• 대기
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• 제25권1호
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• pp.51-66
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• 2015

This study was conducted to perform various sensitivity experiments using WRF (Weather Research and Forecasting) model in order to determine the effects of terrains of the Korean Peninsula and the land-sea thermal contrast on the formation and development of the convergent cloud band for the cases of 1 February 2012. The sensitivity experiments consist of the following five ones: CNTL experiment (control experiment), and TMBT experiment, BDMT experiment and ALL experiment that set the terrain altitude of Taeback Mountains and Northern mountain complex as zero, respectively, and the altitude of the above-mentioned two mountains as zero, and LANDSEA experiment that set to change the Korean Peninsula into sea in order to find out the land-sea thermal contrast effect. These experiment results showed that a cold air current stemming from the Siberian high pressure met the group of northern mountains with high topography altitude and was separated into two air currents. These two separated air currents met each other again on the Middle and Northern East Sea, downstream of the group of northern mountains and converged finally, creating the convergent cloud band. And these experiments suggested that the convergent cloud band located on the Middle and Northern East Sea, and the cloud band lying on the southern East sea to the coastal waters of the Japanese Island facing the East Sea, were generated and developed by different dynamical mechanisms. Also it was found that the topography of Taeback Mountains created a warm air advection region due to temperature rise by adiabatic compression near the coastal waters of Yeongdong Region, downstream of the mountains. In conclusion, these experiment results clearly showed that the most essential factor having an effect on the generation and development of the convergent cloud band was the topography effect of the northern mountain complex, and that the land-sea thermal contrast effect was insignificant.

• 대한전자공학회논문지SD
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• 제39권4호
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• pp.26-34
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• 2002

본 논문에서는 반도체 공정 중, 토포그래피 시뮬레이션을 수행함에 있어서, 기존의 셀 모델을 수정하여, 소요되는 메모리의 양을 최소화하는 셀 전진 모델을 개발하였다. 셀 전진 모델은, 전체 시뮬레이션 영역은 물질 정보만으로 나타내지며, 표면의 셀들만으로 리스트가 구성되고, 리스트에 표면 진화 계산에 필요한 정보가 저장된다. 개발된 시뮬레이터는 해석적 모델과 몬테카를로 모델을 이용하여 식각 공정에 있어서 입사이온 분포가 계산되며, 단위 공정 뿐만 아니라 공정 순서도에 따라 적층 캐패시터 또는 디램 셀(DRAM cell) 제조 공정과 같은 통합 공정을 수행한다. 개발된 시뮬레이터를 이용하여 디램 셀 제조 공정 시뮬레이션을 수행하였을 경우에, 소요된 셀은 5,440,500(130×155×270)개였고, 메모리 양은 22MB에 불과하였다.

• 한국해양공학회지
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• 제20권3호
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• pp.61-66
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• 2006

The estuary has a very complex coastline and bottom topography. Before the close of floodgate, the Keum river estuary was deposited with sediment from the Keum river, created bythe construction of the Keum river estuary dike. So, a periodical dredging is necessary to assure water depth for boat entry and departure to Kunsan port. Theof this study is to find the change of tidal current of M2tide and the topography before and after construction at the Geum River estuary dike. The change of water depth is investigated by digitizing the sea map (No.305) of Kunsan port, which was edited by National Oceanographic Research Institute. The calculated co-range and co-tidal charts of M2tide before the dike construction are similar to the observed ones. Therefore, the amplitude and phase after construction at Geum River estuary dike increases compared to before construction at Geum River estuary dike. The scour occurred in the A-A' section.

• 한국환경과학회지
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• 제9권5호
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• pp.397-402
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• 2000

Numerical simulation model using nesting method and considering topographic features was developed to predict atmospheric environments atmospheric flow temperature and diffusion of air pollutants in Kwangyang bay where having complex areas of point sources Korea. In addition developed simulation model was used tracing of spreading range of pollutants when a gas leaks suddenly from Yeo-cheon industrial complex. by comparing the measured and calculated data on atmospheric flow temperature and diffusion of air pollutants the results showed that this model can be well applied and complicated topography affected the diffusion of air pollutants.

• 한국산학기술학회논문지
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• 제11권12호
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• pp.5207-5215
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• 2010

단지계획 또는 특정 목적의 시설물 설립을 위한 적지선정은 제반여건과 주변환경을 면밀하게 고려해야 한다. 특히, 인간의 생활공간이라면 채광 및 통풍, 부지활용의 효용성 등이 중요한 요소이다. 이를 위해서 3차원 지형 모델링과 가상 시뮬레이션을 통한 다각적인 입체분석이 필요하다. 이러한 지형모델링에 필수적인 고해상 위성영상이 아리랑2호 위성(KOMPSAT2)을 통해 국내기술로 제공되고 있으므로 저렴한 비용으로 처리가 가능해 졌다. 본 연구에서는 특정목적의 단지계획을 위해 몇 개의 후보지를 선정하고 3차원 지형모델링과 토지정보를 이용하여 적지분석을 하고자 하였다. 이를 위해 필지분석, 지가산정, 경사도 분석, 향분석을 실시하였으며 각 후보지 별 평가지표를 마련하여 정량적인 평가를 시도한 결과 효율적이며 합리적으로 적지선정을 할 수 있었다.

• 한국환경과학회지
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• 제20권2호
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• pp.275-289
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• 2011

In order to clarify the relation between sea breeze penetration and Planetary Boundary Layer development in southeastern part of the Korean Peninsula, several numerical assessments were carried out using atmospheric numerical model WRF(Weather Research and Forecasting). Compared with onset time of sea breeze at eastern coast area(Uljin), the time at southern coast region(Masan) with complex costal line tend to delay for several hours. The penetration patterns of sea breeze between two coastal regions are some different due to the shape of their coastal line and back ground topography. Intensified valley wind due to high topography of lee side of Uljin can help penetration of sea breeze at early time. So penetration of sea breeze at early time often prevent PBL to develop at Uljin and lower PBL height last for a day time. But because of late penetration of sea breeze at Masna, PBL Height dramatically decrease after 1500LST. The distribution of front genesis function based on the heat and momentum variation are explained obviously the sea breeze penetration patterns and agreed well with the PBL height distribution.

• 한국콘텐츠학회:학술대회논문집
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• 한국콘텐츠학회 2008년도 춘계 종합학술대회 논문집
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• pp.436-440
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• 2008

단지계획 또는 특정 목적의 시설물 설립을 위한 적지선정은 제반여건과 주변환경을 면밀하게 고려해야 한다. 특히, 인간의 생활공간이라면 채광 및 통풍, 부지활용의 효용성 등이 중요한 요소이다. 이를 위해서 3차원 지형모델링과 가상 시뮬레이션을 통한 다각적인 입체분석이 필요하다. 이러한 지형모델링에 필수적인 고해상 위성영상이 아리랑2호 위성(KOMPSAT2)을 통해 국내기술로 제공되고 있으므로 저렴한 비용으로 처리가 가능해 졌다. 본 연구에서는 특정목적의 단지계획을 위해 몇 개의 후보지를 선정하고 3차원 지형모델링과 토지정보를 이용하여 적지분석을 하고자 하였다. 이를 위해 필지분석, 지가산정, 경사도 분석, 향분석을 실시하였으며 각 후보지 별 평가지표를 마련하여 정량적인 평가를 시도한 결과 효율적이며 합리적으로 적지선정을 할 수 있었다.

• Wind and Structures
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• 제30권6호
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• pp.547-558
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• 2020

With the development of economy and construction technology, more and more bridges are built in complex mountainous areas. Accurate assessment of wind parameters is important in bridge construction at complex terrain. In order to investigate the wind characteristics in the high-altitude difference area, a complex mountain terrain model with the scale of 1:2000 was built. By using the method of wind tunnel tests, the study of wind characteristics including mean wind characteristics and turbulence characteristics was carried out. The results show: The wind direction is affected significant by the topography, the dominant wind direction is usually parallel to the river. Due to the sheltering effect of the mountain near the bridge, the wind speed and wind attack angle along the bridge are both uneven which is different from that at flat terrain. In addition, different from flat terrain, the wind attack angle is mostly negative. The wind profiles obey exponential law and logarithmic law. And the fitting coefficient is consistent with the code which means that it is feasible to use the method of wind tunnel test to simulate complex terrain. As for turbulence characteristics, the turbulence intensity is also related to the topography. Increases sheltering effect of mountain increases the degree of breaking up the large-scale vortices, thereby increasing the turbulence intensity. Also, the value of turbulence intensity ratio is different from the recommended values in the code. The conclusions of this study can provide basis for further wind resistance design of the bridge.

• 한국지구과학회지
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• 제26권7호
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• pp.698-705
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• 2005

한반도 집중호우를 유발시키는 중규모대류복합체는 매우 복잡한 특성을 띠고 있다. 2004년 7월 14일 발생한 중 규모 대류복합체의 발달메커니즘을 분석한 결과, a) 대류복합체 생성 전에 강한 남서기류의 유입이 있었으며, b) 600hPa고도에서 강한 역전층이 나타났다. 역전층은 상층과 하층간의 상당온위의 차이를 유발하여 대기불안정을 더욱 강화시켰다. 그리고 c) 일반적인 중규모대류복합체 특징인 풍향의 쉬어보다는 풍속의 쉬어에 의해 대류계의 열역학 불안정이 강화되었다. 그리고 d) 흑산도 등 해안지방에 의해 유발되는 난류 및 대기불안정으로 인하여 중규모 대류복합체가 해안지방에서 발달한 것으로 보인다. 그러므로 지형에 의한 중규모 대류 복합체의 발달메커니즘 규명이 필요하다.

• 한국환경과학회지
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• 제19권1호
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• pp.27-37
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• 2010

A system coupled the prognostic WRF mesoscale model and CALMET diagnostic model has been employed for predicting high-resolution wind field over complex coastal area. WRF has three nested grids down to from during two days from 24 August 2007 to 26 August 2007. CALMET simulation is performed using both initial meteorological field from WRF coarsest results and surface boundary condition that is Shuttle Radar Topography Mission (SRTM) 90m topography and Environmental Geographic Information System (EGIS) 30m landuse during same periods above. Four Automatic Weather System (AWS) and a Sonic Detection And Ranging (SODAR) are used to verify modeled wind fields. Horizontal wind fields in CM_100m is not only more complex but better simulated than WRF_1km results at Backwoon and Geumho in which there are shown stagnation, blocking effects and orographically driven winds. Being increased in horizontal grid spacing, CM_100m is well matched with vertically wind profile compared SODAR. This also mentions the importance of high-resolution surface boundary conditions when horizontal grid spacing is increased to produce detailed wind fields over complex terrain features.