• 유체기계공업학회:학술대회논문집
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• 유체기계공업학회 2006년 제4회 한국유체공학학술대회 논문집
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• pp.401-402
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• 2006

The turbulent flow around a sphere was investigated using two experimental techniques: smoke-wire flow visualization in wind tunnel at Re=5300, 11000 and PIV measurements in a circulating water channel. The smoke-wire visualization shows flow separation points near an azimuthal angle of $90^{\circ}$, recirculating flow, transition from laminar to turbulent shear layer, evolving vortex roll-up and fully turbulent eddies in the sphere wake. The mean velocity field measured using a PIV technique in x-y center plane demonstrates the detailed near-wake structure such as nearly symmetric recirculation region, two toroidal vortices, laminar separation, transition and turbulent eddies. The PIV measurements of turbulent wake in y-z planes show that a recirculating vortex pair dominates the near-wake region.

• Journal of Advanced Marine Engineering and Technology
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• 제32권1호
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• pp.100-109
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• 2008

The three-dimensional flows in the Weis-Fogh mechanism are studied by flow visualization and numerical simulation by the vortex method. The vortex method. especially the vortex stick method, is employed to investigate the vortex structure in the wake of the two wings. The pressure is estimated by the Bernoulli equation, and the lift on the wing are also obtained. As the results the eddies near the leading edge of each wing in the fling stage take a convex shape because the eddies shed from both tips entrain the flows and the downwash in the rotating stage is deflected toward the outside because the outside tip vortex is stronger than the inside one. And the lift coefficient on the wings in this mechanism is almost independent of the Reynolds number.

• The Journal of the Acoustical Society of Korea
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• 제23권2E호
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• pp.68-73
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• 2004

In the East Sea of Korea, the ocean environments are known to have strong variations in space and time. Their effects are very important factors in sound propagation and sonar performance. We consider the environmental factors such as eddies and thermal fronts affecting underwater sound propagation and target detection performance by sonars. Unfortunately, however, the detailed structure of eddies is usually difficult to understand by using the sea surface temperatures from infrared images alone or a few profiles from the CTD (conductivity, temperature and depth) castings. The temperature fields of eddy and thermal front are simulated with typical patterns of those obtained from several observations. This paper delivers the overviews of environments and acoustic models with their simulation results on sonar performance.

• Journal of Advanced Marine Engineering and Technology
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• 제20권3호
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• pp.101-109
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• 1996

Two-dimensional lid-driven closed flows within square cavity were studied numerically for four Reynolds numbers : $10^4$, 3$\times10^4$, 5$\times10^4$ and 7.5$\times10^4$. A convective difference scheme to maintain the same spatial accurary by irregular grid correction is adopted by applying the interior division principle. Grid number is $80\times80$and its minimum size is about 1/400 of the cavity height. At Re=$10^4$, periodic migration of small eddies appearing in corner separation region and its temporal sinusoidal fluctuation are represented. At three higher Reynolds numbers(3$\times10^4$, 5$\times10^4$ and 7.5$\times10^4$), an organizing structure of four consecutive vorticles at two lower corners is revealed from time-mean flow patterns. But, instantaneous flow characteristics show very random unsteady fluctuation mainly due to the interaction between rotating shed vortices and stationary eddies within the corners.

• 한국해양학회지
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• 제30권3호
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• pp.170-183
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• 1995

1992년 11월부터 1993년 9월 사이 동해남서해역에서 조사한 인공위성 추적부 이, CTD, ADCP 자료를 이용하여 와류와 표층해류의 물리적 구조를 분석하였다. 부이의 이동궤적으로부터 울릉분지내에서 동한난류의 사행과 연구해역에서 다양한 크기의 시계방향과 반시계방향의 와류가 존재하는 것을 처음으로 직접 해류조사로 밝힐 수 있었다. 비교적 오래 지속되는 시계방향의 와류가 울릉분지내와 북부(일 본)분지의 남서쪽에서 관측된 반면에 반시계방향의 와류가 속초와 동해시 사이의 연안역에서 여름철에 관측되었다. 울릉분지의 와류는 적어도 관측기간 중에는 분지 내에 머물러 있었으며, 반시계방향의 와류는 냉수의 존재와 밀접한 관련이 있는 것 으로 나타났다. 북부분지의 시계방향 와류는 울릉분지의 것보다 크며 더 길쭉한 타원 형태를 지녔다. 울릉분지의 와류는 주축과 종축이 각각 120 km, 70 km이고, 회전주기는 13.6일, 평균회전속도는 24 cm/s, 평균 와동운동에너지는 392 $cm^{2}$/s$^{2}$ 이다. 북부분지의 와류는 주축과 종축이 각각 168 km, 86 km이고, 회전 주기는 14.9일, 평균회전속도는 29 cm/s, 평균 와동운동에너지는 629 $cm^{2}$/s/ sup 2/ 의 특성을 보였다. 와류의 평균이동속도는 두 경우 모두 약 3 cm/s이다. 울릉분지내에서 ADCP로 관측한 표층해류와 지형류의 상호일치는 울릉분지의 와류 가 지형평형을 이루고 있음을 시사한다. 관측된 와류는 해저지형에 강하게 지배 되어 있다.

• Wind and Structures
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• 제5권2_3_4호
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• pp.115-126
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• 2002

A mesoscale meteorological model is applied to simulate turbulent airflow and eddy shedding over the Isle of Arran, SW Scotland, UK. Under conditions of NW flow, the mountain ridge of Kintyre, located upwind of Arran, induces gravity waves that also affect the airflow over the island. The possibility to nest domains allows description of the airflow over Arran with a very high resolution grid, while also including the effects of the surrounding mainland of Scotland, in particular of the mountain ridge of Kintyre. Initialised with a stably stratified NW flow, the mesoscale model simulates quasi-stationary gravity waves over the island induced by Kintyre. Embedded in the larger scale wave trains there is continuous development of small-scale transient eddies, created at the Arran hill tops, that move downstream through the stationary wave field. Although the transient eddies are more frequently simulated on the northern island where the terrain is more pronounced, they are also produced over Tighvein, a hill of 458 m on the southern island where measurements of surface pressure and 2 m meteorological variables have been recorded at intermittent intervals between 1996 and 2000. Comparison between early observations and simulations so far show qualitatively good agreement. Overall the computations demonstrate that turbulent flow can be modelled with a horizontal resolution of 70 m, and describe turbulent eddy structure on wavelength of only a few hundred metres.

• 대한기계학회논문집B
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• 제22권4호
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• pp.417-427
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• 1998

The effect of secondary flow on the heat transfer of a turbulent wake generated by a flat plate was experimentally investigated. The secondary flow was induced in a curved duct in which the flat plate wake generator was installed. All three components of turbulent heat flux were measured in the plane containing the mean radius of curvature of the curved duct. The results showed that mean temperature profiles deviate from the similarity of the straight wake because of the cold fluid transported from the free-stream. The half-width of the mean temperature profile increased rapidly by upwash motion of the secondary flow. The changes to turbulence structure caused by the secondary flow show more pronounced effect on heat transport than on momentum transport. This is because the response to the variation of flow conditions is delayed in temperature field. Negative production of the turbulent heat flux is observed in the inner wake region. From the conditional averaging, it has been found that the negative production of the turbulent heat flux is generated due to a mixing process between the hot and low momentum eddies occupied in the inner wake region and the cold and high momentum eddies in the potential region.

• 설비공학논문집
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• 제7권4호
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• pp.622-632
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• 1995

The present numerical study is aimed to investigate time-dependent characteristics of a two-dimensional lid-driven square cavity flow of three high Reynolds numbers, $7.5{\times}10^3$, $10^4$ and $3{\times}10^4$. A conservative convection term on irregular grids was adopted by renewing the MAC type difference schemes on regular grids. Relaxation of velocity and pressure is implemented by SOLA algorithm. In case of $Re=7.5{\times}10^3$, flow behavior converges to steady state after a transient period. But for $Re=10^4$, periodic unsteady sinusoidal fluctuation of local velocity and kinetic energy is found and continuous movements of small eddies in the secondary flow regions are also discovered. Random generation of eddies and their active migrating behavior are detected for $Re=3{\times}10^4$, resulting in complete unsteady and non-linear flow characteristics. And, an organized structure similar to a Moffat vortex is also observed from the time-mean flow patterns. Furthermore, a typoon-like vortex(TLV) appears intemittently and rotates along the separation regions and boundary layers.

• 대한기계학회논문집
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• 제14권6호
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• pp.1661-1668
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• 1990

본 연구에서는 코히런트 와(渦)에 지배되는 난류 예혼합화염의 미세구조를 밝 히기 위해 슐리이렌사진과 온도, 이온전류의 3가지를 동시에 측정하고, 그 변동량을 통계처리, 분석하여, 미시적인 화염구조 모델을 제시하고자 한다.

• 한국해양학회지
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• 제30권6호
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• pp.565-583
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• 1995

난수성 eddy의 운동에 있어서 경계면 마찰과 해저지형의 중요성을 연구하기 위하여 비선형 QG-모델이 사용되었다. 수직구조를 나타내는 유선함수의 경험적 직교함수는 순압과 제 1 경압 역학 함수를 표현한다. 이 모델은 10 km ${\times}$ 10 km의 격자간격을 지닌 1000 km ${\times}$ 1000 km으로 구성되어 있고 360일동안 시험하였다. 대한해협을 통한 유입량은 쓰가루해협을 통하여 빠져 나간다. 울릉분지내(평평한 해저지형)에서는 QG방정식의 비선형 이류항과 ${\beta}$-효과사이에 균형이 난수성 eddy를 북쪽으로 이동하게 한다. 대륙사면위에서의 난수성 eddy는 비선형항이 중요하게 작용하지만, 평평한 지형에서는 보조적인 역활을 한다. 해저지형이 변화하는 해역에서 난수성 eddy의 비선형항은 시간의 함수이다. 강한 eddy는 북쪽으로 이동한다. Eddy의 세기가 약해지면, 비선형항과 지형적인 베타효과항이 균형을 이루게 된다. Eddy의 분산과 함께 비선형성이 감소하므로서, 지형적 Rossby파 개념에 의하여 난수성 eddy는 대륙사면을 따라서 남하한다. 수치실험은 난수성 eddy의 운동에 미치는 경계면 마찰의 중요성을 확인하였다. 난수성 eddy의 북쪽 침투거리는 경계면 마찰계수의 감소로 증가하게 된다 아울러 Reynolds number의 감소로 북쪽이동을 방지할 수 있다. 또한 이 난수성 eddy운동과정에 있어서 해저지형이 중요한 역할을 하는 것이 제시되었다.