• 제목/요약/키워드: Frequency and intensity of typhoon

검색결과 42건 처리시간 0.025초

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.

북한에 상륙한 태풍의 기후학적 특성 (The Climatological Characteristics of the Landfall Typhoons on North Korea)

  • 안숙희;김백조;박소연;박길운
    • 대기
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    • 제20권3호
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    • pp.239-246
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    • 2010
  • In this study, the climatological characteristics of the landfall typhoons on North Korea are surveyed to estimate the frequency, the intensity, the track, and their damage. The data for the period of 1951-2008 are used from both RSMC (Regional Specialized Meteorological Center) Tokyo Typhoon Center and NCEP/NCAR (National Centers for Environmental Prediction/National Center for Atmospheric Research), EM-DAT (Emergency Events Database). There are the ten highest frequencies from 1961 to 1965 and is one frequency for the period of both 1966-1979 and 1976-1980 respectively. Even if a clear trend on the frequency of typhoon is not defined, it is noticeable the intensity has been weak since the frequency of TS (Tropical Storm) decreased. In order to figure out both the characteristic of intensity and the relation between the typhoon track and the expansion of North Pacific High (NPH), Typhoon's tracks are classified into three types as follows: (I) landing on the west coast of North Korea through the mainland of China, (II) landing on the west coast of North Korea, (III) landing on a central/eastern part of the Korean peninsula through South Korea. More often than not, the characteristic of Type (I) is the case of a landfall after it becomes extratropical cyclone. Type(II) and Type(III) show a landfall as TS grade, by comparision. On the relation between the typhoon's track and the expansion of NPH analyzed, Type (I) shows the westward expansion while both Type (II) and Type (III) show the northward expansion and development of NPH. This means the intensity of a typhoon landfall on North Korea is variable depending on the development of NPH. Finally, only two cases are found among total five cases in EM-DAT, reportedly that North Korea was damaged. And therefore, the damage by the wind of Prapiroon (the $12^{th}$ typhoon, 2000) and heavy rainfall with Rusa (the $15^{th}$ typhoon, 2002) landing on North Korea was analyzed. Moreover, it is estimated both Prapiroon and Rusa have done badly damaged to North Korea as the economical losses of as much as six billion and five hundred-thousand US dollar, respectively.

2008년 태풍 특징 (Characteristics of Tropical Cyclones over the Western North Pacific in 2008)

  • 차은정;황호성;양경조;원성희;고성원;김동호;권혁조
    • 대기
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    • 제19권2호
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    • pp.183-198
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    • 2009
  • The purpose of this study is to summarize the tropical cyclone (TC) activity of 2008 over the western North Pacific including the verification of the official track and intensity forecast errors of these TCs. The TC activity - frequency, Normalized Typhoon Activity (NTA), and life span - was lower than 58-year (1951-2008) average. 22 tropical cyclones of tropical storm (TS) intensity or higher formed in the western North Pacific and the South China Sea in 2008. The total number is less than 58-year average frequency of 26.4. Out of 22 tropical cyclones, 11 TCs reached typhoon (TY) intensity, while the rest 11 TCs only reached severe tropical storm (STS) and tropical storm (TS) intensity - six STS and five TS storms. One typhoon KALMAEGI (0807) among them affected the Korea peninsula. However, no significant impact - casualty or property damage - was reported. On average of 22 TCs in 2008, the Korea Meteorological Administration (KMA) official track forecast error for 48 hours was 229 km. There was a big challenge for individual cyclones such as 0806 FENGSHEN and 0817 HIGOS presenting significant forecast error, with both intricate tracks and irregular moving speed. The tropical cyclone season in 2008 began in April with the formation of NEOGURI (0801). In May, four TCs formed in the western North Pacific in response to enhanced convective activity. On the other hand, the TC activity was very weak from June to August. It is found that the unusual anti-cyclonic circulation in the lower level and weak convection near the Philippines are dominant during summertime. The convection and atmospheric circulation in the western North Pacific contributed unfavorable condition for TC activity in the 2008 summertime. The 2008 TC activity has continued the below normal state since mid 1990s which is apparent the decadal variability in TC activity.

Logic tree approach for probabilistic typhoon wind hazard assessment

  • Choun, Young-Sun;Kim, Min-Kyu
    • Nuclear Engineering and Technology
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    • 제51권2호
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    • pp.607-617
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    • 2019
  • Global warming and climate change are increasing the intensity of typhoons and hurricanes and thus increasing the risk effects of typhoon and hurricane hazards on nuclear power plants (NPPs). To reflect these changes, a new NPP should be designed to endure design-basis hurricane wind speeds corresponding to an exceedance frequency of $10^{-7}/yr$. However, the short typhoon and hurricane observation records and uncertainties included in the inputs for an estimation cause significant uncertainty in the estimated wind speeds for return periods of longer than 100,000 years. A logic-tree framework is introduced to handle the epistemic uncertainty when estimating wind speeds. Three key parameters of a typhoon wind field model, i.e., the central pressure difference, pressure profile parameter, and radius to maximum wind, are used for constructing logic tree branches. The wind speeds of the simulated typhoons and the probable maximum wind speeds are estimated using Monte Carlo simulations, and wind hazard curves are derived as a function of the annual exceedance probability or return period. A logic tree decreases the epistemic uncertainty included in the wind intensity models and provides reasonably acceptable wind speeds.

한반도 영향 태풍의 이동경로에 따른 재해 특성 (The Characteristics of Disaster by Track of Typhoon Affecting the Korean Peninsula)

  • 안숙희;김백조;이성로;김호경
    • 한국방재학회 논문집
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    • 제8권3호
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    • pp.29-36
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    • 2008
  • 본 연구의 목적은 동 서해를 중심으로 한반도 주변 해역을 통과하는 태풍과 관련된 재해 특성을 조사하는 것이다. 먼저, 1951년부터 2006년까지 Regional Specialized Meteorological Center (RSMC)-Tokyo의 태풍 자료를 이용하여 한반도에 영향을 준 태풍을 우리나라의 서해와 동해를 통과하는 사례로 구분하고, 각 사례별로 연도별 및 월별의 빈도와 강도에 대해 분석하였다. 특히, 1973년부터 2006년까지의 기간에 대해서는 사례별 태풍 재해의 규모를 파악하여 비교하였다. 서해를 통과하는 태풍의 발생빈도는 거의 변화가 없고 강도가 약한 반면에 동해를 통과하는 태풍의 발생빈도는 증가하는 추세를 보이고 강도가 점차 강해지고 있다. 동해를 통과하는 태풍의 경우에는 집중호우에 의한 침수면적과 농경지피해가 크게 나타났으며, 서해를 통과하는 경우에는 주택, 선박, 도로 및 교량 등 강풍에 의한 시설물 파손에 의한 피해가 크게 발생하였다. 태풍 재해 발생과 관련하여 강수량과 최대풍속 자료를 비교 분석한 결과, 동해를 통과한 태풍의 경우는 집중호우, 서해를 통과한 태풍은 강한 바람에 의한 영향이 크게 나타난 것으로 보였다.

기상재해연구-태풍과 해난- (A Study on the Meteorological Disaster in Korean Waters)

  • 박종길;김유근;안영화
    • 수산해양기술연구
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    • 제27권1호
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    • pp.56-63
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    • 1991
  • This paper aims to describe the relation between the weather condition, especially typhoon and a shipwreck in Korean waters. For this study, it was investigated the statistical characteristics of a shipwreck due to the weather, pressure patterns governing the shipwreck in Korean waters. and the relation between the intensity of typhoon and the amount of a disaster. The results are summarized as follows: 1) The monthly occurrence frequency of a shipwreck was the heighest in July followed by February, March in descending order. 2) The pressure patterns governing the shipwreck were classified broadly into six types and pressure pattern which had most occurrence frequency of a shipwreck was Type V and then cames Type I, Type III and type IV in that order. 3) Occurence frequency of a shipwreck and the amount of a kinetic energy of typhoon have nothing to do with each other. In case of Wind-Typhoon that brought more a strong wind than a heavy rainfall, there were seriously affected ships and buildings by the wind.

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2006년 태풍 특징과 태풍 예보의 개선방향 (Characteristics of Typhoon in 2006 and Improvement of Typhoon Forecast)

  • 차은정;이경희;박윤호;박종숙;심재관;인희진;유희동;권혁조;신도식
    • 대기
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    • 제17권3호
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    • pp.299-314
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    • 2007
  • The purpose of this study is to summarize tropical cyclone activity in 2006. Twenty three tropical cyclones of tropical storm (TS) intensity or higher formed in the western North Pacific and the South China Sea in 2006. The total number is less than the thirty-year (1971~2000) average frequency of 26.7. Out of twenty three tropical cyclones, fifteen cyclones reached typhoon (TY) intensity, while the rest eight cyclones only reached severe tropical storm (STS) and tropical storm (TS) intensity - three STS and five TS storms. The tropical cyclone season in 2006 began in May with the formation of CHANCHU (0601). The convective activity was slightly inactive around the Philippines from late June to early August. In addition, subtropical high was more enhanced than normal over the south of Japan from May to early August. Consequently, most tropical cyclones formed over the sea east of the Philippines after late June, and many of them moved westwards to China. CHANCHU (0601), BILIS (0604), KAEMI (0605), PRAPIROON (0606) and SAOMI (0608) brought damage to China, the Philippines, and Vietnam. On the other hand, EWINIAR (0603) moved northwards and hit the Republic of Korea, causing damage to the country. From late August to early September, convective activity was temporarily inactive over the sea east of the Philippines. However, it turned active again after late September. Subtropical high was weak over the south of Japan after late August. Therefore, most tropical cyclones formed over the sea east of the Philippines and moved northwards. WUKONG (0610) and SHANSHAN (0613) hit Japan to bring damage to the country. On the other hand, XANGSANE (0615) and CIMARON (0619) moved westwards in the South China Sea, causing damage to the Philippines, Thailand, and Vietnam. Another special feature in 2006 tropical cyclone activity is that IOKE (0612) formed in the central North Pacific crossed 180 degree longitude and moved into the western North Pacific. It has been four years since HUKO (0224) in 2002.

태풍 파랑과 지진을 연계한 케이슨식 방파제의 동적거동 (Dynamic Behavior of Caisson Type Breakwater Considering Typhoon-induced Wave Loading Before and After Earthquakes)

  • 윤현수;노병진;윤성규;강기천
    • 한국지반신소재학회논문집
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    • 제23권1호
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    • pp.49-60
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    • 2024
  • 최근 기후변화 등 달라진 해양 환경으로 인해 태풍 파랑의 빈도 및 강도가 증가하고 있다. 뿐만 아니라 일본, 칠레, 아이티, 중국, 인도네시아 등 세계적으로 잦은 지진으로 인해 많은 피해가 발생하고 있다. 우리나라 역시 2000년대에 들어서 태풍에 의한 피해가 증가하고 있으며, 지진의 발생 빈도와 강도도 증가하고 있다. 우리나라는 삼면이 바다로 되어있어 태풍에 의해 해안구조물에 많은 피해가 발생할 수 있으며 지진 역시 해안구조물에 많은 피해를 야기시킨다. 이처럼 국내·외적으로 태풍 파랑과 지진의 빈도 및 강도가 증가하는 추세이나 태풍과 지진을 연계한 연구는 전무하다. 따라서, 본 연구에서는 케이슨식 방파제에 태풍 파랑과 지진을 연계하여 총 4가지 Case에 대해 수치해석을 수행하였다. Case 1은 파랑하중, Case 2는 지진파를 각각 적용하였고, Case 3은 파랑하중 이후 지진 발생, Case 4는 지진파 이후 파랑하중까지 적용하여 수치해석을 수행하였다. 수치해석 결과 태풍과 지진을 연계한 Case 3과 Case 4의 경우 기존에 지반의 강도가 저하된 상태에서 하중을 적용하여 각 하중에 의한 피해가 Case 1과 Case 2에 비해 증가한 것을 확인하였다. 또한, 파랑하중 이후 지진파를 적용한 Case 3에서 피해가 가장 큰 것을 확인하였다.

Investigation of mode identifiability of a cable-stayed bridge: comparison from ambient vibration responses and from typhoon-induced dynamic responses

  • Ni, Y.Q.;Wang, Y.W.;Xia, Y.X.
    • Smart Structures and Systems
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    • 제15권2호
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    • pp.447-468
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    • 2015
  • Modal identification of civil engineering structures based on ambient vibration measurement has been widely investigated in the past decades, and a variety of output-only operational modal identification methods have been proposed. However, vibration modes, even fundamental low-order modes, are not always identifiable for large-scale structures under ambient vibration excitation. The identifiability of vibration modes, deficiency in modal identification, and criteria to evaluate robustness of the identified modes when applying output-only modal identification techniques to ambient vibration responses were scarcely studied. In this study, the mode identifiability of the cable-stayed Ting Kau Bridge using ambient vibration measurements and the influence of the excitation intensity on the deficiency and robustness in modal identification are investigated with long-term monitoring data of acceleration responses acquired from the bridge under different excitation conditions. It is observed that a few low-order modes, including the second global mode, are not identifiable by common output-only modal identification algorithms under normal ambient excitations due to traffic and monsoon. The deficient modes can be activated and identified only when the excitation intensity attains a certain level (e.g., during strong typhoons). The reason why a few low-order modes fail to be reliably identified under weak ambient vibration excitations and the relation between the mode identifiability and the excitation intensity are addressed through comparing the frequency-domain responses under normal ambient vibration excitations and under typhoon excitations and analyzing the wind speeds corresponding to different response data samples used in modal identification. The threshold value of wind speed (generalized excitation intensity) that makes the deficient modes identifiable is determined.

Wind-excited stochastic vibration of long-span bridge considering wind field parameters during typhoon landfall

  • Ge, Yaojun;Zhao, Lin
    • Wind and Structures
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    • 제19권4호
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    • pp.421-441
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    • 2014
  • With the assistance of typhoon field data at aerial elevation level observed by meteorological satellites and wind velocity and direction records nearby the ground gathered in Guangzhou Weather Station between 1985 and 2001, some key wind field parameters under typhoon climate in Guangzhou region were calibrated based on Monte-Carlo stochastic algorithm and Meng's typhoon numerical model. By using Peak Over Threshold method (POT) and Generalized Pareto Distribution (GPD), Wind field characteristics during typhoons for various return periods in several typical engineering fields were predicted, showing that some distribution rules in relation to gradient height of atmosphere boundary layer, power-law component of wind profile, gust factor and extreme wind velocity at 1-3s time interval are obviously different from corresponding items in Chinese wind load Codes. In order to evaluate the influence of typhoon field parameters on long-span flexible bridges, 1:100 reduced-scale wind field of type B terrain was reillustrated under typhoon and normal conditions utilizing passive turbulence generators in TJ-3 wind tunnel, and wind-induced performance tests of aero-elastic model of long-span Guangzhou Xinguang arch bridge were carried out as well. Furthermore, aerodynamic admittance function about lattice cross section in mid-span arch lib under the condition of higher turbulence intensity of typhoon field was identified via using high-frequency force-measured balance. Based on identified aerodynamic admittance expressions, Wind-induced stochastic vibration of Xinguang arch bridge under typhoon and normal climates was calculated and compared, considering structural geometrical non-linearity, stochastic wind attack angle effects, etc. Thus, the aerodynamic response characteristics under typhoon and normal conditions can be illustrated and checked, which are of satisfactory response results for different oncoming wind velocities with resemblance to those wind tunnel testing data under the two types of climate modes.