• 제목/요약/키워드: wind velocity profile

검색결과 88건 처리시간 0.027초

A compensation method for the scaling effects in the simulation of a downburst-generated wind-wave field

  • Haiwei Xu;Tong Zheng;Yong Chen;Wenjuan Lou;Guohui Shen
    • Wind and Structures
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    • 제38권4호
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    • pp.261-275
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    • 2024
  • Before performing an experimental study on the downburst-generated wave, it is necessary to examine the scale effects and corresponding corrections or compensations. Analysis of similarity is conducted to conclude the non-dimensional force ratios that account for the dynamic similarity in the interaction of downburst with wave between the prototype and the scale model, along with the corresponding scale factors. The fractional volume of fluid (VOF) method in association with the impinging jet model is employed to explore the characteristics of the downburst-generated wave numerically, and the validity of the proposed scaling method is verified. The study shows that the location of the maximum radial wind velocity in a downburst-wave field is a little higher than that identified in a downburst over the land, which might be attributed to the presence of the wave which changes the roughness of the underlying surface of the downburst. The impinging airflow would generate a concavity in the free surface of the water around the stagnation point of the downburst, with a diameter of about two times the jet diameter (Djet). The maximum wave height appears at the location of 1.5Djet from the stagnation point. Reynolds number has an insignificant influence on the scale effects, in accordance with the numerical investigation of the 30 scale models with the Reynolds number varying from 3.85 × 104 to 7.30 × 109. The ratio of the inertial force of air to the gravitational force of water, which is denoted by G, is found to be the most significant factor that would affect the interaction of downburst with wave. For the correction or compensation of the scale effects, fitting curves for the measures of the downburst-wave field (e.g., wind profile, significant wave height), along with the corresponding equations, are presented as a function of the parameter G.

온실의 풍압력 산정을 위한 풍속의 수직분포 분석 (Analysis of Wind Velocity Profile for Calculation of Wind Pressure on Greenhouse)

  • 정승현;이종원;이시영;이현우
    • 생물환경조절학회지
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    • 제24권3호
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    • pp.135-146
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    • 2015
  • 본 연구는 온실에 작용하는 풍하중 산정을 위한 설계 풍속을 결정하는데 필요한 자료를 제공하기 위하여 10m 이하 높이에서의 풍속을 측정하여 풍속고도분포지수를 산정하고 변화를 분석하였다. 고도에 따른 풍속분포함수를 결정하기 위한 풍속고도분포지수를 계산하기 위해서는 $5m{\cdot}s^{-1}$ 이상의 풍속을 사용하는 것이 타당하다고 판단된다. 농촌 개활지인 부안지역의 고도에 따른 풍속변화는 지표면으로부터 풍속이 지수함수로 증가하는 우리나라의 RDC 기준과 일본의 JGHA 기준과 잘 일치하였고 풍속고도분포지수도 0.26으로 기준들에서 제시된 0.25와 거의 동일한 값을 나타내었다. 반면 군위지역의 경우는 풍속고도분포지수가 0.06으로 산정되어 지표면조도가 클수록 풍속고도분포지수가 증가하는 일반적인 변화 경향과는 반대로 나타났다. 이는 타워가 주변지대보다 약 2m 가량 더 높은 위치에 설치되었기 때문에 유선의 급격한 변화에 의한 것으로 판단된다. 따라서 일반적으로 농촌 개활지에 설치되는 온실의 설계를 위해 적용할 풍속고도분포로는 우리나라의 RDC기준과 일본의 JGHA기준에서 제시한 풍속고도분포가 가장 타당한 것으로 사료된다. 부안의 경우 오전 7시 경부터 풍속고도 분포지수가 감소하다가 오후 3시경에 최소가 된 후 다시 증가하여 24시경에 일정해지는 것으로 나타나 시간에 따른 풍속고도분포지수의 일반적인 변화경향과 잘 일치하였다. 부안지역은 형상변수가 1.51로 나타나 간척지인 부안지역의 풍속특성이 제주도 연안지역과 유사한 풍속특성을 가지고 있음을 확인하였다.

선형 터빈 케스케이드 통로에서의 3차원 유동 특성 (Three-Dimensional Flow Characteristics in a Linear Turbine Cascade Passage)

  • 차봉준;이상우;이대성
    • 대한기계학회논문집
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    • 제17권12호
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    • pp.3148-3165
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    • 1993
  • A cascade wind tunnel test for a turbine nozzle, which was designed for a small turbo jet engine in a previous study, has been conducted to evaluate its aerodynamic performance and losses. The large-scale blades were based on the mid-span profile of the nozzle. Oil film flow structure, and then 3-dimensional velocity components were measured in the flow passage with a 5-hold pressure probe, in addition to turbulent intensities at mid-span of cascade exit using a hot-wire anemometer. From this study, 3-dimensional growth of horseshoe and passage vortices in the downstream direction was clearly understood with near-wall flow phenomena. In addition, secondary flow and losses associated with the blade configuration were obtained in detail.

취송류의 해석위와 (x-$\sigma$) 수치모형과의 비교 (Comparison of an Analytic Solution of Wind-driven Current and all (x-$\sigma$) Numerical Model)

  • 이종찬;최병호
    • 한국해안해양공학회지
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    • 제4권4호
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    • pp.208-218
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    • 1992
  • 1차원 폐쇄형 수노에서 바람에 의해 발생되는 흐름에 대해 수면구배와 유속의 수직구조를 제시하는 해석해를 정상상태 하에서 유도하였다. 해석해는 저면의 경계조건으로 저면마찰응력 $ au$$_{b}$를 부여하는 가정하에 유도되었으며, 연직 운동양 확산계수 $ extsc{k}$$_{M}$이 수심에 무관한 상수, 수심의 1차함수 및 2차함수일 경우를 포함하며, 저면류속이 no-slip이라는 가정과 저면마찰응력 $\tau$$_{b}$의 매개화에 따른 관계를 제시하고 있다. 모드 분리된, $\sigma$좌표를 채택한 (x-$\sigma$) 수치모형 결과와 유도된 해석해를 비교ㆍ검토하였다. 비교된 경우는 $textsc{k}$$_{M}$이 상수, 수심의 1차 및 2차함수인 경우로써, $textsc{k}$$_{M}$이 상수일 경우는 균일 수심, 완만한 수심경사 및 비교적 급격한 수심경사를 갖는 경우에 대해 수면구배와 유속구조를 검토 하였다. $textsc{k}$$_{M}$이 수심의 1차 및 2차함수인 경우에는 $\tau$$_{b}$의 변화에 대한 유원구조를 비교ㆍ분석하였다. 비교ㆍ분석 결과 유연구조는 $textsc{k}$$_{M}$ 값 뿐만 아니라 $textsc{k}$$_{M}$의 형태에 의해서도 변하며, $\tau$$_{b}$의 간에 의해서도 변하는 것을 보이고 있으며, 계산결과는 전반적으로 해자해와 일치함을 보였다.치함을 보였다.보였다.치함을 보였다.

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과도 액정 기법을 이용한 와동발생기 하류의 유동장 및 열전달 측정 (Detailed Measurement of Flow and Heat Transfer Downstream of Rectanglar Vortex Generators Using a Transient Liquid Crystal Technique)

  • 홍철현;양장식;이기백
    • 대한기계학회논문집B
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    • 제27권11호
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    • pp.1618-1629
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    • 2003
  • The effects of the interaction between flow field and heat transfer caused by the longitudinal vortices are experimentally investigated using a five hole probe and a transient liquid crystal technique. The test facility consists of a wind tunnel with vortex generators protruding from a bottom surface and a mesh heater. In order to control the strength of the longitudinal vortices, the angle of attack of vortex generators used in the present experiment is 20$^{\circ}$, and the spacing between the vortex generators is 25mm. The height and cord length of the vortex generator is 20mm and 50mm, respectively. Three-component mean velocity measurements are made using a f-hole probe system, and the surface temperature distribution is measured by the hue capturing method using a transient liquid crystal technique. The transient liquid crystal technique in measuring heat transfer has become one of the most effective ways in determining the full surface distributions of heat transfer coefficients. The key point of this technique is to convert the inlet flow temperature into an exponential temperature profile using the mesh heater set up in the wind tunnel. The conclusions obtained in the present experiment are as follows: The two maximum heat transfer values exist over the whole domain, and as the longitudinal vortices move to the farther downstream region, these peak values show the decreasing trends. These trends are also observed in the experimental results of other researchers to have used the uniform heat flux method.

지열을 이용한 공조외기부하저감 시스템에 관한 연구 -지하피트 공간 내의 개구부 형상이 시스템의 열적 특성 및 기류성상에 미치는 영향- (Study on Fresh Air Load Reduction System by Using Geothermal Energy - Effect on Thermal Characteristic arid Air Pattern of System by Opening Configuration -)

  • 손원득;이성
    • 설비공학논문집
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    • 제16권11호
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    • pp.1092-1100
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    • 2004
  • This paper presents the effect of opening configuration on the thermal behavior and air pattern of earth tube system. The earth tube system is a fresh air load reduction system by using underground double floor space for air-conditioning. In order to analyze the effect of opening configuration on thermal performance of this system and air pattern in underground double floor space quantitatively, we used a model dealing with tree-dimensional profile of wind velocity and temperature in underground double floor space. In conclusion, it is confirmed that heat exchange of a fresh air is mainly performed with upper and lower wall in underground double floor space, and that heat exchange area increased by installing the opening near the wall.

Water quality big data analysis of the river basin with artificial intelligence ADV monitoring

  • Chen, ZY;Meng, Yahui;Wang, Ruei-yuan;Chen, Timothy
    • Membrane and Water Treatment
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    • 제13권5호
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    • pp.219-225
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    • 2022
  • 5th Assessment Report of the Intergovernmental Panel on Climate Change Weather (AR5) predicts that recent severe hydrological events will affect the quality of water and increase water pollution. To analyze changes in water quality due to future climate change, input data (precipitation, average temperature, relative humidity, average wind speed, and solar radiation) were compiled into a representative concentration curve (RC), defined using 8.5. AR5 and future use are calculated based on land use. Semi-distributed emission model Calculate emissions for each target period. Meteorological factors affecting water quality (precipitation, temperature, and flow) were input into a multiple linear regression (MLR) model and an artificial neural network (ANN) to analyze the data. Extensive experimental studies of flow properties have been carried out. In addition, an Acoustic Doppler Velocity (ADV) device was used to monitor the flow of a large open channel connection in a wastewater treatment plant in Ho Chi Minh City. Observations were made along different streams at different locations and at different depths. Analysis of measurement data shows average speed profile, aspect ratio, vertical position Measure, and ratio the vertical to bottom distance for maximum speed and water depth. This result indicates that the transport effect of the compound was considered when preparing the hazard analysis.

Polar Mesospheric Summer Echo Characteristics in Magnetic Local Time and Height Profiles

  • Young-Sook Lee;Ram Singh;Geonhwa Jee;Young-Sil Kwak;Yong Ha Kim
    • Journal of Astronomy and Space Sciences
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    • 제40권3호
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    • pp.101-111
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    • 2023
  • We conducted a statistical study of polar mesospheric summer echoes (PMSEs) in relation to magnetic local time (MLT), considering the geomagnetic conditions using the K-index (or K). Additionally, we performed a case study to examine the velocity profile, specifically for high velocities (≥ ~100 m/s) varying with high temporal resolution at high K-index values. This study utilized the PMSE data obtained from the mesosphere-stratosphere-troposphere radar located in Esrange, Sweden (63.7°N, 21°E). The change in K-index in terms of MLT was high (K ≥ 4) from 23 to 04 MLT, estimated for the time PMSE was present. During the near-midnight period (0-4 MLT), both PMSE occurrence and signal-to-noise ratio (SNR) displayed an asymmetric structure with upper curves for K ≥ 3 and lower curves for K < 3. Furthermore, the occurrence of high velocities peaked at 3-4 MLT for K ≥ 3. From case studies focusing on the 0-3 MLT period, we observed persistent eastward-biased high velocities (≥ 200 m/s) prevailing for ~18 min. These high velocities were accompanied with the systematic motion of profiles at 85-88 km, including large shear formation. Importantly, the rapid variations observed in velocity could not be attributed to neutral wind effects. The present findings suggest a strong substorm influence on PMSE, especially in the midnight and early dawn sectors. The large zonal drift observed in PMSE were potentially energized by local electromagnetic fields or the global convection field induced by the electron precipitation during substorms.