• 한국해안·해양공학회논문집
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• 제27권6호
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• pp.419-423
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• 2015

인공용승구조물은 흐름이 구조물에 의해 상승류와 배후면의 와류가 발생한다. 이때 저층수에 포함된 영양염이 표층으로 이동되고, 표층에선 플랑크톤 및 어류의 생태활동을 촉진시켜, 어업생산성을 향상시키는 역할을 한다. 본 연구에서는 CFD를 이용하여 성층 상태를 고려한 인공용승류의 변화에 대하여 연구하고자 하였으며, 그 결과, 용승효과는 인공용승구조물의 최상부에서 가까울수록 좋은 효과가 나타났으며, 성층상태를 고려하지 않은 경우, 저층에서 표층으로 향하는 상승류 특성만 나타났으나, 성층상태를 고려한 경우, 상승류와 하강류가 반복되는 흐름특성을 확인 할 수 있었다.

• 해양환경안전학회지
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• 제1권2호
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• pp.53-60
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• 1995

We measured lagrangian currents in the coastal regions off east coast of Korea. The experiment sites are the Ulijin region where Polar Front of the East Sea is formed and the Ulgi region where coastal upwelling occurs frequently in summer. Each drifters are equipped with GPS receiver, and their trajectories are montiored by receiving the data transmitted from drifters through radio signal. The experiment with 'transmitting' GPS is very useful in monitering flows in coastal regions. Trajectories of drifters in the Uljin Polar Front region in October 1994 showed counterclockwise flow pattern. The flow pattern agrees with the SST distributions obtained from NOAA-11 AVHRR image for the same period. The lagrangian trajectories of drifters at 5m and 15m depths in the Ulgi region for normal period of April 1995 showed that the currents at the top 15m layer are almost uniform and their magnitude is 29cm/s. However, the currents, measured by KORDI, during the upwelling period of June 1994 showed that the currents at 5m depth were 1.2 times stronger than those at 15m depth. The current pattern in the Ulgi upwelling region agrees with the horizontal and vertical distributions of seawater temperature measured by NFRDA at the same period.

• Ocean and Polar Research
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• 제34권2호
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• pp.111-123
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• 2012

To understand the phytoplankton community in the eastern part of the Yellow Sea (EYS), in the summer, field survey was conducted at 25 stations in June 2009, and water samples were analyzed using a epifluorescence microscopy, flow cytometry and HPLC method. The EYS could be divided into four areas by a cluster analysis, using phytoplankton group abundances: coastal mixing area, Anma-do area, transition water, and the central Yellow Sea. In the coastal mixing area, water column was well mixed vertically, and phytoplankton was dominated by diatoms, chrysophytes, dinoflagellates and nanoflagellates, showing high abundance ($>10^5\;cells\;l^{-1}$). In Anma-do coastal waters characterized by high dominance of dinoflagellates, high phytoplankton abundance and biomass separated from other coastal mixing area. The southeastern upwelling area was expanded from Jin-do to Heuksan-do, by a tidal mixing and coastal upwelling in the southern area of Manjae-do, and phytoplankton was dominated by benthic diatoms, nanoflagellates and Synechococcus group in this area. Phytoplankton abundance and biomass dominated by pico- and nanophytoplankton were low values in the transition waters and the central Yellow Sea. In the surface of the central Yellow Sea, high dominance of photosynthetic pigments, 19'-hexanoyloxyfucoxanthin and zeaxanthin implies that haptophytes and cyanobacteria could be the dominant group during the summer. These results indicate that the phytoplankton communities in the EYS were significantly affected by the formation of tidal front, thermal stratification, and coastal upwelling showing the differences of physical and chemical characteristics during the summer.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume I
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• pp.352-355
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• 2006

In this study, the seasonal and inter-annual variation of sea surface current in the Gulf of Thailand were revealed through the use of WOD temperature and salinity data and monthly sea surface dynamic heights (SSDH) from TOPEX/Poseidon and ERS-2 altimetry data during 1995-2001. The mean dynamic height and mean geostrohic current were derived from the climatological data while SSDH data gave monthly dynamic heights and their geopstrophic currents. The mean geostrophic current showed strong southward and westward flow of South China Sea water along the gulf entrance. Counterclockwise eddy in the inner gulf and the western side of the gulf entrance associated with upwelling in the area. Seasonal geostrophic currents show basin-wide counterclockwise circulation during the southwest monsoon season and clockwise circulation during the northeast monsoon season. Upwelling was enhanced during the southwest monsoon season. The circulation patterns varied seasonally and inter-annually probably due to the variation in wind regime. And finally we found that congregation, spawning, and migration routes of short-bodied mackerel conform well with coastal upwelling and surface circulation in the gulf.

• 한국해양학회지:바다
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• 제8권2호
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• pp.177-186
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• 2003

하계 진동만 저층수의 저산소화에 미치는 성층 및 바람의 효과를 고려한 수평 및연직 유동성분의 영향을 조사하여 내만역에서의 빈산소수괴 형성기구를 밝혔다. 진동만에서 수온, 염분, 용존산소 및 풍향, 풍속은 1998년 3월부터 1999년 2월 사이에 조사하였다 저층수에서 5 이하의 낮은 용존산소농도가 5월에서 9월에 걸쳐 존재하였으며, 표층수의 고온·저염화에 따라 강한 약층이 형성되어 연직기울기는 매우 크게 나타난 하계(7∼8월)에 3 이하의 극히 낮은 용존산소농도가 출현하였다. 이와 같은 저농도의 용존산소는 특히 만 안쪽 정점에서 춘계(5∼6월)에도 관찰되었다. 또한, 하계(8∼9월)에 5 이하의 낮은 용존산소농도를 가지는 저층수가 약 4∼6 m 수층까지 표층쪽으로 부상하는 특징적인 현상이 나타났다 여름철 진동만에서 바람의 효과를 고려한 잔차류의 연직성분을 살펴보면, 이 지역에서 우세한 북풍이나 서풍계열의 바람에 의해서 만 바깥쪽을 하강류역이, 만 안쪽은 상승류역이 발생한다. 또한, 하강류역인 만 바깥쪽에서 만 안쪽으로 향하는 저층류가 발달하였는데, 이것은 표층으로부터 침강된 유기물질의 만 안쪽으로의 유입을 초래할 수 있을 것으로 기대된다. 한편 말 안쪽에서 나타나는 상승류의 존재가 만 안쪽에서 형성된 저층의 빈산소수를 표층 근처까지 부상하게 하는 역할을 하는 것으로 보인다.

• 수산해양기술연구
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• 제44권3호
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• pp.207-217
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• 2008

Costal regions in Korea often suffer severe damages due to wave-induced disasters, storm surge disasters and so on. therefore, many engineers and researchers have devoted their energy to prevent these costal disasters. The development of artificial reefs including sunken vessels is one of their remarkable achievements and various kind of these artificial upwelling structures have been designed and applied. However, the flow characteristics around a Tetrapod under the water has not been investigated experimentally. So in this article, in uniform flow of circulating water channel and some different velocities, PIV measurement has been conducted on the flow characteristics behind a Tetrapod. The results were analyzed on the flow characteristics of both cases of a Tetrapod. Therefore, it can be concluded that the both cases have its own distinctive flow characteristics behind the bluff body; Case A has an steep upstream flow pattern. On the contrary, Case B has an developed downstream flow pattern in the near wake of the Tetrapod. The velocity gradient at position x=150mm of Case-A appears gently up and down But, the velocity gradient at the same position of Case-B appears better highly up and down.

• 한국해양공학회:학술대회논문집
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• 한국해양공학회 2001년도 추계학술대회 논문집
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• pp.213-219
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• 2001

In this paper, particle velocity of slurry flow, a kind of solid-particle two phase flow, was measured by using a particle tracking velocimetry. Particles are modeled by sphere-shaped glass whose diameters are 3mm, 5mm, and 7mm At first, a particle which is falling in the water is captured and analyzed to give their free falling velocity. The falling velocity was very high up to about 4m/sec in the air, which needs special algorithm for the accurate measurement. For the upwelling slurry flow in the straight duct, there are some noises caused by cavity. However, the effect was so small that it does not affect the measurement of large particles. From the preliminary study of applying the PTV to measurement of particle movement in slurry flow, we could find out the optimum value of parameters: threshold value., searching area radius and correlation area size.

• 대한조선학회논문집
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• 제34권4호
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• pp.148-157
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• 1997

본 논문에서는 유한체적법을 이용한 수치계산과 이차원수조에서의 유동가시화에 의한 실험적 연구를 통해 평행하게 흐르는 유체 내에 설치된 V-형 연직순환 구조물 주위의 유동현상을 해석하였다. V-형 연직순환 구조물은 성층화되어 연직방향으로 정체된 유동장을 교란하여 섞어주는 역할을 하는 해수유동 제어구조물로서 해상 구조물의 주변에 유동정체로 발생될 수 있는 부영양화 등을 감소시키는 도구로 사용될 수 있다. 판과 판의 사이각(dihedral angle; ${\theta}$), 판의 바닥면에 대한 경사각(inclination angle; ${\phi}$) 그리고 Reynolds 수에 대한 와류두(vortex head) 상승높이의 특성 및 유기속도(induced velocity)의 강도를 비교 검토함으로써 파라미터와 유동특성과의 관계를 살펴보았다. 또한 이를 통해서 연직순환 구조물의 최적형상은 사이각과 경사각이 $90^{\circ}$일 때라는 결론을 얻을 수 있었다.

• International Journal of Naval Architecture and Ocean Engineering
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• 제13권1호
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• pp.526-544
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• 2021

Based on the potential flow theory, a fully nonlinear numerical procedure is developed with boundary element method to analyze the interaction between a fixed semi-submersible platform and incident waves in open water. The incident wave is separated from the scattered wave under fully nonlinear boundary conditions. The mixed Euler-Lagrangian method is used to capture the position of the disturbed wave surface in local coordinate systems. The wave forces exerted on an inverted conical frustum are used to ensure the accuracy of the present method and good agreements with published results are obtained. The hydrodynamic characteristics of the semi-submersible platform interacting with regular waves are analyzed. Pressure distribution with time and space, tension and compression of the platform under wave action are investigated. 3D behaviors of wave run-ups are predicted. Strong nonlinear phenomena such as wave upwelling and wave interference are observed and analyzed.

• Journal of the korean society of oceanography
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• 제33권3호
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• pp.53-63
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• 1998

The Princeton ocean model (POM) with free surface in sigma-coordinate, governed by primitive equations, is used to examine the response of sea water in Deukryang Bay to a typhoon. The model reproduces reasonably well the main features in the wind-driven dynamics due to passing of a typhoon. In response to the wind, the coastal jet develops and the upwelling(or downwelling) occurs dominantly in both sides of the bay. This result implies that there should be an overturn in the bay water with the passing of typhoons. Numerical results of POM are also compared to those of a depth-averaged model. From the comparison, it is postulated that the bottom drag coefficient conventionally used for the two-dimensional flow models is inadequate due to overestimation of the computed current field.