idealized external forcings is investigated. The velocity fields due to the buoyancy and flow flux, are spreaded radiately and the surface velocites are much greater than homegeneous discharges. The coastal dischargd due to the Coriolis force and flow flux are shaped a anticyclical gyre (clockwise) and determined the scale of the gyre in the coastal zone, respectively. The bottom topography restricts a outward extention of the coastal fronts and it accelerates a southward flow.

• 한국항해항만학회:학술대회논문집
• /
• 한국항해항만학회 1999년도 추계학술대회논문집
• /
• pp.243-252
• /
• 1999

Recently several research groups using CORMIX, approved by EPA, have been working on the hydrodynamic mixing processes due to the ocean discharges. It provides a useful tool for analyzing near field mixing characteristics through the outfall system. This paper applies CORMIX 1 & 2 to the Pusan Jungang Effluent Outfall System, which is planned to be in the Gamchun harbour and will be completed in 2011. This model output shows the trajectoral variation of dilution and concentration for three cases of outfall system. Dilution differences have been simulated and found the highest dilution condition under the different displacement of outfall system. On the basis of these outputs it will be proposed the optimum outfall system type and location. This approach might contribute on protecting the serious water quality problem due to the ocean discharge.

• International Journal of Naval Architecture and Ocean Engineering
• /
• 제10권5호
• /
• pp.651-659
• /
• 2018

A multi-level overtopping wave energy converter was designed according to the large tidal range and small wave heights in China. It consists of two reservoirs with sloping walls at different levels. The reservoirs share a common outflow duct and a low-head axial turbine. The experimental study was carried out in a laboratory wave-flume to investigate the overtopping performance of the device. The depth-gauges were used to measure the variation of the water level in the reservoirs. The data was processed to derive the time-averaged overtopping discharges. It was found that the lower reservoir can store wave waters at the low water level and break the waves which try to climb up to the upper reservoir. The upper sloping angle and the opening width of the lower reservoir both have significant effects on the overtopping discharges, which can provide more information to the design and optimization of this type of device.

• 한국해양환경ㆍ에너지학회지
• /
• 제11권3호
• /
• pp.164-174
• /
• 2008

섬진강 하구역을 중심으로 광양만과 여수해만에서의 동시 관측한 염분의 현장관측자료의 분석과 기상, 조석, 하천유출수 및 온배수를 고려한 3차원 수치모델(EFDC) 결과를 이용하여 섬진강 하구역의 3차원 혼합특성을 파악하였다. 수치모델에 고려된 입력조건은 수심, 기상, 하천유출수 및 온배수 등이며, 개방경계에서는 염분 및 조석을 고려하여 수치모의하였다. 수치모델 검증은 조위 2개 정점과 조류 2개 정점의 조화분석을 통한조화상수 비교를 통하며 모델결과가 관측결과와 잘 일치하고 있음을 확인하였고, 조시별 유동장을 잘 재현하고 있음을 확인하였다. 동계 및 하계시 월평균 하천유출수를 고려하여 수치모의한 결과, 동계에는 32.0 psu의 등염분선이 섬진강 하구에 국한되어지나, 하계에는 30.0psu의 등염분선이 하천유출량의 영향으로 섬진강 하구역으로 확장되어짐을 확인할 수 있었다. 한편, 섬진강 하구역의 3차원 혼합특성은 전반적으로 섬진강 유출량의 변동, 해수유동구조 및 온배수 등에 의해 복잡한 형태를 보이는 것을 확인할 수 있었다.

• 한국해안해양공학회지
• /
• 제16권4
• /
• pp.213-223
• /
• 2004

마산만 연안유역의 지하수 유출량을 Darcy 방법을 이용하여 추정하였다. 지하수위, 관정의 위치, 투수계수, 대수층 두께, 해안선 길이 정보를 이용하여 추정한 지하수 유출량은 강우량 대비 1.65%정도이다. 마산만 유역의 암반층을 통한 지하수 유출량은 $0.7\times10^4$ $m^2/year$정도로 추정되었으며, 충적층을 통한 지하수 유출량은 $1.0\times10^7$$m^3/year$정도로 추정되어 암반층을 통한 유출량은 무시할 만한 정도로 파악되었다. 한편, 한국해양연구원(2003)에서 방사성 동위원소를 이용하여 추정한 지하수 유출량은 본 연구에서 추정한 지하수 유출량의 20배 정도에 해당하지만, 이는 연안 대수층으로 침입한 재순환 해수의 영향으로 파악되었으며, 해안선에 근접한 관측정의 운영을 통하여 지하수위 및 염도 변화를 지속적으로 관측하여 재순환해수의 정량적인 영향분석을 보다 상세하게 연구할 필요가 있는 것으로 판단된다.

• 한국제4기학회:학술대회논문집
• /
• 한국제4기학회 2004년도 추계학술대회
• /
• pp.37-43
• /
• 2004

The response of the CCCma coupled climate model to the imposition of LGM conditions is investigated. The global mean SAT and SST decrease by about $10^{\circ}C$ and $5.6^{\circ}C$ in the coupled model. Tropical SST decreases by $6.5^{\circ}C$, whereas CLIMAP reconstructions suggest that the tropics cool by only about $1.7^{\circ}C$, although the larger tropical cooling is consistent with the more recent proxy estimates. With the incorporation of a full ocean component, the coupled model gives a realistic spatial SST pattern, capturing features associated with ocean dynamics that are seen in the CLIMAP reconstructions. The larger decrease of the surface temperature in the model is associated with a reduction in global precipitation rate (about 15%). The tropical Pacific warm pool retreats to the west and a mean La $Ni\tilde{n}a$-like response is simulated with less precipitation over the central Pacific and more in the western tropical Pacific. The more arid ocean climate in the LGM results in an increase in SSS almost everywhere. This is particularly the case in the Arctic Ocean where large SSS increase is due to a decrease in river discharge to the Arctic Ocean associated with the accumulation of snow over the ice sheet, but in the North Atlantic by contrast SSS decreases markedly. This remarkable reduction of SSS in the North Atlantic is attributed to an increase in fresh water supply by an increase in discharges from the Mississippi and Amazon rivers and an increase in P-E over the North Atlantic ocean itself. The discharges increase in association with the wetter LGM climate south of the Laurentide ice sheet and in South America. The fresh water capping of the northern North Atlantic results in a marked reduction of deep convection and consequently a marked weakening of the North Atlantic overturning circulation. In the LGM, the maximum overturning stream function associated with the NADW formation decreases by about 60% relative to the control run, while in the Southern Ocean, oceanic convection is stronger in the LGM due to reduced stratification associated with an increase in SSS and a decrease in SST and the overturning stream function associated with the formation of AABW and the outflow increases substantially.