• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume II
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• pp.926-929
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• 2006

Some features of vertical structure of the frontal interaction zone of the warm Kuroshio Current and cold Oyashio Current are known from 1930 from analysis of ship data. Ship data however do not allow carrying out the area detailed survey opposite to satellite infrared (IR) observations which possess by high spatial and temporal resolution. Analysis of NOAA AVHRR IR images demonstrated that process of formation and development of the Kuroshio warm core rings is highly complex. They are formed as a result of development of anticyclonic meanders of the warm Kuroshio waters and spin off them from the current. Joint analysis of thermal infrared images and altimetry data has also indicated that interaction of eddies to the frontal zone plays a crucial role in formation of large eddies moving to the Southern Kuril region.

• 한국해양학회지:바다
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• 제24권2호
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• pp.318-331
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• 2019

HYCOM 재분석 자료를 이용하여 동해에서 2003년과 2014년에 장기간 지속되었던 두 개의 난수성 에디를 선정하여 각각 WE03과 WE14로 명명하고 비교 분석하였다. 두 난수성 에디가 형성되는 시기는 동한난류가 평년에 비해 북상하는 것으로 나타났으며, 이들 난수성 에디는 동한난류와 아한대전선의 상호작용을 통해 상대적으로 수심이 얕은 한국대지 해역에서 생성되었다. 겨울철 연직 혼합에 의해서 난수성 에디의 중심부는 수심 150 m까지 $13^{\circ}C$, 34.1 psu 가량의 균질한 특성을 보였다. WE03이 생성된 후 이듬해인 2004년에 대한해협 서수도를 통해 동해로 유입되는 해수의 양이 평년에 비해 많았으나 WE14가 생성된 후 이듬해인 2015년에는 대한해협 서수도를 통해 동해로 유입되는 해수의 양이 평년에 비해 많지 않았다. 이에서 대마난류가 난수성 에디에 열과 염을 공급하지만, 난수성 에디의 장기 지속에는 큰 영향을 미치지 않음을 알 수 있다. 두 난수성 에디는 울릉도 부근에서 1년 6개월 이상 유지되었는데, 두 에디의 이동경로에 있어 특별한 공통점은 보이지 않았다. 울릉분지 부근에서는 동한난류의 사행 등으로 크고 작은 에디가 계속 생성된다. 장기간 존속하는 난수성 에디는 특별한 외적 요인에 의해서 생성되는 것이 아니라, 동한난류 또는 동한난류가 사행하는 과정에서 생성된 에디와의 상호작용을 통해 생성된 것으로 보인다. 동한난류가 평년에 비해 북상했던 시기에 장기간 지속된 난수성 에디가 항상 발생하지는 않았다는 점이 위와 같은 결론을 뒷받침한다.

• 한국연소학회:학술대회논문집
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• 한국연소학회 2005년도 제31회 KOSCO SYMPOSIUM 논문집
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• pp.198-203
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• 2005

The LES-based level-set flamelet model has been applied to analyze the turbulent propane/air premixed bluff-body flame with a highly wrinkled flame fronts. The present study has been motivated to investigate the interaction between the flame front and turbulent eddies. Special emphasis is given to study the effect of G equation filtering treatment on the precise structure of turbulent premixed flames as well as the effect of sub-grid scale (SGS) eddies on the wrinkling of the flame surface. The level-set/flamelet model has been adopted to account for the effect of turbulence-flame interaction as well as to properly capture the flame front. Numerical results indicate that the present LES-based level-set flamelet approach has a capability to realistically simulate the highly non-stationary turbulent premixed flame.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2005년도 학술발표회(1)
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• pp.347-348
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• 2005

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume II
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• pp.969-972
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• 2006

The long-range High-Frequency (HF) ocean radar system has observed surface velocity field in the upstream of the Kuroshio north of Ishigaki Island and east of Taiwan since 2001. Applying a new method to extract geostrophic velocity component from the HF surface velocity data with the aid of satellite-born wind data, time series of daily surface geostrophic velocity field has been determined. Despite limited width of the study area of the HF radar, analysis of the sea surface height anomaly determined from the satellite altimetry data in a wider area can provide estimated dates of arrival of mesoscale eddies in the study area of the HF radar. Variations of the Kuroshio position and strength are studied in detail for these cases of interaction with mesoscale eddy, although number of occurrence of direct interaction with the Kuroshio in the study area is not statistically enough. For example, when an anticyclonic eddy approaches to the Kuroshio, the Kuroshio axis is found tend to move northward, keeping away from the approaching eddy from the east.

• 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.

• Journal of Mechanical Science and Technology
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• 제15권12호
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• pp.1741-1749
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• 2001

Recent studies of the structure of wall turbulence have lead to the development of a conceptual model that validates and integrates many elements of previous models into a relatively simple picture based on self-assembling packets of hairpin vortex eddies. By continual spawning new hairpins the packets grow longer in the streamwise direction, and by mutual induction between adjacent hairpins the hairpins are strained so that they grow taller and wider as they age. The result is a characteristic growth angle in the streamwise-wall normal plane. The spanwise growth of individual packets implies that packets must either merge or pass through each other when they come into contact. Direct numerical simulations of the growth and interaction of spanwise adjacent hairpins shows that they merge by the vortex connection mechanism originally proposed by Wark and Nagib (199). In this mechanism the quasi-streamwise legs of two hairpins annihilate each other, by virtue of having opposite vorticity, leaving a new hairpin of approximately double the width of the individuals. PIV measurements in planes parallel to the wall support this picture. DNS of multiple hairpins shows how the spanwise scale doubles when the hairpins form an array.

• 대한기계학회논문집
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• 제18권12호
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• pp.3386-3394
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• 1994

An experimental study has been performed on the flow over a rotating disk, where the diameter of the disk is 500 mm and the maximum vertical deviation of the upper surface is $50 \mu{m}$ for the whole range of the angular velocity up to 3400 rpm. The flow visualization experiment for the wall jet flow induced by impinging circular jet is carried out using schlieren system and measurements are made by 3-hole and 5-hole pitot tubes. Schlieren photographs show that as the rotating speed increases the wall jet flow becomes more stable and the size of the largest eddies becomes smaller. Measurements for impinging jet flow on the stationary disk verify the accuracy of the present experiment, and those for free rotating disk flow display the existence of transition region from laminar to turbulent flows. Measurements for impinging jet flow on the rotating disk exhibit the interaction between the wall jet and the viscous pumping effect, which explains the decay in size of turbulent eddies illustrated by the schlieren photographs.

• 한국전산유체공학회지
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• 제18권1호
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• pp.49-57
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• 2013

Analysis of fluid-structure interaction for two nearby underwater vehicles immersed in the sea is quite challenging because simulation of flow around them is very difficult due to the complexity of underwater vehicle shapes. The conventional approach using body-fitted or unstructured grids demands much time in dynamic grid generation, and yields slow convergence of solution. Since an analysis of fluid-structure interaction must be based on accurate simulation results, a more efficient way of simulating flow around underwater vehicles, without sacrificing accuracy, is desirable. An immersed boundary method facilitates implementation of complicated underwater-vehicle shapes on a Cartesian grid system. An LES modeling is also incorporated to resolve turbulent eddies. In this paper, we will demonstrate the effectiveness of the immersed boundary method we adopted, by presenting the simulation results on the flow around a modeled high-speed underwater vehicle interacting with a modeled low-speed one.

• 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.