• 한국농림기상학회지
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• 제24권2호
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• pp.63-77
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• 2022

농업기상재해 조기경보시스템에서 모의되는 농장 규모 풍속 예측자료의 추정오차를 개선하기 위해, 농촌진흥청 농업기상관측망의 2020년 1~12월 풍속 관측자료와 해당 지점에 대한 조기경보시스템 모의 풍속을 이용하여, 87지점 일 8시간대(00, 03, 06 … 21시) 각각 풍속 추정오차를 종속변수로, 추정풍속을 독립변수로 하는 일차 회귀식(Y=aX+b)을 도출하였다. 상관계수가 0.5를 초과하였을 때는 회귀식을 풍속 보정식으로 활용하고, 상관계수가 0.5 이하일 때는 회귀식 대신 해당 지점 및 시간대의 ME를 보정값으로 대체하였다. 풍속 모형을 전국적으로 적용할 수 있도록 87지점×8개 시간의 회귀계수 a와 b, 상관계수 R과 ME 값으로 거리역산가중법으로 공간내삽하여 250m 격자해상도의 분포도를 제작하였다. 모형의 검증을 위하여 회귀계수 a와 b, 상관계수 R과 ME 공간내삽 분포도로 부터 농산촌 지역 13개 기상관측지점의 격자값을 추출하고, 13곳의 2019년 1~12월의 조기경보시스템 모의 풍속(00, 03, 06 … 21시)를 보정한 다음, 기존 추정 풍속과 함께 추정오차를 비교하였다. 검증 지점 풍속의 평균 ME는 0.68m/s에서 보정 후 0.45m/s로 감소하였으며, 평균 RMSE는 1.30m/s에서 1.05m/s로 감소하였다. 조기경보시스템의 풍속은 전 시간대에서 모두 과대 추정되고 있는데, 보정 기법을 적용한 후에는 15시 경을 제외하고 모두 과대추정 경향이 감소하여 ME가 약 33%, RMSE는 19.2% 더 개선되었다. 농업기상재해 조기경보시스템에서 농작물의 풍해 위험 판단은 일 8회의 풍속 평균값으로부터 도출된 일 최대순간풍속을 기반으로 하는데, 풍속의 과대모의 현상을 개선하여 강풍 위험 경보의 오보를 감소시킬 것으로 기대된다.

• 대한기계학회:학술대회논문집
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• 대한기계학회 2000년도 춘계학술대회논문집B
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• pp.740-745
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• 2000

Effects of porous fences on the wind erosion of sand particles from a triangular pile were investigated experimentally. The porous fence and sand pile were installed in a simulated atmospheric boundary layer. The mean velocity and turbulent intensity profiles measured at the sand pile location were well fitted to the atmospheric boundary layer over the open terrain. Particle motion was visualized to see the motion of windblown sand particles qualitatively. In addition, the threshold velocity were measured using a light sensitive video camera with varying the fence porosity ${\varepsilon}$. As a result, various types of particle motion were observed according to the fence porosity. The porous wind fence having porosity ${\varepsilon}=30%$ was revealed to have the maximum threshold velocity, indicating good shelter effect for abating windblown dust particles.

• Wind and Structures
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• 제5권6호
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• pp.515-526
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• 2002

The wind flow over two-dimensional sinusoidal hilly obstacles with slope (the ratio of height to half width) of 0.5 has been investigated experimentally and numerically. Experiments for single and double sinusoidal hill models were carried out in a subsonic wind tunnel. The mean velocity profiles, turbulence statistics, and surface pressure distributions were measured at the Reynolds number based on the obstacle height(h=40 mm) of $2.6{\times}10^4$. The reattachment points behind the obstacles were determined using the oil-ink dot and tuft methods. The smoke-wire method was employed to visualize the flow structure qualitatively. The finite-volume-method and the SIMPLE-C algorithm with an orthogonal body-fitted grid were used for numerical simulation. Comparison of mean velocity profiles between the experiments and the numerical simulation shows a good agreement except for the separation region, however, the surface pressure data show almost similar distributions.

• 한국기계가공학회지
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• 제11권2호
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• pp.118-124
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• 2012

The simulation of the air flow over models in atmospheric boundary layer wind tunnel is a research region based on advanced scientific technologies imposed by the necessity of studying the turbulent fluid dynamics in the proximity of the Earth's surface. In this study, the atmospheric boundary layer wind tunnel of UCD is used, the mean velocities are measured by augmentation devices such as roughness blocks and spires. The experimental results of mean velocity profile are well fitted with the value of power law.

• Wind and Structures
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• 제14권1호
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• pp.15-34
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• 2011

Three wind-tunnel simulations of the atmospheric boundary layer (ABL) flow in suburban country exposure were generated for length scale factors 1:400, 1:250 and 1:220 to investigate scale effects in wind-tunnel simulations of the suburban ABL, to address recommended wind characteristics for suburban exposures reported in international standards, and to test redesigned experimental hardware. Investigated parameters are mean velocity, turbulence intensity, turbulent Reynolds shear stress, integral length scale of turbulence and power spectral density of velocity fluctuations. Experimental results indicate it is possible to reproduce suburban natural winds in the wind tunnel at different length scales without significant influence of the simulation length scale on airflow characteristics. However, in the wind tunnel it was not possible to reproduce two characteristic phenomena observed in full-scale: dependence of integral length scales on reference wind velocity and a linear increase in integral length scales with height. Furthermore, in international standards there is a considerable scatter of recommended values for suburban wind characteristics. In particular, recommended integral length scales in ESDU 85020 (1985) are significantly larger than in other international standards. Truncated vortex generators applied in this study proved to be successful in part-depth suburban ABL wind-tunnel simulation that yield a novel methodology in studies on wind effects on structures and air pollution dispersion.

• 한국환경보건학회지
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• 제16권2호
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• pp.21-29
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• 1990

This study investigated to find out the patterns of the wind direction and wind speeds influenced by concentration of sulfur dioxide in Taegu area for a year in 1988.The results were as follows: Prevailing wind by months where easterly wind from May to September and the other months were westerly and / or west-north-westerly wind. Condition of calm was the most at December(8.6%). Prevailing wind by seasons were westerly and easterly wind in spring and autumn, east-north-easterly and/or west-south wind in summer, the other hand, west-south-westerly and/or west-north-westerly wind in winter. Mean concentration of sulfur dioxide (SO$_{2}$) at each sites were influenced by prevailing wind and location of industrial estates. Mean wind speeds by times were the highest at the before and after 4 P.M.,but the lowest at the before and after 5 A.M. Average wind velocity were highest at Spring (3.38m / sec).

• 한국방재안전학회논문집
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• 제6권2호
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• pp.49-56
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• 2013

본 논문에서는 재난변동풍하중을 받는 고층건물의 예비설계과정에서 필요로 하는 자료를 얻기 위하여 경계층풍동 실험을 실시했다. 먼저 본 실험에 앞서 경계층풍동내의 자연풍을 얻기 위하여 확산장치를 이용했고, 이로부터 평균풍속 수직분포, 난류강도, 파워스펙트럼으로 입증했으며, 이 후 변장비 1:2 강체모형을 이용 경계층풍동실험을 실시한 결과로부터 다음과 같은 결론을 얻을 수 있었다. 1. 경계층풍동에서의 평균풍속 및 난류강도의 수직분포가 자연풍과 같이 잘 실현되었다. 2. 변동풍속 스펙트럼은 Von Karman spectrum과 비교한 결과 잘 일치했다. 3. 변동압력 스펙트럼에서 풍상면의 피크분포는 0.01-0.1 Hz영역에서 발생했고, 풍후면은 0.1 Hz영역에서 발생했다. 4. 자기상관계수는 재난변동풍하중의 작용시간이 증가하면 정성확률과정으로 분포하는 사실을 알 수 있었다.

• 대한기계학회논문집B
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• 제24권9호
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• pp.1175-1184
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• 2000

Effects of porous wind fences on the wind erosion of particles from a triangular sand pile were investigated experimentally. The porous fence and sand pile were installed in a simulated atmospheric boundary layer. The mean velocity and turbulent intensity profiles measured at the sand pile location were well fitted to the atmospheric boundary layer over the open terrain. Flow visualization was carried out to investigate the motion of windblown sand particles qualitatively. In addition, the threshold velocity were measured using a light sensitive video camera with varying the particle size, fence porosity $\varepsilon$ and the height of sand pile. As a result, various types of particle motion were observed according to the fence porosity. The porous wind fence having porosity $\varepsilon$=30% was revealed to have the maximum threshold velocity, indicating good shelter effect for abating windblown dust particles. With increasing the sand particle diamter, the threshold velocity was also increased. When the height of sand pile is lower than the fence height, threshold velocity is enhanced.

• Wind and Structures
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• 제28권6호
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• pp.381-388
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• 2019

This paper described the application of Geospatial Analysis in determining mean wind speed, $V_h$ for wind load calculation imposed to electrical transmission tower structural design. The basic wind speed data on available station obtained from Malaysian Meteorology Department is adjusted by considering terrain and ground roughness factor. The correlation between basic wind speed, terrain factor and ground roughness stated in EN-50341-1 is used to obtain the $V_h$ for overhead transmission line elements 50 m above ground. Terrain factor, $k_r$ and ground roughness, $z_0$ in this study are presented by land use types of study area. Wind load is then calculated by using equation stated in design code EN-50341-1 by using the adjusted mean wind speed. Scatter plots of $V_h$ for different $k_r$and $z_0$ are presented in this paper to see the effect of these parameters to the value of $V_h$. Geospatial analysis is used to represent the model of $V_h$. This model can be used to determine possible area that will subject to wind load which severe to the stability of transmission tower and transmission line.

• Wind and Structures
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• 제5권2_3_4호
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• pp.165-176
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• 2002

Results of measurements of surface pressure and of velocity field made on a full-scale 6 m cube in natural wind are reported. Comparisons are made with results from boundary-layer wind-tunnel studies reported in the literature. Two flow angles are reported; flow normal to a face of the cube (the $0^{\circ}$ case) and flow at $45^{\circ}$. In most comparisons, the spread of wind-tunnel results of pressure measurements spans the full-scale measurements. The exception to this is for the $0^{\circ}$ case where the roof and side-wall pressures at full-scale are more negative, and as a result of this the leeward wall pressures are also lower. The cause of this difference is postulated to be a Reynolds Number scale effect that affects flow reattachment. Measurements of velocity in the vicinity of the cube have been used to define the mean reattachment point on the roof centre line for the $0^{\circ}$ case, and the ground level reattachment point behind the cube for both $0^{\circ}$ and $45^{\circ}$ flow. Comparisons are reported with another full-scale experiment and also with wind-tunnel experiments that indicate a possible dependency on turbulence levels in the approach flow.