• 제목/요약/키워드: low level strong wind

검색결과 58건 처리시간 0.028초

금정산 풍하측 저고도의 강풍 현상 (On the Low Level Strong Wind Occurring at the Downwind Side of the Kumjeong Mountain.)

  • 임상진;서광수
    • 한국환경과학회지
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    • 제5권6호
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    • pp.713-718
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    • 1996
  • We identified two characteristic turbulent flow cases, weakening and strengthening, which appear at the downwind side. Observations were made two times, Dec. 2-3. 1995 and Feb. 13-14. 1996 at Pusan National University site located downwind side of Kumjeong mountain. Meteorological observation system, tethersonde, was adopted to present observation. In the case of the west wind which blows perpendicular to Sanghak mountain located westward from the site, the wind speed highly increased in exponential with height. Therefore, the low level wind speed was so weak just like Taylor(1988)'s review. While the wind speed was intensified at 200-400m layer when the northwest wind blows from the continental Siberian high. We suppose 기 is because of the strong vertical convergence of flow between the surface inversion layer and the upper one, and also the horizontal convergence along the saddle and valley between the two mountains, Kumjeong and Sanghak-because of Bernoulli's effect. The inversion layer existed at surface-l00m and 500-600m level and the strong wind existed at about 200-400m layer.

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제주국제공항 활주로에 양배풍을 유발하는 기압 패턴에 관한 연구 (A Study on the Pressure Patterns that Causes Bidirectional Tailwind on the Runway of Jeju International Airport)

  • 조진호;이강민;백호종;박장훈
    • 한국항공운항학회지
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    • 제31권3호
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    • pp.93-102
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    • 2023
  • Jeju International Airport is characterized by the occurrence of low-level windshear due to its location, surrounding terrain, and its weather characteristics. Especially the low-level windshear accompanied by tailwinds on both sides of the runway i.e., bidirectional tailwind, is a hazardous weather phenomenon with unique characteristics that are difficult to find at any other airports. This study focuses on bidirectional tailwind occurrence at Jeju International Airport in 2020-2021. As a result, characteristic pressure patterns of the types that cause bidirectional tailwind was identified as it was possible to categorize strong wind types such as 1) strong southwest wind, 2) strong east wind, and 3) strong northwest wind, which do not cause bidirectional tailwind, and wind direction variation types such as 4) bidirectional tailwind, and 5) south wind followed by southwest wind, which cause bidirectional tailwind. The results of this study are expected to contribute to improving aviation safety by enabling aviation operators to predict and take appropriate safety measures based on their understanding of the causes and characteristics of bidirectional tailwind.

항공기 복행사례를 통한 제주국제공항 저층 윈드시어의 특징 연구 (A Study on the Characteristics of Low-Level Wind Shear at Jeju International Airport from Go-Around Flight Perspective)

  • 조진호;백호종
    • 한국항공운항학회지
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    • 제29권1호
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    • pp.1-8
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    • 2021
  • Low level wind shear, which often occurs at Jeju International Airport, is a phenomenon that occurs when the topological location and topographical characteristics of Jeju Island are combined with weather characteristics. Low level wind shears, which are caused by rapid changes in wind direction and wind speed, pose a threat to aircraft safety and also cause abnormal situations, such as aircraft go-around, diversion, and cancellation. Many meteorological studies have been conducted on weather patterns, occurrence periods and frequency of low level wind shears. However, researches related to aircraft operations are limited where here we study the similarities and differences between strong southwest winds and bidirectional tailwind type low level wind shears based on aircraft go-around cases at Jeju International Airport. The results are expected to be used to enhance safety when operating to Jeju International Airport, which includes pilot training that reflects the characteristics generated by wind changes, pilot prior notification, providing pilots with latest trends, and increasing extra fuel.

Development of Algorithm for the Decision of Ship's Strong Wind Warning Levels

  • Shouhu, Hu;Moon, Serng-Bae
    • 한국항해항만학회지
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    • 제42권5호
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    • pp.317-322
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    • 2018
  • Marine weather information provided for vessels is mainly offered by radio devices such as NAVTEX, Weather Fax., and others. However, the information is too general for large areas, and lacks more detail. So, many seafarers are disinclined to use the information to initiate proper readiness of vessels' safety, avoiding marine accidents such as grounding, hull and cargo damage, but cannot develop an optimal and economical navigation plan, considering the inadequate level of low precision weather information. The purpose of this paper is to develop a strong wind warning system, based on the digital anemometer installed on the bridge. This study analyzed the data on 10-minutes average wind speed, when the vessel's grounding accidents happened in Korean ports. Results reveal that the vessel's strong wind warning algorithm, can estimate the growing of wind speed two-three hours in advance.

A Case Study on Heavy Rainfall Using a Wind Profiler and the Stability Index

  • Hong, Jongsu;Jeon, Junhang;Ryu, Chansu
    • 통합자연과학논문집
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    • 제8권3호
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    • pp.221-232
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    • 2015
  • In this study, the vertical characteristics of wind were analyzed using the horizontal wind, vertical wind, and vertical wind shear, which are generated from a wind profiler during concentrated heavy rain, and the quantitative characteristics of concentrated heavy rain were analyzed using CAPE, SWEAT, and SRH, among the stability indexes. The analysis of the horizontal wind showed that 9 cases out of 10 had a low level jet of 25 kts at altitudes lower than 1.5 km, and that the precipitation varied according to the altitude and distribution of the low-level jet. The analysis of the vertical wind showed that it ascended up to about 3 km before precipitation. The analysis of the vertical wind shear showed that it increased up to a 1 km altitude before precipitation and had a strong value near 3 km during heavy rains. In the stability index analysis, CAPE, which represents thermal buoyancy, and SRH, which represents dynamic vorticity, were used for the interpretation of the period of heavy rain. As SWEAT contains dynamic upper level wind and thermal energy, it had a high correlation coefficient with concentrated-heavy-rain analysis. Through the case studies conducted on August 12-13, 2012, it was confirmed that the interpretation of the prediction of the period of heavy rain was possible when using the intensive observation data from a wind profiler and the stability index.

Observations of Coastal Upwelling at Ulsan in summer 1997

  • Lee, Jae-Chul;Kim, Dae-Hyun;Kim, Jeong-Chang
    • Journal of the korean society of oceanography
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    • 제38권3호
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    • pp.122-134
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    • 2003
  • Low-pass filtered time series of wind, coastal temperature, sea level and current were analyzed to understand the coastal upwelling processes in the southeast coast of Korea. Southerly winds favorable for coastal upwelling were dominant in summer of 1997. Total period of four major wind events amounts to 58 days during one hundred days from June to early September. Coastal temperature is most sensitive to variations of wind. The time lag between the onset of southerly (northerly) winds and decrease (increase) of temperature is 3-18 hours. In the frequency domain the coherent bands have periods of 2.4 and 4.0-5.4 days with respective phase lags of 17 and 27-37 hours. Despite the sensitive response, the magnitude of temperature change is not quantitatively proportional to the intensity or duration of the wind, because it depends on the degree of baroclinic tilting of isotherms built dynamically by the strong Tsushima Warm Current (TWC). Current is particularly strong near the coast and has a large vertical shear during the upwelling periods, which is associated with the baroclinic tilting. Both of current and sea level are poorly coherent with wind or temperature except for the period of 4 days.

강풍 사례의 해상풍 모의를 위한 모형의 최적화 (Model Optimization for Sea Surface Wind Simulation of Strong Wind Cases)

  • 허기영;이정욱;하경자;전기천;박광순
    • 한국지구과학회지
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    • 제29권3호
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    • pp.263-279
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    • 2008
  • 이 연구에서는 2006년 9월 17일의 태풍 산산과 2006년 12월 16일의 시베리아 고기압 확장에 의한 강풍 사례에 대하여 MM5와 WRF 중규모 수치 모형을 이용한 실험을 통해 강한 해상풍을 모의하기 위한 모형의 최적화가 조사되었다. 모형의 최적화는 모형의 최하층 고도, 물리 모수화, 모형 해상도에 대해 조사되었으며, 결과를 요약하면 다음과 같다. 1) 두 사례 모두 최하층 연직 고도를 해상풍 관측 고도인 10m가지 선형적으로 내리는 것보다 대기 하층의 안정도와 해수면 거칠기를 고려하여 로가리듬의 함수로 변환하는 것이 더 정확한 모의를 하였다. 2) 강한 해상풍 모의를 위한 최적의 모수화 방안을 찾기 위해, 여러 물리 모수화 방안을 조합하여 모형에 적용하였다. 3) 3-km의 고분해능의 모형 결과가 9-km 분해능의 모형 결과에 비해 강풍 지역과 저기압의 강도와 같은 저기압의 중규모 구조를 잘 나타내었다.

Potentials of elastic seismic design of twisted high-rise steel diagrid frames

  • Kim, Seonwoong;Lee, Kyungkoo
    • Steel and Composite Structures
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    • 제18권1호
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    • pp.121-134
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    • 2015
  • This paper is to investigate the potentials of the elastic seismic design of twisted high-rise steel diagrid frame buildings in the strong wind and moderate/low seismicity regions. First, the prototypes of high-rise steel diagrid frames with architectural plans that have a twist angle of 0 (regular-shaped), 1, and 2 degrees were designed to resist wind. Then, the effects of the twist angle on the estimated quantities and structural redundancies of the diagrid frames were examined. Second, the seismic performance of the wind-designed prototype buildings under a low seismicity was evaluated. The response spectrum analysis was conducted for the service level earthquake (SLE) having 43-year return period and the maximum considered earthquake (MCE) having 2475-year return period. The evaluation resulted that the twisted high-rise steel diagrid frames resisted the service level earthquake elastically and most of their diagrid members remained elastic even under the maximum considered earthquake.

沿岸境界層에서의 表層風의 日變化 (Diurnal Variation of the Surface Wind in the Coastal Boundary Layer)

  • 최효
    • 한국해양학회지
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    • 제19권2호
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    • pp.210-216
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    • 1984
  • 5년간의 시간별 풍속 자료를 이용하여 연안 표층풍의 일변화가 분석되었다. 특히 내륙으로 부는 바람 (onshore flow)이 지배적인 계절에는 야간 최대풍의 최대 출현 빈도가 자정에 나타났다. 연평균 남풍 계열을 갖는 야간 최대풍은 북풍 계열 보다 약 3배이상의 출현을 보여준다. 중림의 대기 안정도가 연안에 지배적이므로 바람이 해양에서 내륙으로 불 경우는 (offshore flow) 상승된 전선역전층과 지표역전층에 의해 형성된 전단력(shear flow)이 연안경계층으로 전이되어 야간 연안 최대표층풍이 형성된다.

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해풍 효과에 의한 저층대기구조 변화의 측정 (Observation on Structural Change of Low Level Atmosphere due to Effect of Sea Breeze)

  • 전병일;김유근
    • 한국환경과학회지
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    • 제5권4호
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    • pp.441-451
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    • 1996
  • The surface meteorological and upper layer meteorological observation carried out to investigate influences of sea breeze effect on lower layer atmosphere at Gori nuclear power plant for 29∼30 July, 1996. According to surface meteorological data, the inflow of sea breeze was occurred 11:30 on 29 July, 10:30-on 30 July, respectively, at observation site. And the meteorological tower data showed that wind direction of sea breeze was identified as south-westerly, and wind speed of 58 m was 2 times stronger than that of 10 m. It is notworthy that surface inversion layer which built from the night time to daybreak of next day was not broken off by seab reeze's inflow for daytime, and strong inversion layer observed at 47∼243 m with moderately stable class (F) by URC. It was found that strong stable layer of potential temperature appeared at that layer, maximum relative humidity observed at the bottom of inversion layer and maximum mixing ratio observed in the low of inversion layer.

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