• 한국전산유체공학회:학술대회논문집
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• 한국전산유체공학회 1999년도 추계 학술대회논문집
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• pp.152-157
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• 1999

For the simulation of the blood flow in coronary artery, the system modeling of coronary hemodynamics is combined with CFD technique. The blood flow in coronary artery interacts with the global coronary circulation. Especially in case of the coronary artery with stenosis, the interaction plays an important role in the hemodynamics of the circulation. In this study we present a combined numerical approach using both the CFD technique for flow simulation and the global system model of coronary circulation. We use a lumped parameter model for the global simulation of coronary circulation whereas the finite element method is employed to compute the viscous flow field in stenosed coronary artery, The time variation of the pressure drop due to stenosis is obtained from the proposed numerical method. Numerical results shows that the flow resistance and pressure drop due to stenosis has a relatively large value in systole.

• 한국해안해양공학회지
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• 제16권4
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• pp.241-257
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• 2004

전구해양순환모형인 Bryan-Cox-Semtner모형에서 파생된 NCAR의 NCOM모형을 이용하여 한반도 주변해역의 해수순환을 가능한 세밀하게 해상시킨 예단적 전구해양순환모형을 수립하였다. 모형영역은 남북방향으로 $80.6{^\circ}S~88.6{^\circ}N$의 범위로서 북극해가 제외되었으며, 한반도 주변이 약 $0.3^\circ$로 해상된 수평 가변격자와 연직방향으로 15층으로 구성하였다. 섬 주변해안의 순환을 적절히 재현하기 위한 구멍완화법(Hole-relaxation method)을 적용하여 22개의 섬처리가 고려되었으며, NCAR에서 CSM(Climate System Model)운용을 위해 300년동안 spin-up 계산된 결과를 초기자료로 하고, Choi et al.(2002)의 접합 대기해양모형의 결과로부터 얻은 바람응력자료가 사용되었다. 모형결과로부터, 전구와 북서태평양 해역의 순환패턴을 살펴보았으며, 한반도 주변의 5개해협에서의 용적수송량을 Choi et al.(2002)의 결과 및 관측치와 비교하였다.

• Ocean and Polar Research
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• 제34권4호
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• pp.431-444
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• 2012

We simulated and compared present and future ocean circulation in the East China Sea using an East Asia Regional Ocean model. Mean climate states for 1990~1999 and 2030~2039 were used as surface conditions for simulations of present and future ocean circulation, which were derived from the simulations of three different global climate models, ECHAM5-MPI, GFDL-CM2.0 and MIROC3.2_hires, for the 20th century and those of 21st century as projected by the IPCC SRES A1B. East Asia Regional Ocean model simulated the detailed patterns of temperature, salinity and current fields under present and future climate conditions and their changes instead of the simple structures of global climate models. To some extent, there are consistent ocean circulation changes derived from the three pairs corresponding to the global climate model in so much as the temperature increases not only in winter but summer at both the surface and bottom and that temperature and salinity changes are prominent near the Chinese coast and in the Changjiang bank. However, the simulated circulations are different among each other depending on the prescribed atmospheric conditions not only under present climate but also with regard to future climate conditions. There is not a coincident tendency in ocean circulation changes between present and future simulations derived from the three pairs. This suggests that more simulations with different pairs are needed.

• 한국지구과학회지
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• 제28권5호
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• pp.545-555
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• 2007

Ocean general circulation model developed by GFDL on the basis of MOM4 of FMS are examined and evaluated in order to elucidate the global ocean status. The model employs a tripolar grid system to resolve the Arctic Ocean without polar filtering. The meridional resolution gradually increases from $1/3^{\circ}$ at the equator to $1^{\circ}$ at $30^{\circ}N(S)$. Other horizontal grids have the constant $1^{\circ}$ and vertical grids with 50 levels. The ocean is also coupled to the GFDL sea ice model. It considers tidal effects along with fresh water and chlorophyll concentration. This model is integrated for a 100 year duration with 96 cpu forced by German OMIP and CORE dataset. Levitus, WOA01 climatology, serial CTD observations, WOCE and Argo data are all used for model validation. General features of the world ocean circulation are well simulated except for the western boundary and coastal region where strong advection or fresh water flux are dominant. However, we can find that information concerning chlorophyll and sea ice, newly applied to MOM4 as surface boundary condition, can be used to reduce a model bias near the equatorial and North Pacific ocean.

• Journal of Astronomy and Space Sciences
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• 제31권1호
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• pp.91-99
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• 2014

The atmospheric flow in the 3-Cell model of global atmosphere circulation is described by the Lagrange's equation of the non-inertial frame where pressure force, frictional force and fictitious force are mixed in complex form. The Coriolis force is an important factor which requires calculation of fictitious force effects on atmospheric flow viewed from the rotating Earth. We make new Mathematica platform to solve Lagrange's equation by numerical analysis in order to analyze dynamics of atmospheric general circulation in the non-inertial frame. It can simulate atmospheric circulation process anywhere on the earth. It is expected that this pedagogical platform can be utilized to help students studying the atmospheric flow understand the mechanisms of atmospheric global circulation.

• 대기
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• 제23권4호
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• pp.377-387
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• 2013

Projections of changes in the low latitude atmospheric circulation under global warming are investigated using the results of the CMIP5 ensemble mean. For this purpose, 30-yr periods for the present day (1971~2000) and the end of the $21^{st}$ century (2071~2100) according to the RCP emission scenarios are compared. The wintertime subtropical jet is projected to strengthen on the upper side of the jet due to increase in meridional temperature gradient induced by warming in the tropical upper-troposphere and cooling in the stratosphere except for the RCP2.6. It is also found that a strengthening of the upper side of the wintertime subtropical jet in the RCP2.6 due to tropical upper-tropospheric warmings. Model-based projection shows a weakening of the mean intensity of the Hadley cell, an upward shift of cell, and poleward shift of the Hadley circulation for the winter cell in both hemispheres. A weakening of the Walker circulation, which is one of the most robust atmospheric responses to global warming, is also projected. These results are consistent with findings in the previous studies based on CMIP3 data sets. A weakening of the Walker circulation is accompanied with decrease (increase) in precipitation over the Indo-Pacific warm pool region (the equatorial central and east Pacific). In addition, model simulation shows a decrease in precipitation over subtropical regions where the descending branch of the winter Hadley cell in both hemispheres is strengthened.

• 한국지구과학회지
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• 제22권5호
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• pp.415-422
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• 2001

대류권과 성층권의 대기대순환에 관한 연구는 전지구 규모의 기후변동에 대한 인간활동의 영향을 이해하는 데에 있어서 매우 중요하다. 최근, 상부대류권과 성층권의 대기대순환에 있어서의 일년주기의 존재가 많은 연구에 의하여 보고되어졌다. 이 연구에서는 10년간(1985년 12월${\sim}$1995년 11월)의 자료에 대하여, 변형오일러평균방정식계의 운동방정식과 연속방정식을 이용하여 잔차평균자오면순환을 구하고, 그 순환과 100hPa면을 가로지르는 질량 플럭스들의 장기변동을 조사한다. 그 장기변동을 정량적으로 파악하기 위하여 중회귀통계모델을 사용한다. 특히, 이 연구에서는 이상기상과 전지구 규모의 기후변동의 원인으로서 알려진 엘니뇨현상과 관련한 대류권과 성층권의 평균자오면순환에 초점을 맞춘다. 연구의 결과는, 전지구 규모의 대류권-성층권 평균자오면순환은 엘니뇨현상과 준2년주기진동의 동풍 위상 동안에 강화되어지고, 라니냐현상과 준2년주기진동의 서풍 위상 동안에 약화되어진다는 사실을 보인다. 그리고, 1991년 6월에 있었던 피나투보 화산 폭발의 신호가 얻어진다. 그 화산 폭발 때문에 전지구 규모의 대류권-성층권 평균자오면순환은 급격히 강화되어진다.

• 한국수자원학회논문집
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• 제32권6호
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• pp.617-625
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• 1999

지구 온난화는 산업혁명이후 이미 시작되었으며 최근에 와서 그 정도가 심해지고 있다. CO2와 같은 온실기체의 증가를 가장 큰 원인으로 하는 지구 온난화의 영향이 아직 정량적으로 밝혀지고 있지만 대기순환모형(General Circulation Model: GCM)을 이용한 연구에서 이러한 온실기체의 증가가 지구의 평균온도를 상승시킨다고 밝히고 있다. 지구 온난화는 전지구적 물의 순환에도 영향을 미쳐 지구 곳곳의 강수패턴에 변화를 가져오는데 근래에 자주 발생하는 대규모 가뭄이나 홍수화 같은 극치기상이 이러한 지구온난화의 간접증거로 자주 언급되곤 한다. 국내의 경우도 예외는 아니어서 근래에 들어 빈번한 홍수 및 가뭄을 경험하고 있다. 본 연구에서는 지구온난화에 따른 홍수 및 가뭄의 빈도변화 분석을 목적으로 한다. 이러한 연구목적을 달성하기 위해 먼저 현재상태가 지구온난화 과정의 한 시점이라는 가정 아래 현재까지 관측된 일강수량 자료를 분석하여 과거 연강수량의 증가가 일강수량의 분포에 어떤 식으로 영향을 미치고 있는지를 분석하여 보았다. 대상자료는 금강유역의 17개 지점을 선정하여 이용하였고, 분석결과로서 연강수량과 무강수일수는 상대적으로 작은 상관을 보이고 있음을 밝힐 수 있었으며 오히려 10mm이하 또는 50mm이상의 강수일수에 0.8-0.9의 높은 상관을 보임을 파악할 수 있었다.

• 한국원자력학회:학술대회논문집
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• 한국원자력학회 2005년도 추계학술발표회
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• pp.602-603
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• 2005

• Ocean and Polar Research
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• 제35권2호
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• pp.127-134
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• 2013

In this study we investigated changes in the Tsushima Warm Current (TWC) under the global warming scenario RCP 4.5 by analysing the results from the World Climate Research Program's (WCRP) Coupled Model Intercomparison Project Phase 5 (CMIP5). Among the four models that had been employed to analyse the Tsushima Warm Current during the 20th Century, in the CSIRO-Mk3.6.0 and HadGEM2-CC models the transports of the Tsushima Warm Current were 2.8 Sv and 2.1 Sv, respectively, and comparable to observed transport, which is between 2.4 and 2.77 Sv. In the other two models the transports were much greater or smaller than the observed estimates. Using the two models that properly reproduced the transport of the Tsushima Warm Current we investigated the response of the current under the global warming scenario. In both models the volume transports and the temperature were greater in the future climate scenario. Warm advection into the East Sea was intensified to raise the temperature and consequently the heat loss to the air.