Simulation of the extreme waves generated by typhoon Bolaven (1215) in the East China Sea and Yellow Sea

JUN Ki Cheon; JEONG Weon Mu; CHOI Jin Yong; PARK Kwang Soon; JUNG Kyung Tae; KIM Mee Kyung; CHAE Jang Won; QIAO Fangli

doi:10.1007/s13131-015-0779-4

doi: 10.1007/s13131-015-0779-4

1.
Coastal Disaster Research Center, Korea Institute of Ocean Science and Technology, Ansan 426-744, Republic of Korea
2.
Coastal & Environmental Engineering Division, Korea Institute of Ocean Science and Technology, Ansan 426-744, Republic of Korea
3.
Marine Radionuclide Research Center, Korea Institute of Ocean Science and Technology, Ansan 426-744, Republic of Korea
4.
First Institute of Oceanography, State Oceanic Administration, Qindao 266061, China

基金项目: The Ministry of Oceans and Fisheries of Korea -"The Research and Development on Coastal Hydraulic Investigation of Busan New Port" and "Cooperative Project on Korea-China Bilateral Committee on Ocean Science"; the Korea Institute of Ocean Science and Technology (KIOST) Project under contract No. PE99325; the China-Korea Joint Ocean Research Center (CKJORC)-"Cooperation on the Development of Basic Technologies for the Yellow Sea and East China Sea Operational Oceanographic System (YOOS)"; both the Nuclear Safety Project of CKJORC and Major Project of KIOST under contract No. PE99304.

计量
- 文章访问数: 1641
- HTML全文浏览量: 33
- PDF下载量: 2822
- 被引次数: 0
出版历程
- 收稿日期: 2015-07-20
- 修回日期: 2015-09-21

Simulation of the extreme waves generated by typhoon Bolaven (1215) in the East China Sea and Yellow Sea

1.
Coastal Disaster Research Center, Korea Institute of Ocean Science and Technology, Ansan 426-744, Republic of Korea
2.
Coastal & Environmental Engineering Division, Korea Institute of Ocean Science and Technology, Ansan 426-744, Republic of Korea
3.
Marine Radionuclide Research Center, Korea Institute of Ocean Science and Technology, Ansan 426-744, Republic of Korea
4.
First Institute of Oceanography, State Oceanic Administration, Qindao 266061, China

摘要

- /
- /
- /
- /
Abstract: Record-breaking high waves occurred during the passage of the typhoon Bolaven (1215) (TYB) in the East China Sea (ECS) and Yellow Sea (YS) although its intensity did not reach the level of a super typhoon. Winds and directional wave measurements were made using a range of in-situ instruments mounted on an ocean tower and buoys. In order to understand how such high waves with long duration occurred, analyses have been made through measurement and numerical simulations. TYB winds were generated using the TC96 typhoon wind model with the best track data calibrated with the measurements. And then the wind fields were blended with the reanalyzed synoptic-scale wind fields for a wave model. Wave fields were simulated using WAM4.5 with adjustment of C_d for gust of winds and bottom friction for the study area. Thus the accuracy of simulations is considerably enhanced, and the computed results are also in better agreement with measured data than before. It is found that the extremely high waves evolved as a result of the superposition of distant large swells and high wind seas generated by strong winds from the front/right quadrant of the typhoon track. As the typhoon moved at a speed a little slower than the dominant wave group velocity in a consistent direction for two days, the wave growth was significantly enhanced by strong wind input in an extended fetch and non-linear interaction.
- extreme waves /
- typhoon /
- measurements /
- numerical simulation /
- East China Sea

HTML全文

参考文献(33)

Allan J C, Komar P D. 2002. Extreme storms on the Pacific northwest coast during the 1997-98 El Niño and 1998-99 La Niña. J Coast Res, 18(1):175-193

Bender C, Smith J K, Kennedy A, et al. 2013. STWAVE simulation of Hurricane Ike:model results and comparison to data. Coast Eng, 73:58-70

Bidlot J -R. 2012. Present status of wave forecasting at ECMWF. In:The ECMWF Workshop on Ocean Waves. Reading, United Kingdom:ECMWF Bouws E, Komen G J. 1983. On the balance between growth and dissipation in an extreme depth-limited wind-sea in the southern North Sea. J Phys Oceanogr, 13(9):1653-1658

Cardone V J, Greenwood C V, Greenwood J A. 1992. Unified program for the specification of hurricane boundary layer winds over surfaces of specified roughness. Final Report, Contract Report CERC-92-1, Dept of the Army, WES, Vicksburg, MS Chae J W, Jeong W M, Jun K C, et al. 2013. Extreme waves generated by typhoon Bolaven (201215) in Southern Korean Waters. In:Proceedings of the 7th APAC, Bali, Indonesia Cox A T, Cardone V J. 2000. Operational system for the prediction of tropical cyclone generated winds and waves. In:Proceedings of the 6th International Workshop on Wave Hindcasting and Forecasting. Monterey, California Dolan R, Davis R E. 1992. An intensity scale for Atlantic coast northeast storms. J Coast Res, 8(4):840-853

Donelan M A, Haus B K, Reul N, et al. 2004. On the limiting aerodynamic roughness of the ocean in very strong winds. Geophys Res Lett, 31(18), doi: 10.1029/2004GL019460

DY Engineering (DY Eng.). 2012. Proposal of detail design for the damaged breakwaters' repair works of Seogwipo Harbor. Internal Report (in Korean)

Evans A D, Falvey R J. 2012. Annual tropical cyclone report. JTWC, 117

Günther H. 2005. WAM cycle 4.5 version 2.0. Institute for Coastal Research, GKSS Research Centre, Geesthacht, Germany Gusdal Y, Carrasco A, Furevik B R, et al. 2010. Validation of the operational wave model WAM and SWAN-2009. Norwegian Meteorological Institute Report 18/2010, Oslo, 24

Hasselmann K, Barnett T P, Bouws E, et al. 1973. Measurements of wind-wave growth and swell decay during the Joint North Sea Wave Project (JONSWAP). Dtsch Hydrogr Z, 12:A8

Holland G J. 1980. An analytic model of the wind and pressure profiles in hurricanes. Mon Wea Rev, 108:1212-1218

Holthuijsen L H, Powell M D, Pietrzak J D. 2012. Wind and waves in extreme hurricanes. J Geophys Res, 117(C9):C09003

Hu Kelin, Chen Qin. 2011. Directional spectra of hurricane-generated waves in the Gulf of Mexico. Geophys Res Lett, 38(19):L19608

Japan Meteorological Agency (JMA). 2012. Annual report on the activities of the RSMC Tokyo-Typhoon Center:92

Jensen R E, Gunther H, Janssen P A E M. 2007. Updates to WAM Cycle 4.5+. In:Proceedings of the 10th International Works on Wave Hindcasting and Forecasting. Hawaii Jeong W M, Jun K C, Ryu K H, et al. 2012. Wave climate around Seogwipo Harbor induced by typhoon Bolaven. In:Proceedings of the 20th Conference of Korean Society of Coastal and Ocean Engineers (in Korean), Special Vol:3-13

Kim C S, Lim H S, Jeong J Y, et al. 2014. Responses of coastal waters in the Yellow Sea to typhoon Bolaven. J Coast Res, (70):278-283

Komen G J, Caverleri L, Donelan M, et al. 1994. Dynamics and modelling of ocean waves[dissertation]. Cambridge:Cambridge University Press Korea Hydrographic and Oceanographic Administration (KHOA). 2012. Data report of typhoon Bolaven (201215) (in Korean)

Korea Meteorological Agency (KMA). 2013. 2012 Typhoon report, technical report 2013-7, 375

Korea Ocean Research & Development Institute (KORDI). 2005.Wave hindcasting for the estimation of deep-water design waves in Korean Waters (in Korean), Report Ⅱ Moon I -J, Isaac G, Hara T, et al. 2003. Numerical simulation of sea surface directional wave spectra under hurricane wind forcing.J Phys Oceanogr, 33(8):1680-1760

Osborne A R, Onorato M, Serio M. 2000. The nonlinear dynamics of rogue waves and holes in deep-water gravity wave trains. Phys Lett, 275(5-6):386-393

Park W S. 2012. Breakwater damages of Seogwipo harbor by typhoon Bolaven:its causes and suggested remedies. In:Proceedings of the 20th Conference of Korean Society of Coastal and Ocean Engineers (in Korean), Special Vol:15-34

Powell M D, Murillo S, Dodge P, et al. 2010. Reconstruction of hurricane Katrina's wind fields for storm surge and wave hindcasting.Ocean Eng, 37(1):26-36

Powell M D, Vickery P J, Reinhold T A. 2003. Reduced drag coefficient for high wind speeds in tropical cyclones. Nature, 422:270-283

Shim J S, Min I K, Lee D Y. 2005. Analysis of data observed at Ieodo Ocean Research Station and buoy. In:Proceedings of the Joint Conf. on Ocean Science and Tech. Korea Association of Ocean Science of Technology Society (in Korean), May, Korea, 8

Suh K D, Kim M, Kim S W. 2012. Comparison of calculation methods of cumulative damage to breakwater armor layer. J Waterway Port Coastal Ocean Eng,139(4):277-285, doi: 10.1061/(ASCE)WW.1943-5460.0000181

The WAMDI Group. 1988. The WAM model-a third generation ocean wave prediction model. J Phys Oceanogr, 18(12):1775-1810

Thompson E F, Cardone V J. 1996. Practical modeling of hurricane surface wind fields. J Waterway Port Coastal Ocean Eng, 122(4):195-205

Tolman H L, Banner M L, Kaihatu J M. 2013. The NOPP operational wave model improvement project. Ocean Mod, 70:2-10

Van der Meer J W. 1987. Stability of breakwater armour layers-design formulae. Coast Eng, 11(3):219-239

Weber N. 1991. Bottom friction for wind sea and swell in extreme depth-limited situations. J Phys Oceanogr, 21(1):149-172

Wu Jin. 1982. Wind-stress coefficients over sea surface from breeze to hurricane. J Geophys Res, 87(C12):9704-9706

Young I R. 2006. Directional spectra of hurricane wind waves. J Geophys Res, 111(C8), doi: 10.1029/2006JC003540

Young I R, Vinoth J. 2013. An "extended fetch" model for the spatial distribution of tropical cyclone wind-waves as observed by altimeter.Ocean Eng, 70:14-24

Zijlema M, Van Vledder G, Holthuijsen L H. 2012. Bottom friction and wind drag for wave models. Coast Eng, 65:19-26

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 1641
HTML全文浏览量: 33
PDF下载量: 2822
被引次数: 0

doi: 10.1007/s13131-015-0779-4

计量

出版历程

Simulation of the extreme waves generated by typhoon Bolaven (1215) in the East China Sea and Yellow Sea

计量

出版历程

目录