Figure 6. Maximum inundation field in simulations with (a) no barrier on the seawall (red line), (b) a 1 m barrier across the entire sea wall, and (c) a 1.7 m barrier partially installed on the seawall.

Jae-Seol Shim†, Jinah Kim†, Dong-Chul Kim‡, Kiyoung Heo†, Kideok Do†, Sun-Jung Park ‡
† Coastal Disaster Research Center,
Korea Institute of Ocean Science &
Technology, 426-744, Ansan, Gyeonggi,
Korea
jsshim@kiost.ac
jakim@kiost.ac
kyheo21@kiost.ac
kddo@kiost.ac
‡ Technology R&D Institute
Hyein E&C Co., Ltd., Seoul 157-861,
Korea
skkkdc@chol.com
Nayana_sj@nate.com

ABSTRACT

Shim, J., Kim, J., Kim, D., Heo, K., Do, K., Park, S., 2013. Storm surge inundation simulations comparing threedimensional with two-dimensional models based on Typhoon Maemi over Masan Bay of South Korea. In:
Conley, D.C., Masselink, G., Russell, P.E. and O’Hare, T.J. (eds.), Proceedings 12th International Coastal Symposium
(Plymouth, England), Journal of Coastal Research, Special Issue No. 65, pp. 392-397, ISSN 0749-0208.
Severe storm surge inundation was caused by the typhoon Maemi in Masan Bay, South Korea in September 2003. To
investigate the differences in the storm surge inundation simulated by three-dimensional (3D) and two-dimensional
models, we used the ADvanced CIRCulation model (ADCIRC) and 3D computational fluid dynamics (CFD) model
(FLOW3D). The simulation results were compared to the flood plain map of Masan Bay following the typhoon Maemi.
To improve the accuracy of FLOW3D, we used a high-resolution digital surface model with a few tens of centimeterresolution, produced by aerial LIDAR survey. Comparison of the results between ADCRIC and FLOW3D simulations shows that the inclusion of detailed information on buildings and topography has an impact, delaying seawater propagation and resulting in a reduced inundation depth and flooding area. Furthermore, we simulated the effect of the installation of a storm surge barrier on the storm surge inundation. The barrier acted to decrease the water volume of the inundation and delayed the arrival time of the storm surge, implying that the storm surge barrier provides more time for residents’ evacuation.

Keywords: Typhoon Maemi, digital surface elevation model, Reynolds-Averaged NavierStokes equations.

2003 년 9 월 대한민국 마산만 태풍 매미에 의해 심한 폭풍 해일 침수가 발생했습니다. 3 차원 (3D) 및 2 차원 모델로 시뮬레이션 한 폭풍 해일 침수의 차이를 조사하기 위해 ADvanced CIRCulation 모델 ( ADCIRC) 및 3D 전산 유체 역학 (CFD) 모델 (FLOW3D).

시뮬레이션 결과는 태풍 매미 이후 마산만 범람원 지도와 비교되었다. FLOW-3D의 정확도를 높이기 위해 우리는 항공 LIDAR 측량으로 생성된 수십 센티미터 해상도의 고해상도 디지털 표면 모델을 사용했습니다.

ADCRIC과 FLOW3D 시뮬레이션의 결과를 비교하면 건물과 지형에 대한 자세한 정보를 포함하면 해수 전파가 지연되고 침수 깊이와 침수 면적이 감소하는 것으로 나타났습니다.

또한, 폭풍 해일 침수에 대한 폭풍 해일 장벽 설치의 효과를 시뮬레이션했습니다. 이 장벽은 침수 물량을 줄이고 폭풍 해일 도착 시간을 지연시키는 역할을 하여 폭풍 해일 장벽이 주민들의 대피에 더 많은 시간을 제공한다는 것을 의미합니다.

INTRODUCTION

2003 년 9 월 12 일 태풍 매미로 인한 강한 폭풍 해일이 남해안을 강타했습니다. 마산 만 일대는 심한 폭풍우 침수로 인해 최악의 피해를 입었고 광범위한 홍수를 겪었습니다. 따라서 마산 만에 예방 체계를 구축하기 위해 폭풍 해일에 의한 침수에 대한 수치 예측을 시도하는 선행 연구가 수행되었다 (Park et al. 2011).

그러나 일반적인 2 차원 (2D) 또는 3 차원 (3D) 수압 가정을 사용할 때 지형의 해상도는 복잡한 해안 구조를 표현하기에 충분하지 않습니다. 따라서 우리는 마산 만의 고해상도 지형도를 통해 전산 유체 역학 (CFD)의 침수 시뮬레이션을 제시한다.

태풍 매미는 2003 년 9 월 12 일 12시 (UTC)에 한반도에 상륙하여 남동부 해안을 따라 추적했습니다 (그림 1). 2003 년 9 월 13 일 6시 (UTC)에 동 일본해로 이동하여 온대 저기압이되었습니다.

풍속과 기압면에서 한국을 강타한 가장 강력한 태풍 중 하나입니다. 특히 마산 만에 접해있는 마산시는 폭풍 해일 홍수로 최악의 피해를 입어 32 명이 사망하고 심각한 해안 피해를 입었다. 태풍이 지나가는 동안 중앙 기압은 950hPa, 진행 속도는 45kmh-1로 마산항의 조 위계를 통해 최대 약 2.3m의 서지 높이를 기록했다.

마산 만에 접한 주거 및 상업 지역은 홍수가 심했고 지하 시설은 폭풍 해일로 침수로 어려움을 겪었습니다 (Yasuda et al. 2005). 이 논문에서는 3D CFD 모델 (FLOW 3D)과 2D ADvanced CIRCulation 모델 (ADCIRC)을 사용하여 기록 된 마산 만에서 가장 큰 폭풍 해일 중 하나에 의해 생성 된 해안 침수를 시뮬레이션했습니다.

건물의 높이와 공간 정보를 포함하는 디지털 표면 모델 (DSM)은 LiDAR (Airborne Light Detection and Ranging)에 의해 만들어졌으며, 폭풍 해일 침수 모델, 즉 3D CFD 모델 (FLOW 3D)의 입력 데이터로 사용되었습니다. ). 또한 ADCIRC의 시뮬레이션 결과는 FLOW3D의 경계 조건으로 사용됩니다.

본 연구의 목적은 극심한 침수 높이와 해안 육지로의 범람을 포함하여 마산 만에서 태풍 매미로 인한 폭풍 해일 침수를 재현하는 것이다.

<중략>………………

Figure 1. The best track and the central pressures of the typhoon Maemi from the Joint Typhoon Warning Center (JTWC). Open circles indicate the locations of the typhoon in 3 h intervals. Filled circles represent locations of the cited stations; A, B, C and D indicate Jeju, Yeosu, Tongyoung, and Masan, respectively.
Figure 1. The best track and the central pressures of the typhoon Maemi from the Joint Typhoon Warning Center (JTWC). Open circles indicate the locations of the typhoon in 3 h intervals. Filled circles represent locations of the cited stations; A, B, C and D indicate Jeju, Yeosu, Tongyoung, and Masan, respectively.
Figure 2. Model domain with FEM mesh for Typhoon Maemi.
Figure 2. Model domain with FEM mesh for Typhoon Maemi.
Figure 3. Validation of surge height for the four major tidal stations on the south coast of the Korea.
Figure 3. Validation of surge height for the four major tidal stations on the south coast of the Korea.
Figure 4. Inundation depth results from (a) ADCIRC, (b) FLOW3D, and (c) inundation field surveying hazard map following typhoon Maemi.
Figure 4. Inundation depth results from (a) ADCIRC, (b) FLOW3D, and (c) inundation field surveying hazard map following typhoon Maemi.
Figure 5. Inundation depth results computed by Flow3D at each time period following arrival of storm surge wave at harbor mouth.
Figure 5. Inundation depth results computed by Flow3D at each time period following arrival of storm surge wave at harbor mouth.
Figure 6. Maximum inundation field in simulations with (a) no barrier on the seawall (red line), (b) a 1 m barrier across the entire sea wall, and (c) a 1.7 m barrier partially installed on the seawall.
Figure 6. Maximum inundation field in simulations with (a) no barrier on the seawall (red line), (b) a 1 m barrier across the entire sea wall, and (c) a 1.7 m barrier partially installed on the seawall.

LITERATURE CITED

Bunya S, Kubatko EJ, Westerink JJ, Dawson C.,2010. A wetting and drying treatment for the Runge–Kutta discontinuous Galerkin solution to the shallow water equations. Computer Methods in Applied Mechanics and Engineering, Oceanography and Coastal Research, 198, 1548-1562.
Chan, J.C.L. & Shi, J.,1996. Long term trends and interannual variability in tropical cyclone activity over the western North Pacific. Geophysical Research Letters 23, 2765-2767.
Choi, B.H., Kim, D.C., Pelinovsky, E. and Woo, S.B., 2007. Threedimensional simulation of tsunami run-up around conical island. Coastal Engineering, 54, 618-629.
Choi, B.H., Pelinovsky, E., Kim, D.C., Didenkulova, I. and Woo, S.B., Two- and three-dimensional computation of solitary wave runup on non-plane beach. Nonlinear Processes in Geophysics, 15, 489-502.
Choi B.H., Pelinovsky E., Kim D.C., Lee H.J., Min B.I. and Kim K.H., Three-dimensional simulation of 1983 central East (Japan) Sea earthquake tsunami at the Imwon Port (Korea). Ocean Engineering, 35, 1545-1559.
Choi, B.H., Eum, H.M., Kim, H.S., Jeong, W.M. & Shim, J.S., 2004. Wave-tide-surge coupled simulation for typhoon Maemi, Workshop on waves and storm surges around Korean peninsula, 121-144.
Choi, K.S., & Kim, B.J., 2007. Climatological characteristics of tropical cyclone making landfall over the Korean Peninsula. Journal of the Korean Meteorological Society 43, 97-109.
Clark, J.D. & Chu, P., 2002. Interannual variation of tropical cyclone activity over the central North Pacific. Journal of the Meteorological Society of Japan, 80, 403-418.
Davies, A.M. & Flather, R.A., 1978. Application of numerical models of the North West European continental shelf and the North Sea to the computation of the storm surges of November to December 1973.
Deutsche Hydrographische Zeitschrift Ergänzungsheft Reihe A, 14, 72. Flow Science, 2010. FLOW-3D User’s Manual. Fujita, T., 1952. Pressure distribution in a typhoon. Geophysical Magazine 23.
Garratt, J.R., 1977. Review of drag coefficients over oceans and continents. Monthly Weather Review, 105, 915-929.
Gary Padgett, 2004. Gary Padgett September 2003 Tropical Weather Summary. Typhoon 2000.
Goda Y., Kishira Y. and Kamiyama Y., 1975. Laboratory investigation on the overtopping rate of seawalls by irregular waves, Report of Port and Harbour Research Inst.,14(4), 3-44.
Heaps, N.S., 1965. Storm surges on a continental shelf. Philos. Trans. R. Soc. London, Ser. 257, 351-383.
Hirt, C.W. and Nichols, B.D., 1981. Volume of fluid (VOF) method for the dynamics of free boundaries. Journal of Computational Physics, 39, 201-225.
Holland, G.J., 1980. An Analytic Model of the Wind and Pressure Profiles in Hurricanes. Monthly Weather Review, 108, 1212-1218.
Independent Levee Investigation Team, 2006. Investigation of the Performance of the New Orleans Flood Protection Systems in Hurricane Katrina on August 29, 2005
Klotzbach, P. J. , 2006. Trends in global tropical cyclone activity over the past twenty years (1986-2005). Geophysical Research Letters, 33.
Large, W.G. & Pond, S., 1981. Open ocean momentum flux measurements in moderate to strong winds. Journal of Physical Oceanography, 11, 324-336.
Landsea, C.W., Nicholls, N., Gray, W.M. & Avila, L.A., 1996. Downward trends in the frequency of intense Atlantic hurricanes during the past five decades. Geophysical Research Letters, 23, 1697-1700.
Lighthill, J., Holland, G., Gray, W., Landsea, C., Creig, G., Evans, J., Kurikara, Y. and Guard, C., 1994. Global climate change and tropical cyclones. Bulletin of the American Meteorological Society, 75, 2147- 2157.
Luettich, R.A. & Westerink, J.J., 2004. Formulation and Numerical Implementation of the 2D/3D ADCIRC finite element model version 44.XX.
Matsumoto, K., Takanezawa, T. & Ooe, M., 2000. Ocean tide models developed by assimilating TOPEX/POSEIDON altimeter data into hydrodynamical model: A global model and a regional model around Japan, Journal of Oceanography, 56(5) 567-581.
Mitsuyasu, H. and Kusaba, T., 1984. Drag Coefficient over Water Surface Under the Action of Strong Wind. Natural Disaster Science, 6, 43-50.
Mitsuyasu, H., F. Tasai, T. Suhara, S. Mizuno, M. Ohkusu, T. Honda and K. Rikiishi, 1980. Observation of the power spectrum of ocean waves using a cloverleaf buoy. Journal of Physical Oceanography, 10, 286- 296.
Multiple Lines of Defense Assessment Team, 2007. Comprehensive Recommendations Supporting the Use of the Multiple Lines of Defense Strategy to Sustain Coastal Louisiana.
Myers, V.A. and Malkin, W., 1961. Some Properties of Hurricane Wind Fields as Deduced from Trajectories. U.S. Weather Bureau, National Hurricane Research Project, Report 49.
Saito, K., T. Fujita, Y. Yamada, J. Ishida, Y. Kumagai, K. Aranami, S. Ohmori, R. Nagasawa, S. Kumagai, C. Muroi, T. Kato, H. Eito and Y. Yamazaki, 2006. The operational JMA Nonhydrostatic Mesoscale Model. Monthly Weather Review, 134, 1266-1298.
Shibaki H., Nakai K., Suzuyama K. and Watanabe A., 2004. Multi-level storm surge model incorporating density stratification and wave-setup. Proc. of 29th Int. Conf. on Coastal Eng., ASCE, 1539-1551.JSCE (1999). Hydraulic formulas, page 245 (in Japanese).
Shibaki, H., Suzuyama, K., Kim, J.I., & Sun, L., 2007. Numerical simulation of storm surge inundation induced by overflow, overtopping and dike breach. Asian and Pacific Coasts 2007, Nanjing, China.
Smagorinsky J., 1963. General circulation experiments with the primitive equations: I. The basic experiment. Monthly Weather Review, 91, 99- 164.
Smith, S.D. & Banke, E.G., 1975. Variation of the sea surface drag coefficient with wind speed. Quarterly Journal of the Royal Meteorological Society, 101, 665-673.
Versteeg, H.K., Malalasekera, W., 1995.An introduction to computational fluid dynamics. The Finite Volume Method. Prentice Hall, 257p.
Wang Xinian, Yin Qingjiang, Zhang Baoming, 1991. Research and Applications of a Forecasting Model of Typhoon Surges in China Seas. Advances In Water Science.
Wu, J., 1982. Wind-Stress Coefficients over Sea Surface from Breeze to Hurricane. Journal of Geophysical Research, 87, 9704-9706.
Yeh, H., Liu, P., Synolakis, C., 1996. Long-wave Runup Models. World Scientific.
Yakhot, V. and Orszag, S.A., 1986. Renormalization group analysis of turbulence, I. Basic theory. Journal of Scientific Computing, 1, 1-51.
Yakhot, V. and Smith, L.M., 1992. The renormalization group, the expansion and derivation of turbulence models, Journal of Scientific Computing, 7, 35-61
Yasuda, T., T. Hiraishi, H. Kawai, K. Nagase, S.W. Kang, and W.M. Jeong, 2005. Field survey and computation analysis of storm surge disaster in Masan due to Typhoon Maemi, Proceedings of Asian and Pacific Coasts 2005, Jeju, Korea.