• Title/Summary/Keyword: 태풍 풍속

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A Study on the Flight Initiation Wind Speed of Wind-Borne Debris (강풍에 의한 비산물의 비행 시작 풍속에 관한 연구)

  • Jeong, Houigab;Lee, Seungho;Park, Junhee;Kwon, Soon-duck
    • KSCE Journal of Civil and Environmental Engineering Research
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    • v.40 no.1
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    • pp.105-110
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    • 2020
  • This study provides a method and data for predicting the flight initiation wind speed of wind-borne debris. From the force equilibrium acting on debris including aerodynamic and inertia forces, the equation for predicting the flight initiation wind speeds are presented. Wind tunnel tests were carried out to provide necessary aerodynamic data in the equation for the debris with various aspect ratios. The proposed equation for flight initiation wind speeds was validated from free flying tests in the wind tunnel. The flights of debris were mostly initiated by slip when width to thickness was less than 10, otherwise overturning were dominant. The actual flight initiation speeds were lower than that of the computed ones. The surface boundary layer flow and the gap between the debris and surface might affect the prediction error.

A Study on Development and Utilization of Wind Hazard Maps (강풍위해지도 개발 및 활용 방안에 관한 연구)

  • Lee, Young-Kyu;Lee, Sung-Su;Ham, Hee-Jung
    • Journal of the Korean Society of Hazard Mitigation
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    • v.11 no.3
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    • pp.1-8
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    • 2011
  • In this study, a wind hazard map over Korea peninsula based on geographical information is developed, which consists of the surface roughness model, the topographical effect model and the homogeneous wind model. The surface roughness model is assessed to evaluate the effect of the surface roughness on the wind field near ground. The topographical effect model is assessed to quantify the effect of the speed-up caused by topology, which is calculated by adopting the topographical effect factor in Korea building code (2005). The homogeneous wind map is created either by a frequency analysis method for meteorological data or a typhoon simulation. The results show that the wind hazard map can be applied to the determination of insurance premium as well as the assessment of loss and damage.

Development of Typhoon Damage Forecasting Function of Southern Inland Area By Multivariate Analysis Technique (다변량 통계분석을 이용한 남부 내륙지역 태풍피해예측모형 개발)

  • Kim, Yonsoo;Kim, Taegyun
    • Journal of Wetlands Research
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    • v.21 no.4
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    • pp.281-289
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    • 2019
  • In this study, the typhoon damage forecasting model was developed for southern inland district. The typhoon damage in the inland district is caused by heavy rain and strong winds, variables are many and varied, but the damage data of the inland district are not enough to develop the model. The hydrological data related to the typhoon damage were hour maximum rainfall amount which is accumulated 3 hour interval, the total rainfall amount, the 1-5 day anticipated rainfall amount, the maximum wind speed and the typhoon center pressure at latitude 33° near the Jeju island. The Multivariate Analysis such as cluster Analysis considering the lack of damage data and principal component analysis removing multi-collinearity of rainfall data are adopted for the damage forecasting model. As a result of applying the developed model, typhoon damage estimated and observed values were up to 2.2 times. this is caused it is difficult to estimate the damage caused by strong winds and it is assumed that the local rainfall characteristics are not considered properly measured by 69 ASOS.

Inundation Analysis in Urban Area Resulting from River Overflow during Typhoon Event (태풍권 발생 시 하천범람에 따른 도시지역 침수해석)

  • Keum, Ho Jun;Lee, Jae Yeong;Kim, Hyun Il;Cho, Hong Je;Han, Kun Yeun
    • Proceedings of the Korea Water Resources Association Conference
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    • 2018.05a
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    • pp.413-413
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    • 2018
  • 최근 도시지역에 태풍과 집중호우로 인한 홍수발생 빈도와 그 규모가 커지고 있다. 이에 따른 재산 및 인명피해 양상도 매우 심각한 상황이다. 태풍 차바 처럼 강력한 10월 태풍의 출현은 지구 온난화의 전조로 받아들여지고 있다. 또한 10월 태풍임에도 초속 56.5m의 순간 최대풍속과 시간당 최대 116.7mm(제주 서귀포), 139mm(매곡) 등의 강수량은 지역 최대 강수량을 기록함으로써 이제 언제나 태풍 및 홍수에 대한 대비가 필요하게 되었다. 현재 재해에 대비하기 위해 다양한 대책들은 꾸준히 마련되어지고 있으며, 설계 기준 또한 강화되었다. 그러나 저류조 및 배수펌프장 등의 시설물 설치에는 막대한 예산이 필요한데다 장기간의 시간이 필요하며, 비구조적 대책도 마련되어 있으나 태풍 차바의 사례에서 경험한 것처럼 재해 발생 시 대책과 구체적인 방안의 마련이 더욱 시급해 보인다. 이에 본 연구에서는 태풍 차바 시의 호우에 대하여 UNET모형에 의한 부정류모의를 수행하였다. 부정류모의의 경계조건으로써 상류단 경계조건과 측방유입량 조건은 HEC-HMS를 이용하여 유출해석을 실시한 다음 입력 자료로 이용하였으며, 하류단 경계조건으로는 국토부 관할 수위지점의 수위를 이용하여 UNET 모형에 의한 수리학적 하도추적을 수행하였으며, 저지대 침수분석은 지형정보시스템 응용프로그램 중 하나인 ArcGIS를 활용하여 대상유역의 벡터자료를 구축하고 인접도엽의 접합 및 보정을 실시하여 수치고도자료를 생성하여 2차원 홍수범람해석을 위한 HEC-RAS 5.0을 적용하여 침수분석을 수행하였다. 본 연구의 결과를 수재해 피해저감 대책을 수립하는데 기초자료로 활용될 수 있을거라 판단된다.

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Typhoon Intensity Analysis using GMS Meteorological Satellita Image Data (GMS 기상위성 영상자료를 이용한 태풍강도 분석)

  • 서애숙;김동호;박경선
    • Korean Journal of Remote Sensing
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    • v.11 no.2
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    • pp.17-27
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    • 1995
  • One of the world widely used methods in determining the intensity of a typhoon is Dvorak's technique. By applying the Dvorak's method to the typhoons which affected our country in various degress and extents without regard to their individual severity, we estimated their intensity for six different cases of typhoons. We have derived a regression equation of estimating the central pressures and maximum wind speeds for the six selected typhoons. Their intensity was estimated from the Dvork's method using GMS satellite image data. The derived equation has tested to typhoon ORCHID and the computed values have been compared with the direct observations in its central pressure and maximum wind speed. The computed values in the Dvork's method are smaller in their magnitudes than the observed corresponding values. But their relative magnitudes do not change so much at each different time step. But our results are significantly different from those of NOAA and JMA. The cause of differences are not investigated in depth in this analysis.

Relationship between Tropical Cyclone Intensity and Physical Parameters Derived from TRMM TMI Data Sets (TRMM TMI 관측과 태풍 강도와의 관련성)

  • Byon, Jae-Young
    • Korean Journal of Remote Sensing
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    • v.24 no.4
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    • pp.359-367
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    • 2008
  • TRMM TMI data were used to investigate a relationship between physical parameters from microwave sensor and typhoon intensities from June to September, 2004. Several data such as 85GHz brightness temperature (TB), polarization corrected temperature (PCT), precipitable water, ice content, rain rate, and latent heat release retrieved from the TMI observation were correlated to the maximum wind speeds in the best-track database by RSMC-Tokyo. Correlation coefficient between TB and typhoon intensity was -0.2 - -0.4 with a maximum value in the 2.5 degree radius circle from the center of tropical cyclone. The value of correlation between in precipitable water, rain, latent heat, and typhoon intensity is in the range of 0.2-0.4. Correlation analysis with respect to storm intensity showed that maximum correlation is observed at 1.0-1.5 degree radius circle from the center of tropical cyclone in the initial stage of tropical cyclone, while maximum correlation is shown in 0.5 degree radius in typhoon stage. Correlation coefficient was used to produce regressed intensities and adopted for typhoon Rusa (2002) and Maemi (2003). Multiple regression with 85GHz TB and precipitable water was found to provide an improved typhoon intensity when taking into account the storm size. The results indicate that it may be possible to use TB and precipitable water from satellite observation as a predictor to estimate the intensity of a tropical cyclone.

Determination of Design Waver along the West Coast of Korea (한국 서해안에서의 설계파의 결정)

  • 김태인;청형식
    • Water for future
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    • v.20 no.2
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    • pp.127-138
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    • 1987
  • For determination of the design wave, a method of estimating the design wind speed at sea from the wind records at the nearby weather stations on land is proposed. Along the West Coast, the design wind speed are shown to have two main directions; namely, N through W, and WSW through S. Through the analysis of weather maps, fetches for the main wind directions along the West Coast are determined. The wind speeds at sea are found to have 0.8~0.9 times the wind speed at the stations on land for U$\geq$20m/s. The West Coast may be divided into three regions for which fetches are determind uniquely. Design waves with return period of 100 years are determined by the revised S.M..B. method along the West Coast, and show the deep water significant wave heights of 4.4~8.3 meters with wave periods of 8.9~12.0 seconds.

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Time and Spatial Distribution of Probabilistic Typhoon Storms and Winds in Korean Peninsula (한반도에 내습한 태풍의 확률강우 및 풍속의 시공적 분포 특성)

  • 윤경덕;서승덕
    • Magazine of the Korean Society of Agricultural Engineers
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    • v.36 no.3
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    • pp.122-134
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    • 1994
  • The objective of this study is to provide with the hydrometeological and probabilistic characteristics of the storms and winds of typhoons that have been passed through the Korea peninsula during the last twenty-three years since 1961. The paths and intensities of the typhoons were analyzed. Fifty weather stations were selected and the rainfall and wind data during typhoon periods were collected. Rainfall data were analyzed for the patterns and probabilistic distributions. The results were presented to describe the areal distributions of probabilistic characteristics. Wind data were also analysed for their probabilistic distributions. The results obtained from this study can be summarized as follows: 1. The most frequent typhoon path that have passed through the Korean peninsula was type E, which was followed by types CWE, W, WE, and S. The most frequent typhoon intensity was type B, that was followed by A, super A, and C types, respectively. 2. The third quartile typhoon rainfall patterns appear most frequently followed by the second, first, and quartiles, respectively, in Seoul, Pusan, Taegu, Kwangju and Taejon. The single typhoon rainfalls with long rainfall durations tended to show delayed type rainfall patterns predominantly compared to the single rainfalls with short rainfall durations. 3. The most frequent probabilistic distribution for typhoon rainfall event is Pearson type-III, followed by Two-parameter lognormal distribution, and Type-I extremal distribution. 4. The most frequent probability distribution model of seashore location was Pearson type-III distribution. The most frequent probability distribution model of inland location was two parameter lognormal distribution. 5. The most frequent probabilistic distribution for typhoon wind events was Type-I xtremal distribution, followed by Two-parameter lognormal distribution, and Normal distribution.

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Development of Evacuation Algorithm from Coastal Inundation (해안침수 대피경로 알고리즘 개발)

  • Kim, Won Beom;Jung, Woo Chang;Son, Kwang Ik
    • Proceedings of the Korea Water Resources Association Conference
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    • 2020.06a
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    • pp.355-355
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    • 2020
  • 최근 쓰나미와 해일 등 이상기후에 의한 해수면 상승 등으로 인한 해안지역의 침수가 빈번해지고 있다. 태풍 매미의 경우, 피해규모는 인명피해 130명, 이재민 4089세대 10975명, 재산피해 4조 7810억원이며 침수피해는 규모는 주택 21,015동과 농경지 37,986ha으로 나타났다. 특히 이 태풍은 경남 사천시 부근 해안에 상륙할 때의 중심기압은 950hPa로 중심부근 최대풍속 40m/s 이었으며 풍속 15 m/s 이상으로로, 태풍의 강도는 [강], 크기는 [중형]이었음에도 그 피해는 과거에 비해 크게 나타났다. 내륙과는 달리 해일 등의 피해로 인한 해안지역의 침수피해 저감기법은 월파방지 파라펫 설치 또는 침수예상 지역의 지반고를 높이는 이외에는 확실한 대책이 없는 것이 특징이라 하겠다. 따라서 해안지역 침수예방은 월파방지 파라펫과 함께 인명피해 최소화를 위해서는 충분한 선행시간을 통한 대피안내와 가장 효율적인 대피경로를 제공하는 것이 최선이라 할 수 있다. 본 연구에서는 경남 창원지역의 해수면 상승으로 인한 해안지역 침수를 모의할 수 있는 2차원 부정류 프로그램을 개발하고 매미 당시 창원지역의 침수피해 결과와 비교하여 프로그램 모의 결과를 검증하였다. 해안을 따라 다양한 높이의 월파방지 파라펫을 모의하여 시간대별 대상지역의 침수규모를 시간대별로 예측하였다. 모의결과 월파방지 파라펫 규모 별 침수규모와 이에 따른 경제적 피해규모를 산정하였으며 경제성 원칙에 따른 최적의 파라펫 규모를 제시하였다. 또한 이때 시간대별 침수범위 예측 결과를 바탕으로 시간대별 등침수선을 제시하고 일정 시간대별 등침수선을 모의결과를 이용하여 산정하였다. 도로 경사와 대피자의 연령 등을 고려한 대피소요 시간을 산정하여 침수 소요 시간과 비교하여 대피가 가능한 대피경로를 제시하는 알고리즘을 제안하였다. 본 연구결과는 기존에 알려진 대피경로와는 달리 다양한 침수저감 기법규모에 따라 다양한 대피경로를 제안할 수 있었으며 이는 추후 다양한 대피 시나리오를 제시할 수 있는 기초자료를 제공할 수 있을 것으로 기대된다.

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