• 제목/요약/키워드: strong wind speed

검색결과 311건 처리시간 0.024초

Investigation of Typhoon Wind Speed Records on Top of a Group of Buildings

  • Liu, Min;Hui, Yi;Li, Zhengnong;Yuan, Ding
    • 국제초고층학회논문집
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    • 제8권4호
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    • pp.313-324
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    • 2019
  • This paper presents the analysis of wind speeds data measured on top of three neighboring high-rise buildings close to a beach in Xiamen city, China, during Typhoon "Usagi" 2013. Wind tunnel simulation was carried out to validate the field measurement results. Turbulence intensity, turbulence integral scale, power spectrum and cross correlation of recorded wind speed were studied in details. The low frequency trend component of the typhoon speed was also discussed. The field measurement results show turbulence intensity has strong dependence to the wind speed, upwind terrain and even the relative location to the Typhoon center. The low frequency fluctuation could severely affect the characteristics of wind. Cross correlation of the measured wind speeds on different buildings also showed some dependence on the upwind terrain roughness. After typhoon made landfall, the spatial correlation of wind speeds became weak with the coherence attenuating quickly in frequency domain.

56년간 한반도 강수 및 풍속의 극값 변화 (The Variation of Extreme Values in the Precipitation and Wind Speed During 56 Years in Korea)

  • 최의수;문일주
    • 대기
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    • 제18권4호
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    • pp.397-416
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    • 2008
  • This study investigates a long-term variation of the annual extreme value for the instantaneous wind speed and the daily precipitation during 56 years (1951-2006) in Korea. Results show that there is a uptrend for both wind and precipitation extreme records, although regional trends are different from overall pattern in some places, particularly for wind speed. The estimated linear trends are 230 mm/56 yr in the daily precipitation and $15ms^{-1}$/56 yr in the maximum instantaneous wind speed. For precipitation, other indexes such as total annual precipitation, the number of extreme precipitation event, and precipitation intensity have dramatically increased as well, while there has been a clear downtrend for the number of strong wind events (> $14ms^{-1}$). It is found that the minimum surface pressure recorded during typhoon attacks in Korea tends to be decreasing, about 10 hPa/56 yr. This partly explains why the extreme values in the precipitation are increasing in Korea.

기후변화 시나리오에 근거한 한반도 미래 풍력·태양-기상자원 변동성 (Variability of Future Wind and Solar Resource Over the Korean Peninsula Based on Climate Change Scenario)

  • 변재영;김유미;최병철
    • 신재생에너지
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    • 제10권2호
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    • pp.29-39
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    • 2014
  • This study examines the future variability of surface wind speed and solar radiation based on climate change scenario over the Korean Peninsula. Climate change scenarios used in this study are RCP 4.5 and 8.5 with a 12.5 km horizontal resolution. Climate change scenario RCP 4.5 and 8.5 reproduce the general features of wind speed over the Korean Peninsula, such as strong wind speed during spring and winter and weak wind speed during summer. When compared with the values of wind speed and solar radiation of the future, they are expected to decrease current wind and solar resource map. Comparing the resource maps using RCP 4.5 and 8.5 scenarios, wind speed and solar radiation decrease with increasing greenhouse gas concentration. Meteorological resource maps of future wind and solar radiation should be improved with high resolution for the industrial application.

자갈비산 메커니즘 연구를 위한 고속철도차량 하부유동 계측 (Track Measurements of Strong Wind under High-speed Train to Investigate Ballast-flying Mechanism)

  • 권혁빈;박춘수;남성원;고태환
    • 한국정밀공학회:학술대회논문집
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    • 한국정밀공학회 2005년도 춘계학술대회 논문집
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    • pp.369-373
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    • 2005
  • To investigate the mechanism of ballast-flying phenomena by strong wind induced by high-speed trains, wind velocity in the vicinity of the track has been measured using 16-channel Kiel-probe array and detailed flow structure near the surface of the track has been analyzed. The position at which the underflow fully develop has been examined in order to assess the driving force of the turbulent flow under train and the results yields that the turbulent flow owing to the cavity of the inter-car as well as the friction force at the underbody of the train is the main reason of the strong wind under high-speed train. The preceding wind tunnel test results has been introduced to assess the probability of ballast-flying during the passage of the high-speed train by comparing the results from field-measuring. The results shows that when the G7 train as well as the KTX train runs at 300km/h, about 25m/s wind gust is induced just above the tie and the probability for small ballast under 50g to fly is about 50% when it is on the tie. If the G7 train runs at 350km/h, the wind gust just above the tie increases to 30m/s, therefore more radical countermeasure seems to be needed.

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중규모 수치모델 WRF를 이용한 북한 풍력-기상자원지도 개발 (Development of wind Map Over North Korea using the Mesoscale Model WRF)

  • 서범근;변재영;최영진
    • 대기
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    • 제21권4호
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    • pp.471-480
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    • 2011
  • This study investigates the characteristics of surface wind in North Korea using mesoscale model WRF. Hourly wind fields were simulated for one year representing mean characteristics of an 11-years period from 1998 to 2008. The simulations were performed on a nested grid from 27 km to 1 km horizontal resolution. The simulated wind map at 10 m above ground level is verified with 27 surface observations. Statistical verification skill score indicates that wind speed tends to overestimate in surface layer. The average RMSE value of the simulated wind speed is around $2.8ms^{-1}$. Wind map in North Korea showed that strong wind speed is distributed in the mountainous and western coastal region. The results of this wind mapping study contribute for the founding of wind energy potential location.

바람의 강도에 따른 강하먼지와 불용성 성분의 조성특성 (A study on bulk deposition flux of dustfall and insoluble components by the wind intensity in Busan, Korea)

  • 황용식;김유근;박종길;문덕환
    • 한국환경과학회지
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    • 제11권7호
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    • pp.651-662
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    • 2002
  • Weather elements were observed by the AWS (Automatic Weather System) and dustfall particles were collected by the modified American dust jar (wide inlet bottle type) at 4 sampling sites in Busan area from March. 1999 to February, 2000. Thirteen chemical species (Al, Ca, Cd, Cr, Cu, Fe, K, Mg, Mn, Ni, Pb, Si, and Zn) were analyzed by AAS and ICP. The purposes of this study were to estimate qualitatively various bulk deposition flux of dustfall and insoluble components by applying regional and seasonal wind intensity. Frequency of wind speed were found in order of low(1-3m/s), very low(<1m/s), medium(3-8m/s) and high(>8m/s), and annual mean had higher range at low(1-3m/s) for 56.3%. Strong negative linear correlation were observed between dustfall and wind direction (northeastern and eastern), but strong positive linear correlation were observed between dustfall and wind direction (western and northwestern) at industrial, commercial and coastal zone(p<0.05). While a negative correlation were observed between wind speed frequency of very low(<1 m/s) and dustfall, and positive correlation were observed between wind speed frequency of low(1-3m/s) and dustfall in coastal zone(p<0.05). The correlation coefficient was observed 0.556 between wind speed frequency of low(1-3m/s) and Ni by commercial zone(p<0.05). The correlation coeffcient show well-defined insoluble trace metals (Al, Ca, Cr, Cu, Fe, Pb, and Zn) and wind speed frequency of low(1-3m/s) at coastal zone, which was found significant difference(p<0.01).

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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A Review on the Building Wind Impact through On-site Monitoring in Haeundae Marine City: 2021 12th Typhoon OMAIS Case Study

  • Kim, Jongyeong;Kang, Byeonggug;Kwon, Yongju;Lee, Seungbi;Kwon, Soonchul
    • 한국해양공학회지
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    • 제35권6호
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    • pp.414-425
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    • 2021
  • Overcrowding of high-rise buildings in urban zones change the airflow pattern in the surrounding areas. This causes building wind, which adversely affects the wind environment. Building wind can generate more serious social damage under extreme weather conditions such as typhoons. In this study, to analyze the wind speed and wind speed ratio quantitatively, we installed five anemometers in Haeundae, where high-rise buildings are dense, and conducted on-site monitoring in the event of typhoon OMAIS to determine the characteristics of wind over skyscraper towers surround the other buildings. At point M-2, where the strongest wind speed was measured, the maximum average wind speed in 1 min was observed to be 28.99 m/s, which was 1.7 times stronger than that at the ocean observatory, of 17.0 m/s, at the same time. Furthermore, when the wind speed at the ocean observatory was 8.2 m/s, a strong wind speed of 24 m/s was blowing at point M-2, and the wind speed ratio compared to that at the ocean observatory was 2.92. It is judged that winds 2-3 times stronger than those at the surrounding areas can be induced under certain conditions due to the building wind effect. To verify the degree of wind speed, we introduced the Beaufort wind scale. The Beaufort numbers of wind speed data for the ocean observatory were mostly distributed from 2 to 6, and the maximum value was 8; however, for the observation point, values from 9 to 11 were observed. Through this study, it was possible to determine the characteristics of the wind environment in the area around high-rise buildings due to the building wind effect.

해상교량의 풍하중을 고려한 제한 속도 도출 방안 (A Study on Variable Speed Limit Considering Wind Resistance on Off-Shore Bridge)

  • 이선하;강희찬
    • 대한교통학회지
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    • 제22권5호
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    • pp.75-87
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    • 2004
  • 우리나라 해안지역은 강풍의 빈도가 높고 세기도 크지만 아직까지 바람을 고려한 적정속도를 안내하는 시스템은 전무한 상태이다. 강풍이 부는 곳에서의 무리한 주행은 핸들 조작의 어려움으로 인한 사고 위험과 풍속을 고려하지 않은 과속으로 인한 전복사고 등의 위험이 크다. 이러한 측면에서 바람 잦은 곳 중 주요지점에 기상정보센서(WIS:Weather Information Sensor)를 설치하고 이로부터 실시간으로 측정된 기상정보를 바탕으로 차량의 구동력과 주행저항의 크기를 극대화하는 적정속도를 VMS를 통하여 제공하는 방안이 필요하다. 목포시에 건설예정인 목포대교를 대상으로 풍속별 적정 속도를 산출한 결과, 연중 평균 풍향인 남풍일 경우 교량의 입지(정남-북)에 따라 남측으로 주행하는 차량에 대하여 풍속이 8m/h이상일 경우에는 평상시와 달리 돌풍을 대비한 여유구동력이 큰 60km/h의 속도를 안내해 주는 것이 바람직 한 것으로 나타났다. 또한 2003년도에 발생한 태풍 매미 시 목포시의 풍속인 18m/s 일 경우 시속 40km/s에서의 주행저항은 1131N으로써, 이미 변속 4단에서의 구동력(약 1054N)으로는 극복할 수 없으므로 3단 이하에서 변속을 하여야 하며, 이때의 적정속도는 주행저항과 구동력간의 차이가 가장 크게 발생하는 40km/h인 것으로 분석되었다.

경상북도에서 태풍에 의한 영향과 유형별 진로 특성 분석 (Influence of Typhoon Landfall and Its Track Characteristics in Gyeongsangbuk-do)

  • 박두선;허창회;황종국
    • 대기
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    • 제18권4호
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    • pp.525-532
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    • 2008
  • This study has examined influences of tropical cyclone (TC) landfalls on the Gyoengsangbuk-do region, located in southeast of Korea, for the period 1978-2006. This region is known as one of major pass ways of landfalling TCs, and has many cultural properties including Bulguksa, Sukgulam, etc. Thus the influences caused by TCs (i.e., TC damages) may be larger than elsewhere in the nation. Here, TC influence is defined as the cases of strong instantaneous wind speed (${\geq}20ms^{-1}$) and heavy rainfall (${\geq}100mmday^{-1}$) at each station. This study analyzed long-term trends ofTC influences and the relationship with TC tracks are examined. As a result, it is found that large increase of the heavy rainfall cases along the coastal region. By contrast, there are marginal changes in the strong wind speed associated with TC landfalls. Further, it is also found that the cases of the heavy rainfall only are related with TCs passing through the Yellow Sea and the cases of both the strong wind and the heavy rainfall are related with TCs landing from southern Korea.