• Journal of the Korean Society for Aeronautical & Space Sciences
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• v.33 no.10
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• pp.17-25
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• 2005

A grid adaptation method within systems of chimera and patched grids is presented. Problem domains are divided into near-body and off-body fields. Near-body field is filled with curvilinear body-fitted grids that extend only a short distance from body surfaces and connected to other grid systems via chimera domain connectivity method. Off-body field is filled with patched uniform cartesian grids of varying levels of refinement. This method gives flexibility in grid generation and efficient adaptation capability. Several numerical experiments including 2D store separation were performed to show the performance of the proposed adaptation method.

• Proceedings of the Korean Association of Geographic Inforamtion Studies Conference
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• 2008.06a
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• pp.461-464
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• 2008

연안에서의 태풍 해일에 의한 침수범람 지역 예측을 위하여 GIS를 통한 정밀 육도-해도 접합 및 분석을 만리포 해변을 대상으로 시범 수행하였다. 만리포 해변의 정밀 육도-해도 접합을 위하여 고해상도 지상 LIDAR 시스템의 시범 측량 자료와 국토지리정보원의 수치지형도, 국립해양조사원의 수치해도 수심자료 및 한국 주변해역의 30초격자 수심자료를 사용하였다. 또한 평균해수면 산정을 위하여 만리포에 설치된 수압식파고계 조위자료와 해변의 표척을 통한 목측 관측을 통한 조위자료를 활용하였다. 다양한 자료의 GIS 기반 육도-해도 접합 및 분석을 통한 정밀 지형도 구축 기술은 태풍 해일에 의한 침수범람 예측을 위한 정밀 격자 수치모델의 입력 자료로 활용되어 침수 범람 예측 결과의 재해도(Hazard Map) 작성이 가능하고, 나아가 침식 퇴적 등의 지속적인 해안선 변화 모니터링에 활용될 수 있다.

• Journal of the Korean Society for Aeronautical & Space Sciences
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• v.48 no.2
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• pp.109-117
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• 2020

A structured grid system can be efficiently constructed by applying the patched-grid algorithm that alleviates many constraints of the conventional structured grid system. Three approaches were applied to case 4 of the EFD-CFD workshop: delta wing-cylindrical body shape to solve the existing grid generation problems and verify the results by comparing them with experimental data. Surface pressure distributions slightly differed from the experimental data at high angles of attack. The slope variation of the pitching moment with Mach number is analyzed and the variation can be explained with the tuck under phenomenon. In the supersonic region, the bow shock waves in front of the shape expand the region generating lift up to the rear of the configuration. Also, the tendency of the pitching moment with both Mach number and angle of attack was analyzed by comparing the positions of the center of pressure and the center of gravity.

• Journal of the Korean Magnetics Society
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• v.16 no.2
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• pp.111-114
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• 2006

We investigated the magnetism and electronic structures for the layered structures consisting of (110) layers of zinc-blende CrAs and MnAs. We calculated the electronic structures for $(CrAs)_3(MnAs)_3(110)$ superlattice consisted of alternating three layers of CrAs(110) and MnAs(110) by the full-potential linearized augmented plane wave (FLAPW) method. The calculated magnetic moment of Cr in interface layer ($3.07\;\mu_B$) was slightly larger than that of Cr atom in center layer ($3.06\;\mu_B$), while that of interface Mn atom ($3.74\;\mu_B$) was slightly smaller than the value of Mn atom in center layer ($3.76\;\mu_B$). The electronic structure and half-metallicity in this superlattice were discussed using the calculated density of states.

• Korean Journal of Remote Sensing
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• v.36 no.6_3
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• pp.1643-1652
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• 2020

To investigate the characteristics of detailed flows in a building-congested district, we coupled a computation fluid dynamics (CFD) model to the local data assimilation and prediction system (LDAPS), a current operational numerical weather prediction model of the Korea Meteorological Administration. For realistic numerical simulations, we used the meteorological variables such as wind speeds and directions and potential temperatures predicted by LDAPS as the initial and boundary conditions of the CFD model. We trilinearly interpolated the horizontal wind components of LDAPS to provide the initial and boudnary wind velocities to the CFD model. The trilinearly interpolated potential temperatures of LDAPS is converted to temperatures at each grid point of the CFD model. We linearly interpolated the horizontal wind components of LDAPS to provide the initial and boundary wind velocities to the CFD model. The linearly interpolated potential temperatures of LDAPS are converted to temperatures at each grid point of the CFD model. We validated the simulated wind speeds and directions against those measured at the PKNU-SONIC station. The LDAPS-CFD model reproduced similar wind directions and wind speeds measured at the PKNU-SONIC station. At 07 LST on 22 June 2020, the inflow was east-north-easterly. Flow distortion by buildings resulted in the east-south-easterly at the PKNU-SONIC station, which was the similar wind direction to the measured one. At 19 LST when the inflow was southeasterly, the LDAPS-CFD model simulated southeasterly (similar to the measured wind direction) at the PKNU-SONIC station.

• Proceedings of the Korean Vacuum Society Conference
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• 2010.08a
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• pp.222-222
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• 2010

III-V반도체 태양전지는 다양한 에너지 밴드갭을 만들 수 있으며 다중접합 태양전지의 경우 흡수 전류가 커져 효율이 증가한다. 태양전지의 효율의 증가는 태양광 발전시스템의 발전 단가를 낮추는 중요한 요인이다. 우리는 효율이 높은 III-V 태양전지를 제작하기 위해 일차적으로 Ge기판 위에 GaAs를 성장하고자 한다. Ge기판과 GaAs의 격자상수는 0.07%차이로 거의 일치하나 물질의 열팽창계수가 다르고 비극성인 Ge기판 위에 극성인 GaAs를 성장 시 위상불일치(Anti Phase Domain) 나타난다. 위상불일치 현상을 줄이기 위해 성장 시 온도와 V/III비율, 성장두께 등을 달리하여 성장한다. 표면의 상태가 좋아질수록 위상불일치 현상이 작으며 단일성장 보다 두 단계 과정으로 성장 했을 때 표면의 상태가 더 좋은 결과를 바탕으로[1], 20nm 이하로 얇게 seed층을 성장하고 그 위에 두꺼운 버퍼층을 성장하는 두 단계로 진행하였다. seed층의 성장온도는 $400{\sim}550^{\circ}C$, V/III 비율을 3.5~30으로 다양하게 바꿔가면서 표면의 상태를 비교하였다. 이때 버퍼층의 성장 온도와 V/III 비율은 $680^{\circ}C$, 192으로 일정하게 유지하였다. 표면은 SEM과 AFM을 통해 분석하였으며 결정질의 상태는 XRD 장비(Panalytical사)로 분석하고 광학적 특성은 LTPL(Accent Optical Technologies사)로 측정하였다. 실험의 결과는 seed층의 온도가 낮고 V/III 비율이 낮으며 성장률이 높았을 때 표면상태가 좋은 반면 버퍼층은 온도가 높고 V/III 비율이 높으며 성장률이 낮을 때 표면상태가 좋았다. seed층을 $450^{\circ}C$온도에서 V/III 비율이 3.5이고 성장률이 버퍼층에 비교하여 크게 하여 성장 했을 때 표면 거칠기가 3.75nm로 작아 표면의 상태가 좋음을 확인할 수 있었다. 두 단계 성장 시 표면의 상태는 seed층의 조건에 따라 결정됨을 알 수 있었다. 표면상태가 좋았을 때 결정상태 역시 좋았으며 성장률이 바뀜에 따라 반치폭이 42~45 arcsec의 값을 나타내었다. 광학적 특성은 10K에서 1.1512eV 밴드갭 에너지를 가지고 있어 양질의 GaAs가 성장됨을 알 수 있다.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.3 no.1
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• pp.16-24
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• 1998

In this study, Ocean General Circulation Model (OGCM) has been developed as a counterpart of Atmospheric General Circulation (AGCM) for the study of coupled ocean-atmosphere climate system. The oceanic responses to given atmospheric boundary conditions have been investigated using the OGCM. In an integration carried out over 100 simulated years with climatological monthly mean data (EXP 1), most parts of the model reached a quasi-equilibrium climate reproducing many of the observed large-scale oceanic features remarkably well. Some observed narrow currents, however, such as North Equatorial Counter Current, were inevitably distorted due to the model's relatively coarse resolution. The seasonal changes in sea ice cover over the southern oceans around Antarctica were also simulated. In an experiment (EXP 2) under boundary condition of 10-year monthly data (1982-1991) from NCEP/NCAR Reanalysis Project model properly reproduced major oceanic changes during the period, including El Ni$\tilde{n}$os of 1982-1983 and 1986-87. During the ENSO periods, the experiment showed eastward expansion of warm surface waters and a negative vertical velocity anomalies along' the equator in response to expansion of westerly current velocity anomalies as westerly wind anomalies propagated eastward. Simulated anomalous distribution and the time behavior in response to El Ni$\tilde{n}$o events is consistent with that of the observations. These experiments showed that the model has an ability to reproduce major mean and anomalous oceanic features and can be effectively used for the study of ocean-atmosphere coupling system.