• 제목/요약/키워드: WIND FLOWS

검색결과 308건 처리시간 0.027초

Aerodynamic loading of a typical low-rise building for an experimental stationary and non-Gaussian impinging jet

  • Jubayer, Chowdhury;Romanic, Djordje;Hangan, Horia
    • Wind and Structures
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    • 제28권5호
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    • pp.315-329
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    • 2019
  • Non-synoptic winds have distinctive statistical properties compared to synoptic winds and can produce different wind loads on buildings and structures. The current study uses the new capabilities of the WindEEE Dome at Western University to replicate a stationary non-Gaussian wind event recorded at the Port of La Spezia in Italy. These stationary non-Gaussian wind events are also known as intermediate wind events as they differ from non-stationary non-Gaussian events (e.g., downbursts) as well as stationary Gaussian events (e.g., atmospheric boundary layer (ABL) flows). In the present study, the wind loads on a typical low-rise building are investigated for an intermediate wind event reproduced using a continuous radial impinging jet (IJ) at the WindEEE Dome. For the same building model, differences in wind loads between ABL and IJ are also examined. Wind loads on different surface zones on the building, as defined in the ASCE code for design loads, are also calculated and compared with the code.

해양 표면취송류(skin drift)의 라그랑쥐 측류 및 모델링 (Lagrangian observation and modelling of sea surface wind-induced drift(skin drift))

  • 이문진;강용균
    • 한국해양환경ㆍ에너지학회지
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    • 제3권2호
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    • pp.11-17
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    • 2000
  • 해양에서 해수보다 비중이 낮은 유류의 이동.확산은 해면 (0m) 유동에 따라 좌우된다. 해양에서의 유류확산에 대한 현실에 부합되는 모델 개발의 일환으로 한반도 연안역 4개 해역에서 해양 표면 취송류 (skin drift) 추정에 대한 연구를 수행하였다. 본 연구에서는 해면과 수면하 1.5m의 유동을 동시 관측하여 둘간의 차이로서 바람에 의한 해양표면 취송류를 추정하였다. 표면취송류 유속의 평균 크기는 바람의 2.9% 였으며, 풍향에 대한 표면취송류 편향의 평균치는 바람의 오른쪽 18.6° 였다. 관측 결과는 표면취송류의 모델링에 활용하였다. 모델링에서는 바람에 따른 표면 취송류의 공간적 변동을 재현하였으며, 관측된 결과와 비교하여 검증하였다.

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풍력자원 평가를 위한 바람자료 동화 특성 평가 (Investigation of the Assimilated Surface Wind Characteristics for the Evaluation of Wind Resources)

  • 이화운;김민정;김동혁;김현구;이순환
    • 한국대기환경학회지
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    • 제25권1호
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    • pp.1-14
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    • 2009
  • Wind energy has been recognized as one of the most important and fastest growing energy resources without emission of air pollutant. Thus, it is necessary to predict wind speed and direction accurately both in time and space toward the efficient usage of wind energy. Numerical simulation experiments using the Fifth-Generation Mesoscale Model (MM5) are carried out to clarify the impact of surface observation data assimilation on the estimation of wind energy resources. The EXP_Radius run was designed with respect to the radius of influence in the Four-Dimensional Data Assimilation (FDDA), and the EXP_Impact run was made by changing the nudging coefficient that determines the relative magnitude of the nudging term. The simulation period covers a clear-sky event on 3 - 5 June 2007 and another is on 2 - 4 December 2006. It is found that the simulated results are very sensitive to the radius of influence and nudging parameters in the FDDA. The further analysis of the results shows that the impact of the radius of influence tends to be stronger in weak synoptic flow episode than that in strong synoptic flows episode. The nudging factor is also sensitive to the intensity of the synoptic flows.

CFD 모델을 이용한 건물군 주변의 흐름 특성 연구 (A Study on the Characteristics of Flows around Building Groups Using a CFD Model)

  • 이한경;김재진;이영곤
    • 대기
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    • 제25권3호
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    • pp.501-510
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    • 2015
  • In this study, the characteristics of flows around building groups are investigated using a computational fluid dynamics (CFD) model. For this, building groups with different volumetric ratios in a fixed area are considered. As the volumetric ratio of the building group increases, the region affected by the building group is widened. However, the wind-speed reduced area rather decreases with the volumetric ratio near the ground bottom (z ${\lesssim}$ 0.7H, here, H is the height of the building group) and, above 0.7H, it increases. As the volumetric ratio decreases (that is, space between buildings was widened), the size of recirculation region decreases but flow recovery is delayed, resulting in the wider wind-speed reduced area. The increase in the volumetric ratio results in larger drag force on the flow above the roof level, consequently reducing wind speed above the roof level. However, above z ${\gtrsim}$ 1.7H, wind speed increases with the volumetric ratio for satisfying mass conservation, resultantly increasing turbulent kinetic energy there. Inside the building groups, wind speed decreased with the volumetric ratio and averaged wind speed is parameterized in terms of the volumetric ratio and background flow speed. The parameterization method is applied to producing averaged wind speed for 80 urban areas in 7 cities in Korea, showing relatively good performance.

CALMET 및 ENVI-MET를 이용한 산업단지 입지에 따른 국지 바람장 분석 (An Analysis of Local Wind Field by Location of Industrial Complex using CALMET and ENVI-MET)

  • 송동웅
    • 환경영향평가
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    • 제21권3호
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    • pp.417-429
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    • 2012
  • In this study, a diagnostic wind model, CALMET and a micrometeorological numerical model, ENVI-MET were used to analyze the wind field in and out of the site designated for the industrial complex around Buron-myeon, Wonju, Gangwon-do. The results of modeling with CALMET showed that the air flow in industrial complex was little affected by the surrounding terrain. And the result of wind field analysis with ENVI-MET showed there are turbulent air flows such as cavity and wake around structures in the industrial complex, which can cause high-air pollution. Therefore, it is necessary to design the industrial complex considering the wind path according to wind directions.

동해 해수순화 모의를 위한 회전반 실험 (Simulation of East Sea Circulation in a Laboratory Experiment of Rotating Cylindrical Container)

  • 나정열;최진영
    • 한국해양학회지
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    • 제30권1호
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    • pp.57-63
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    • 1995
  • $\beta$-효과를 포함한 원통 용기 내의 상하층유체의 하충운동을 하충수와 같은 밀도를 갖는 외부유체를 주입하여 야기시키고 상층수와 같은 유체를 유입 및 유출시켜 지형류 조절에 의한 경계면의 변형 및 이에 따른 상층운동 특성을 실험적으로 관찰하였다. 특 히 유입-유출 위치를 변경시키고 동시에 유입과 유출양을 다르게 하여 상층수에 해상 풍의 효과를 첨가하였다. 실험의 목적은 극전선 형성과 관련하여 유입-유출 경로(대만 난류의 유입-쓰가루, 쏘야 유출)를 결정짓는 외부 인자를 파악하고자 함이다. 유입, 유출양이 같은 경우 유입수의 경로는 서안에 따라 북상하다가 이안후 위도에 평행하게 유출된 반면 상층수에 해상풍의 영향을 주었을시 서안 경계류의 분기(negative curl of wind stress 효과시), 남향의 서안 경계류에 의한 유입수의 내부로 침투(positive curl of wind stress 효과시) 등의 현상을 보여준다. 한편 유입-유출의 위치를 변경 시켜 유입수의 위치를 서안경계에 두었을 시 유입수의 경로가 경계면의 지형류 조절에 의한 서안에 근접하게 북상후 유출 (negative curl), 동안에 근접하게 북상후 유출 (positive curl)의 특성을 보여준다. 북부의 반시계방향의 흐름이 유입수의 북방 한계 를 결정짓는 역할을 하고 있음도 관찰되었다.

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대기오염 확산 해석을 위한 포항지역 기상장 연구 -바람장 수치모의- (A Study of Atmospheric Field around the Pohang for Dispersion Analysis of Air Pollutants -Numerical Simulation of Wind Field-)

  • 이화운;정우식;김현구;이순환
    • 한국대기환경학회지
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    • 제20권1호
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    • pp.1-15
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    • 2004
  • Sea/land circulation system is a representative mesoscale local circulation system in coastal area. In this study, wind fields around coastal area. Pohang, which is affected by this system was investigated and its detailed characteristic analysis was carried out. The following can be found out from the numerical simulation. Generally, at nighttime mountain winds prevail and land breeze toward the coastal area was well simulated During daytime, valley wind and sea breeze was simulated in detail. Especially, as a result of analyzing the land breeze path, it could be found along the coastline as it flows out through low land coastal area. In order to investigate the accuracy of model results. wind speed, temperature and wind direction of continuous typical sea/land breeze occurrence day was compared with observation data. Analyzing the characteristics of local circulation system was very hard because of horizontally sparse observation data but from the above result, a numerical simulation using RAMS, which satisfies the spatial high resolution, will provide more accurate results.

복잡한 지형내 오염물질의 대기확산 풍동실험: I. 산지지형에서의 확산 (Wind Tunnel Experiments for Studying Atmospheric Dispersion in the Complex Terrain I.Dispersion in a mountainous Area)

  • 경남호;김영성;손재익
    • 한국대기환경학회지
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    • 제8권3호
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    • pp.169-178
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    • 1992
  • Dispersion of pollutant in a mountainous area is simulated in a wind tunnel. In the northwest side of the terrain model, the sea level is assumed. Wind from the sea initially confronts hills along the shoreline, a line of large buildings next, and finally a valley between high mountains in the south and in the east. In the northwest wind conditions, severe flow separation occurs in the lee side of hills, even beyond the building area. Pollutant from the buildings is trapped in this region and its concentration is the highest. In the west wind conditions, pollutant from the buildings flows along the hills aslant the main wind direction in this case. Since large valley is located in the downstream, pollutant tends to disperse along the valley.

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종횡비 변화에 따른 사각주형 구조물주위의 풍압계수 결정 (Determination of Wind Pressure Coefficients around Prismatic Structures with Different Aspect Ratios)

  • 서상호;이광열;유상신;노형운
    • 설비공학논문집
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    • 제7권1호
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    • pp.52-62
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    • 1995
  • The purpose of this study is to determine the wind pressure coefficients around prismatic structures with different aspect ratios. Air flows around a model of prismatic shape are investigated experimentally in the wind tunnel and simulated using finite volume method. Pressure distributions and the corresponding pressure coefficients are calculated from the experimental and numerical results. The effects of aspect ratios on the pressure coefficients are discussed extensively. The numerical results are compared with those of experiments. The simulated and experimental results for average wind pressure coefficients are considerably lower than those defined in the Korean Architectural Standard Code.

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Non-uniform wind environment in mountainous terrain and aerostatic stability of a bridge

  • Chen, Xingyu;Guo, Junjie;Tang, Haojun;Li, Yongle;Wang, Lei
    • Wind and Structures
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    • 제30권6호
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    • pp.649-662
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    • 2020
  • The existence of a dam has potential effects on the surrounding wind environment especially when it is located in mountainous areas. In this situation, the long-span bridge over the reservoir can easily be exposed to non-uniform incoming flows, affecting its wind-resistance performance. This paper presents a study on the aerostatic stability of such a bridge. Wind tunnel tests were first carried out to investigate the wind environment above a mountainous reservoir. The results show that the angle of attack and the wind speed along the bridge axis show obvious non-uniform characteristics, which is related to the inflow direction. When winds come from the south where the river is winding, the angle of attack varies along the span direction significantly. The finite element model for the bridge was established using ANSYS software, and effects of non-uniform wind loads on the aerostatic stability were computed. Non-uniform angle of attack and wind speed are unfavorable to the aerostatic stability of the bridge, especially the former. When the combined action of non-uniform angle of attack and wind speed is considered, the critical wind speed of aerostatic instability is further reduced. Moreover, the aerostatic stability of the bridge is closely related to the dam height.