• 제목/요약/키워드: Valley wind

검색결과 78건 처리시간 0.032초

대구지역의 국지적 대기순환풍의 환기경로에 관한 수치모의 실험 (Numerical Simulation Experiment on the Wind Ventilation Lane of the Local Circulation Winds in Daegu)

  • 구현숙;김해동;강성대
    • 한국환경과학회지
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    • 제13권4호
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    • pp.367-376
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    • 2004
  • In urban area, thermal pollution associated with heat island phenomena is generally regarded to make urban life uncomfortable. To overcome this urban thermal pollution problem, urban planning with consideration of urban climate, represented by the concept of urban ventilation lane, is widely practiced in many countries. In this study, the prevailing wind ventilation lane of a local winds in Daegu during the warm climate season was investigated by using surface wind data and RAMS(Reasonal Atmospheric Model System) simulation. The domain of interest is the vicinity of Daegu metropolitan city(about 900 $km^{2})$ and its horizontal scale is about 30km. The simulations were conducted under the synoptic condition of late spring with the weak gradient wind and mostly clear sky. From the numerical simulations, the following two major conclusions were obtained: (1)The major wind passages of the local circulation wind generated by radiative cooling over the mountains(Mt. Palgong and Mt. Ap) are found. The winds blow down along the valley axis over the eastern part of the Daegu area as a gravity flow during nighttime. (2)After that time, the winds blow toward the western part of Daegu through the city center. As the result, the higher temperature region appears over the western part of Daegu metropolitan area.

용문산 산악지역의 봄철 기온특성 (Characteristics of Springtime Temperature Within Mt. Youngmun Valley)

  • 천지민;김규랑;이선용;강위수;최종문;홍순성;박종선;박은우;김용삼;최영진;정현숙
    • 한국농림기상학회지
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    • 제16권1호
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    • pp.39-50
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    • 2014
  • 본 연구는 경기도 양평군 용문면 연수리 계곡에서 관측을 통하여 봄철 용문산 계곡의 온도 및 바람의 시공간적인 특성을 밝히고자 하였다. 2012년 3월부터 5월까지 기온 및 2, 3차원 바람을 관측하고 자료를 수집하였다. 연수리 계곡의 집중관측 자료를 분석한 결과, 용문산의 전기간 평균 기온감률은 $-0.44^{\circ}C$/100m이며 맑은 날($-0.48^{\circ}C$/100m), 강수일($-0.41^{\circ}C$/100m, 흐린 날($-0.40^{\circ}C$/100m) 순으로 기온감률이 낮아지는 것을 알 수 있었다. 기온상승률은 산 정상부분($0.89^{\circ}C$/1시간)에서 탁월한 대기와의 혼합효과에 의한 영향으로 계곡하부($1.45^{\circ}C$/1시간)보다 낮게 나타난다. 맑은 날 야간에는 산사면을 따라 냉각된 공기가 흘러내리는 현상이 온도와 바람장을 통해 확인하였다. 또한 계곡 저지대로부터 100-300m사이에서 온난대 형성도 확인 할 수 있었다. 산정상과 계곡하부에서 측정한 고도별 온도분포의 관측결과 계곡하부에서는 지면으로 부터 1.5m까지 지면의 영향을 받는 냉기층이 존재함을 알 수 있었다. 관측 높이별 바람분포를 관측한 결과 풍속은 높은 곳(3.5m)에서 강하며 비슷한 고도에 위치한 지점이어도 종관풍의 영향을 많이 받는 지점은 국지적인 바람의 패턴이 뚜렷하게 나타나지 않고 있었다.

대기안정도(大氣安定度)와 지형조건(地形條件)에 따른 풍향변동폭(風向變動幅)의 특성(特性) (Influence of Atmospheric Stability and Topography on the Wind Direction Fluctuations)

  • 김용국;이종범
    • 한국대기환경학회지
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    • 제8권2호
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    • pp.138-145
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    • 1992
  • Dependence of the standard deviation of wind direction fluctuations, ${\sigma}_{\theta}$, on atmospheric stability, averaging time and topography were analysed with the data measured at three sites, Youngjongdo beach of the Yellow Sea, Chuncheon basin and Doam-Dam valley. The results show that the mean value of ${\sigma}_{\theta}$ is large in complex terrain, the Doam-Dam site. It is notable that the large value of ${\sigma}_{\theta}$ at night is associated with the low wind speed and the strong stable condition. In order to study the long-period fluctuations of the wind direction, ${\sigma}_{\theta}$ for longer than 10 minutes averaging time was further analysed using the data obtained at the Chuncheon basin. At the averaging time shorter than 60 minutes, larger ${\sigma}_{\theta}$ is associated with longer averaging time in the strong stable condition. However, ${\sigma}_{\theta}$ was not affected significantly by wind speed and averaging time in neutral conditions. The results of the spectrum analysis for the time series data of wind direction showed that low-frequency fluctuations ranging from 10 to 60 minutes were dominated at the Chuncheon basin in strong stable condition.

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고속철도 열차 주행풍의 풍력발전 활용성에 대한 연구 (Study on Potential Utility of Wind Power Generation Based on Driving Wind of High-Speed Trains)

  • 김제근;서기범
    • 한국산학기술학회논문지
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    • 제18권10호
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    • pp.681-687
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    • 2017
  • 본 논문은 고속철도 차량 주행풍에 기반한 풍력 발전의 가능성을 분석한다. 저자는 풍속계와 데이터 분석 프로그램을 포함한 풍속 측정 장비를 구성하였으며, 이를 활용해 실제 고속 철도 차량 노선 부근에서 주행풍의 특성을 측정하였다. 저자는 반복적인 측정을 통해 주행풍 특성의 변화를 야기할 수 있는 다양한 요인들의 영향을 고려하였다. 우선적으로, 저자는 터널의 유무 및 계곡 지형 요인에 의해 구분되는 세 지점에서 개별적으로 주행풍의 풍속 및 지속 시간을 측정하여, 지형 요인에 따른 주행풍의 특성 차이를 분석한다. 또한 세 단계에 걸쳐 높이를 점증시키며 주행풍의 특성을 측정해, 차량과의 상대적인 높이에 따른 주행풍의 변화를 분석한다. 나아가 주행 차량의 특성을 고려하여, 길이와 중량에서 차이가 있는 Korean Train eXpress (KTX) 차량과 Super Rapid Train (SRT) 차량에 따른 주행풍의 차이를 분석한다. 끝으로 측정된 주행풍의 풍속 및 지속 시간을 토대로, 실제 풍력 발전에 도입할 경우 얻을 수 있는 풍력 에너지 수준을 도출하고, 이를 통해 기대되는 효용성에 대해 논의한다.

The influence of sea surface temperature for vertical extreme wind shear change and its relation to the atmospheric stability at coastal area

  • Geonhwa Ryu;Young-Gon Kim;Dongjin Kim;Sang-Man Kim;Min Je Kim;Wonbae Jeon;Chae-Joo Moon
    • Wind and Structures
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    • 제36권3호
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    • pp.201-213
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    • 2023
  • In this study, the effect of sea surface temperature (SST) on the distribution of vertical wind speed in the atmospheric boundary layer of coastal areas was analyzed. In general, coastal areas are known to be more susceptible to various meteorological factors than inland areas due to interannual changes in sea surface temperature. Therefore, the purpose of this study is to analyze the relationship between sea surface temperature (ERA5) and wind resource data based on the meteorological mast of Høvsøre, the test bed area of the onshore wind farm in the coastal area of Denmark. In addition, the possibility of coastal disasters caused by abnormal vertical wind shear due to changes in sea surface temperature was also analyzed. According to the analysis of the correlation between the wind resource data at met mast and the sea surface temperature by ERA5, the wind speed from the sea and the vertical wind shear are stronger than from the inland, and are vulnerable to seasonal sea surface temperature fluctuations. In particular, the abnormal vertical wind shear, in which only the lower wind speed was strengthened and appeared in the form of a nose, mainly appeared in winter when the atmosphere was near-neutral or stable, and all occurred when the wind blows from the sea. This phenomenon usually occurred when there was a sudden change in sea surface temperature within a short period of time.

산악 계곡지형에서의 오염확산에 관한 연구(II) :수치해석 (A Study on the Pollutant Dispersion over a Mountain Valley Region (II) : Numerical Simulation)

  • 심우섭;김석철;유성연
    • 설비공학논문집
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    • 제17권11호
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    • pp.1060-1071
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    • 2005
  • Passive gas dispersions over a 1/1000 scale terrain model at Eiffel type wind tunnel were reproduced by numerical simulation. Large eddy simulation was used to treat the sub-grid scale turbulences. The terrain features were represented by millions of point forces densely distributed over the solid surface using the virtual boundary method. The model simulations agreed very well with the experiments in a consistent fashion for all wind directions. The measured profiles of the wind speeds as well as the tracer gas concentrations were nicely simulated by the CFD model at most locations scattered over the model terrain. With scale factor adjusted and the thermal stratification effects incorporated, the CFD model was expected to provide reliable information on pollutant dispersions over the real complex terrains.

국지순환풍 모델을 이용한 광양만권 대기오염물질의 수치모델링 (Numerical Modeling of Pollutants using Local Wind Model in Gwangyang Bay, Korea)

  • 이상득
    • 한국대기환경학회지
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    • 제19권1호
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    • pp.13-23
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    • 2003
  • A local wind model and a three dimensional local environmental model including advection, diffusion, deposition. and photochemical reactions were performed at Gwangyang Bay, Korea, to predict air flow and air pollutants concentrations. A large grid was used, and nesting method was employed for small grid calculation. From the meterological module simulation, we were able to reproduce local wind characteristics such as sea/land winds and mountain/valley winds simulation at Gwangyang Bay. In addition, the concentration module showed high concentration regions at Yosu industrial complex, Gwangyang steel company. and Container anchor. It was also seen that air pollutants were dispersed by sea/land winds. A comparison between the measurement and the prediction of sulfur dioxide and nitric oxide, which are relatively low-reacted pollutants, was performed. However, the measured nitrogen dioxide and ozone concentrations were higher than the simulated ones. Particularly, ozone concentration between 8 a..m. and 8 p.m. agreed well, but the measured ozone during the rest of time were generally higher.

한반도 남동해안 해상풍 모의에 적합한 경계층 물리방안 연구 (Study on planetary boundary layer schemes suitable for simulation of sea surface wind in the southeastern coastal area, Korea)

  • 김유근;정주희;배주현;송상근;서장원
    • 한국환경과학회지
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    • 제14권11호
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    • pp.1015-1026
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    • 2005
  • The southeastern coastal area of the Korean peninsula has a complex terrain including an irregular coastline and moderately high mountains. This implies that mesoscale circulations such as mountain-valley breeze and land-sea breeze can play an important role in wind field and ocean forcing. In this study, to improve the accuracy of complex coastal rind field(surface wind and sea surface wind), we carried out the sensitivity experiments based on PBL schemes in PSU/NCAR Mesoscale Model (MM5), which is being used in the operational system at Korea Meteorological Administration. Four widely used PBL parameterization schemes in sensitivity experiments were chosen: Medium-Range Forecast (MRF), High-resolution Blackadar, Eta, and Gayno-Seaman scheme. Thereafter, case(2004. 8. 26 - 8. 27) of weak-gradient flows was simulated, and the time series and the vertical profiles of the simulated wind speed and wind direction were compared with those of hourly surface observations (AWS, BUOY) and QuikSCAT data. In the simulated results, the strength of rind speed of all schemes was overestimated in complex coastal regions, while that of about four different schemes was underestimated in islands and over the sea. Sea surface wind using the Eta scheme showed the highest wind speed over the sea and its distribution was similar to the observational data. Horizontal distribution of the simulated wind direction was very similar to that of real observational data in case of all schemes. Simulated and observed vertical distribution of wind field was also similar under boundary layer(about 1 km), however the simulated wind speed was underestimated in upper layer.

복잡지형의 대기확산모델 비교 (Comparison of Complex Terrain Dispersion Models)

  • 김영성;오현선
    • 한국대기환경학회지
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    • 제14권2호
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    • pp.81-94
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    • 1998
  • Six complex terrain dispersion models recommended by the U. S. Environmental Protection Agency were investigated using a hypothetical case in which a plume approaches complex terrain. The six models considered were Valley, CTSCREEN, COMPLEX 1, SHORTZ, RTDM, and CTDMPLUS, the latter four being closely studied. Highest concentrations were predicted for 48 receptors and plume behaviors were compared for stable and unstable meteorological conditions. Under stable conditions, ground-level concentrations were determined by the height of the plume centerline above the terrain. The concentrations estimated by SHORTZ and COMPLEX I were higher than those estimated by CTSCREEN, with CTDMPLUS predicting the lowest concentrations. In particular, the height of the lift midpoint, as well as the co.nterline of the plume, are important in the model calculation of CTDMPLUS. Under unstable conditions, the vertical dispersion plays a key role in determining ground -level concentrations. For this case, concentrations predicted by CTDMPLUS were the 'highest, whereas those predicted by SHORTZ were the lowest. Concentration distributions predicted by CTDMPLUS are quite similar to typical Gaussian distributions even on complex terrain, except for a slight shift of the plume centerline due to the of(tract of the geostrophic wind. In addition,24-hour average concentrations were estimated for comparison with results from the Valley model. Among the four models studied closely, CTDMPLUS predicted the lowest 24-hour average concentrations, but the concentrations estimated by Valley were lower than those estimated by CTDMPLUS.

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풍하중을 고려한 확률론적 운동특성 평가기법 개발에 관한 연구 (Development of a Probabilistic Approach to Predict Motion Characteristics of a Ship under Wind Loads)

  • 이상의
    • 한국항해항만학회지
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    • 제47권6호
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    • pp.315-323
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    • 2023
  • 지난 10년간, 복원력 상실로 인한 어선의 해양 사고는 지속해 증가하고 있다. 특히, 소형선박 사고의 대부분은 갑작스러운 바람이 주요 원인으로 지목되었다. 바람에 의한 소형선박의 갑작스러운 사고를 예방하기 위해서는 체계적인 분석기법 개발이 필요한 실정이다. 본 연구는 확률론적 극값 추정법을 기반으로 선박의 운동성능에 바람이 미치는 영향을 평가하는 데 그 목적이 있다. 이를 위해 운동 해석, 극값 추출, 운동 특성 분석 등의 연구를 수행하였다. 운동 해석은 Sea State 5의 파랑에서 파도, 파도와 균일 바람, 파도와 NPD풍속 모델 바람이 작용하는 3가지 조건을 적용하였다. 극값 추출은 Hysteresis 필터링 및 Peak-Valley 필터링 기법을 적용하였다. 추출된 극값을 이용하여 적합도 시험(Goodness of Fit Test)을 4가지 분포함수에 대해 수행하여 극값을 가장 잘 표현하는 최적의 분포함수를 선정하였다. 어선의 운동 특성은 3가지 주기 운동에 대하여 (Heave, Roll, Pitch)에 평가 후, 결과를 비교하였다. 선박의 운동성능 해석은 상용 솔버인 ANSYS-AQWA를 이용하였다.