• 한국군사과학기술학회지
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• 제18권4호
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• pp.469-477
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• 2015

In this study, the characteristics of main wind direction, vertical temperature and wind speed profile near the Moseulpo airfield for HALE UAV(High Altitude Long Endurance Unmaned Aerial Vehicle) is investigated. The results are summarized as follows, main wind direction is governed by air mass according to season and local wind such as land-sea breeze. The directions of landing and take-off of HALE UAV will be selected as the south-east direction in June ~ August, north-west direction in October ~ March, and south-east direction at daytime in April ~ May, September. Annual variation of temperature at 100 hPa showed that temperature in summer season is lower than winter season. On the other hands, wind speed at 250 hPa in winter season is higher than summer season. The threshold values of temperature and wind speed for HALE UAV flight are $-75^{\circ}C$ and $90ms^{-1}$, which were determined by 5 % frequency value($1.96{\sigma}$), respectively.

• 한국산림과학회지
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• 제100권2호
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• pp.246-255
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• 2011

본 연구는 2010년 9월 2일 강한 바람으로 우리나라 중부 지방에 영향을 미친 제7호 태풍 곤파스로 인해 피해를 입은 홍릉수목원 내 풍도목을 대상으로 풍도목의 특징, 임내 외 풍향 및 풍속의 특징을 구명하고자 실시하였다. 풍도목은 피해 유형에 따라 바람에 쓰러진 나무, 기울어진 나무, 수간이 부러진 나무 등 크게 세 가지로 구분하여 조사하였다. 바람이 불기 시작한 9월 2일 04시부터 바람이 완전히 멎은 12시까지의 풍속을 분석한 결과, 임내 평균풍속과 순간최대풍속은 각각 1.4 m/s와 3.5 m/s 이었으며, 06시 10분 임내 평균풍속과 순간최대풍속이 각각 3.4 m/s와 8.7 m/s로 최고치를 기록하였다. 곤파스의 피해를 받은 2010년 9월 2일과 강풍주의보가 발효되었던 과거 5일(2009년 2월 13일, 2월 20일, 4월 21일, 10월 16일, 2010년 3월 20일)의 평균풍속 차이와 파동을 비교 분석한 결과, 풍도목 발생 원인은 바람의 세기보다는 단위시간당 바람파동횟수와 관련이 깊은 것으로 사료된다. 풍향 분석 결과 임내 평균풍향은 방위각 $112.5^{\circ}{\sim}180^{\circ}$(ESE-SE-SSE-S)와 $247.5^{\circ}$(WSW) 방향에서 불어 들어왔으며, 임내 외 순간 최대풍향 모두 방위각 $157.5^{\circ}$(SSE) 방향에서 강하게 불어 들어왔다. 풍도목의 도복 방향과 위치를 분석한 결과 84.0%의 풍도목이 방위각 $270^{\circ}{\sim}22.5^{\circ}$(W-WNW-NW-NNW-N-NNE) 방향으로 쓰러졌으며, 97.3%의 풍도목이 완경사지(경사 $15^{\circ}$ 미만)와 경사지(경사 $15^{\circ}{\sim}20^{\circ}$)에서 발생하였다. 풍도목 중 침엽수가 45.3%를 차지했고, 활엽수가 54.7%를 차지하였으나, 임상별로 보면 풍도목은 활엽수림보다 침엽수림과 혼효림에서 주로 발생한 것으로 나타났다.

• 센서학회지
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• 제22권4호
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• pp.292-296
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• 2013

The ultrasonic wind sensor that pass through the air, beating the delivery of ultrasonic wind speed increases or decreases by the physical characteristics of the wind speed and the direction of the sensor, the transmission and reception of ultrasonic time difference measured by a two-axis vector wind and wind speed measured by calculating a device that converts the digital signal is Anemometer and wind direction meteorological facilities management, management of the ship sail used for various purposes, including, but used the existing 3-cup (mechanical) anemometer wind rotor caused by mechanical wear parts replacement due to the short-term, the reliability of the product is low, parts replacement, and according to the characteristics caused the car, there is a problem in high maintenance costs. In addition, because the bearings use of the marine environment and the cryogenic environment was constrained. In this study, the excellent long-term reliability, using ultrasonic-type environment that is not constrained to produce wind anemometer located $90^{\circ}$ conformal road using four piezoelectric sensors were fabricated structures, the piezoelectric oscillator circuit produces a rash and receiving transmit and receive speeds the car through the two-axis vector calculation to measure wind velocity processor firmware programming, and its characteristics were tested.

• Wind and Structures
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• 제38권4호
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• pp.277-293
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• 2024

The recorded thunderstorm winds at a point contain tri-directional components. The probabilistic characteristics of such recorded winds in terms of instantaneous mean wind speed and direction, and the probability distribution and the time-frequency dependent crossed and non-crossed power spectral density functions for the high-frequency fluctuating wind components are unclear. In the present study, we analyze the recorded tri-directional thunderstorm wind components by separating the recorded winds in terms of low-frequency time-varying mean wind speed and high-frequency fluctuating wind components in the alongwind direction and two orthogonal crosswind directions. We determine the time-varying mean wind speed and direction defined by azimuth and elevation angles, and analyze the spectra of high-frequency wind components in three orthogonal directions using continuous wavelet transforms. Additionally, we evaluate the coherence between each pair of fluctuating winds. Based on the analysis results, we develop empirical spectral models and lagged coherence models for the tri-directional fluctuating wind components, and we indicate that the fluctuating wind components can be treated as Gaussian. We show how they can be used to generate time histories of the tri-directional thunderstorm winds.

• 풍력에너지저널
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• 제9권4호
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• pp.40-46
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• 2018

In this study, a three-dimensional Navier-Stokes simulation around Wido Island was performed to analyze the wake effect behind an island. A 10 m/s wind speed and pressure boundary conditions were assigned for the inflow and outflow boundary conditions, respectively. Wido Island was modeled using GIS data. A prevailing wind from the north-northwest direction was determined based on QuikSCAT satellite data. A computational domain of $40km{\times}20km{\times}5km$ covering Wido Island was applied for numerical analysis. Sixty points were specified to extract the wind speed data. A wind speed profile inside the atmospheric boundary layer was compared with a wind profile using a simple power law. It turns out that the wake effect decreases the mean wind speed by 5% more or less, which corresponds to a 14% decrease in wind energy. Thus, the installation of a meteorological mast or development of a wind farm behind Wido Island is not highly recommended.

• 풍력에너지저널
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• 제4권2호
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• pp.34-39
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• 2013

The wind resource assessment for measured wind data over 1 year by using the meteorological mast should be a prerequisite for business feasibility of the wind farm development. Even though the direction of boom mounting the wind vane and anemometer is carefully engineered to escape the interference of wakes generated from the met-mast structures, the shadow effect is not completely avoided due to seasonal winds in the Korean Peninsula. The shadow effect should be properly calibrated because it is able to distort the wind resources. In this study a calibration method is introduced for the measured wind data at Julpo in Jeonbuk Province. Each sectoral terrain conditions along the selected wind direction nearby the met-mast is investigated, and the distorted wind data due to shadow effects can be calibrated effectively. The correction factor is adopted for quantitative calibration by carrying out the WindSim analysis.

• 한국해양공학회지
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• 제21권1호
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• pp.1-6
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• 2007

While a typhoon is traveling, characteristics of its wind fields are continuously changing, producing severe changes in local water level and wave conditions, especially, when a typhoon comes into shallow water. However, there have not been many studies related to local typhoon effects, especially, considering real time changes of wind direction related to the coastal topography. In the study, the characteristics of the wind field by typhoon and topographical characteristics in shallow water are considered, as well as conditions of wave climate estimation. These are performed by the SWAN (Simulating waves nearshore) model, in order to estimate the growth of wave energy due to the wind field. It can be strongly suggested that the wave energy of theof an inner bay should be estimated when the direction of the bay entrance and the wind direction of the typhoon are identical. The result of the numerical calculations is in better agreement with the observed data than the result of the conventional estimation techniques.

• 생물환경조절학회지
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• 제23권4호
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• pp.269-280
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• 2014

To cope with increasing of vegetables and flowers consumptions, horticulture facilities have been modernized. Korea government recently announced construction plan of new greenhouse complex at reclaimed land. However wind characteristics of reclaimed land is totally different from those of inland, wind pressure on greenhouse built in reclaimed land should be carefully evaluated to secure structural safety on the greenhouse. In this study, as a first step, wind pressure coefficient and local wind pressure coefficient on even-span greenhouse were measured using wind tunnel test. ESDU was adopted to realize wind characteristics of reclaimed land such as wind and turbulence profiles. From the wind tunnel test, when wind direction was 0 degree, it was concluded that KBC2009 standard underestimated scale of wind pressure coefficients at roof area of greenhouse whereas NEN-EN2002 standard underestimated those at every surface of greenhouse. When wind direction was 90 degree, both standards did not well reflect the characteristics of wind pressure distribution. From the analysis of local wind pressure coefficients according to wind direction conditions, design of covering, glazing bar of greenhouse where large effects of the local wind pressure were estimated should be well established. Wind pressure coefficients and local wind pressure coefficients according to parts of the greenhouse were finally suggested and these results could be practically used for suggesting new design standards of greenhouse.

• 산업기술연구
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• 제29권B호
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• pp.173-180
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• 2009

Simulations using two well-known commercial codes, WAsP and WindSIM, were performed to predict the wind resources in complex terrains of Korea. The predictions from the codes were compared with the measured data. Cross predictions were performed for two closely located measurement sites. The results from WindSIM were found to be more accurate than those from WAsP. The predictions for wind velocity and direction in five different sites of complex terrain from WAsP and WindSIM were also compared. It was found that if the self prediction of the wind velocity and direction from WAsP is close to the measured wind data, the discrepancies between WAsP results and WindSIM results are also close.

• 한국지구과학회지
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• 제26권3호
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• pp.240-252
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• 2005

한반도 주변 해역의 5개 지점(덕적도, 칠발도, 거문도, 거제도, 동해 정점)에서 관측된 기상청의 해양 기상 관측 부이 자료를 이용하여 각 해역에서 바람과 파도의 관계를 분석하였다. 전반적으로는 서해 정점에서는 파도가 바람의 영향을 가장 많이 받고 남해 정점에서는 파도가 바람의 영향을 가장 적게 받으며 동해 정점에서는 그 중간이며 각 정점별 특징은 다음과 같다. 칠발도에서는 풍속이 강한 겨울철의 주 풍향인 북서방향으로 바다가 트여있고 얕은 수심에 의한 여울효과로 가장 높은 파고가 발달하며 풍향과 파향이 다른 정점에 비해서 가장 잘 일치한다. 이에 비해 덕적도는 북서방향이 황해도에 의해 막혀 있기 때문에 취송거리가 제한되어 겨울철에 충분히 발달한 파도가 생기지 않는다. 이러한 취송거리의 제한은 남해 정점에서 더 크다. 북풍이 우세한 남해의 두 정점에서는 북쪽의 육지 때문에 파도의 발달이 제한되어 바람이 강해도 파고는 거의 높아지지 않는다. 남해 정점에서는 어느 방향에서 바람이 불든지 모든 파향의 파가 고르게 유입되며 그 중 우세한 파향은 항상 동중국해에서 유입되는 방향이다. 그 방향은 거문도와 거제도에서 각각 남쪽 방향과 남서 방향이며 이 방향으로는 바람이 약할 때도 파도가 유입된다. 동해 정점에서는 수심이 깊어 파도가 크게 발달하지만 풍향과 파향이 일치하지 않는 경우가 많아 파고의 발달이 칠발도에서 보다는 낮다. 이와 같이 풍속과 더불어 풍향이 파랑발달에 중요한 이유는 풍향에 의해 취송거리가 결정되기 때문이다. 덕적도와 칠발도에서 풍향이 변하지 않고 오래 지속되는 경우를 보면 파향이 풍향과 일치하며 파고는 최대풍속 후에 최대파고가 나타나는 반응시간이 길수록 커지는 것을 볼 수 있다. 그러나 풍향과 파향이 일치하지 않는 동해 정점의 경우에서는 풍속이 크고 반응시간이 길어도 파고가 서해 정점에서와 같이 많이 높아지지는 않는다. 이상의 결과는 풍속이 클수록, 취송거리가 길수록, 지속시간이 길수록 파고가 크게 발달하는 일반적인 경향과 더불어 각 정점별로는 육지와 바다의 방향, 해저지형, 주변해역의 규모 등의 환경조건에 의해 바람에 의한 파도의 발달율이 달라지는 것을 보여준다.