• 한국해양공학회:학술대회논문집
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• 한국해양공학회 2004년도 학술대회지
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• pp.229-234
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• 2004

A Typhoon wave is generated by wind fields during the Passage of Typhoon. Transporting wind field makes wind wave and swell in the open sea, and then, those wave components are transported in the shallow water. Typhoon waves in the shallow water is generated by Typhoon wind field and incident wave. Bisides, Incident waves to the shallow water are deformated by topographic conditions. This paper estimated the analysis of the Typhoon waves by wind fields and incident waves according to wave action balance equation model. As the result of wave numerical experiment, wave field during the passage of Typhoon 'Memi' in the shallow water is strongly effect by wind fields. Wave action balance equaion can be partially used for Typhoon wave simulations.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2006년도 학술발표회 논문집
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• pp.567-573
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• 2006

An efficient typhoon wave-generating model is applied to northeast Asia sea zone presented that can be used by civil defense agencies for real-time prediction and fast warnings on typhoon-generated wind wave and storm surge. Instead of using commercialized wave models such as WAM, SWAN, the wind waves are simulated by using a new concept of wavelength modulation to enhance broader application of the hyperbolic wave model of the mild-slope equation type. The results simulated along the Korean coasts during Typhoon Nabi (2005) showed reasonable agreement with the recorded wind waves.

• 한국해양공학회지
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• 제26권1호
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• pp.47-53
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• 2012

A coastal flood area was predicted using the empirical superposition of the typhoon surge level and typhoon wave height along the Busan coastal area. The historical typhoon damages were reviewed, and the coastal topography was measured using VRS-GPS. A FEMA formula was applied to estimate the coastal flood area in a typhoon case when the measured and predicted data of typhoon waves are not available. The results in the area of Haeundae beach and Gwangalli beach were verified using the flood area data from the case of Typhoon Maemi (2003). If a Hurricane Katrina class typhoon were to pass through the Maemi trajectory, the areathat would be flooded along theBusan coastal area was predicted and compared with the results of the Maemi case. Because of the lack of ocean environment data such as data for the sea level, waves, bathymetry, wind, pressure, etc., it is hard to improve the prediction accuracy for the coastal flood area in the typhoon case, which could be reflected in the policy to mitigate a typhoon's impact. This paper discusses the kinds of ocean environment information that is needed to predict a typhoon's impact with better accuracy.

• 한국해양공학회지
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• 제19권6호통권67호
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• pp.22-28
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• 2005

We investigated the characteristics of the overflow/wave overtopping, induced by the storm surge and high waves in Masan bay and Busan Coast during Typhoon 'Maemi', which landed at the southeast coast of the Korean peninsula on September, of 2003, causing a severe inundation disaster. Characteristics of the water level, increase by the overflow / wave overtopping, were discussed in two patterns. One is the increase of water level in the region, located inside of a bay, like Masan fishing port, and the waves are relatively small. The other is in the open sea, in which the waves act directly, as on the seawall in Suyong bay. In the former region, the water level increase was affected by the storm surge, as well as the long period oscillation and waves. In Masan fishing port, about $80\%$ of the water level increase on the quay wall was caused by the storm surge. In the latter one, it was greatly affected by the wave run-up. In Suyong bay, about $90\%$ of the water level increase on the seawall was caused by the wave run-up.

• 한국해양공학회지
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• 제21권1호
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• pp.1-6
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• 2007

While a typhoon is traveling, characteristics of its wind fields are continuously changing, producing severe changes in local water level and wave conditions, especially, when a typhoon comes into shallow water. However, there have not been many studies related to local typhoon effects, especially, considering real time changes of wind direction related to the coastal topography. In the study, the characteristics of the wind field by typhoon and topographical characteristics in shallow water are considered, as well as conditions of wave climate estimation. These are performed by the SWAN (Simulating waves nearshore) model, in order to estimate the growth of wave energy due to the wind field. It can be strongly suggested that the wave energy of theof an inner bay should be estimated when the direction of the bay entrance and the wind direction of the typhoon are identical. The result of the numerical calculations is in better agreement with the observed data than the result of the conventional estimation techniques.

• 수산해양기술연구
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• 제48권3호
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• pp.227-234
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• 2012

This paper describes the remote monitoring of breaking ocean waves generated by Typhoon Nabi, whose name means butterfly in Korean, using a marine X-band radar in the Yongho Man, Busan, Korea. The basic purpose of this study is to investigate the dynamic behavior and to estimate the periods of breaking waves across the surf zone from radar image sequences. In these experiments, the land-based radar system imaged the inshore zone of three miles from the coastline to a isobath of 30 meters. The wave period and the dominant wave direction for breaking ocean waves extracted directly from radar image sequences were 157.4 meters and 298 degrees, respectively. However, the result calculated quantitatively by the continuous wavelet transform (CWT) showed that the period of breaking waves was 154.3 meters. The average difference in breaking wave periods between the value extracted by using EBRL (electronic bearing and range line) of radar and the calculated value by CWT was 3.1 meters, showing that the CWT method is also accurate. These results suggest that a marine X-band radar system is a viable method of monitoring the breaking ocean waves.

• 한국항해학회지
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• 제13권3호
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• pp.45-65
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• 1989

Various typhoon data near Yongil Bay, Korea from 1961 to 1985 were collected with some critria and analyzed with the help of the computer. Introducing the pressure profile models and predicting the typhoon wind and wave fields, the 100-year design wave parameters were calculated. Additionally, the wave data at the southeast coast of Korea were statistically analyzed. The deep water wave climate of this bay indicated that Typhoon Brenda, 1985 had wave characteristics of 100-year return period, Typhoon model and storm surge model studies were made for this typhoon. These, including other design parameters, were introduced into the calculation of total design water depth.

• 한국해안해양공학회지
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• 제18권4호
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• pp.294-300
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• 2006

양해법의 하나인 풍상차분을 사용하는 WAM 모형의 수치기법을 분할차분법을 이용한 음해법으로 바꾸고 수치분산을 줄이기 위해 FCT 기법을 적용하였다. 새로운 수치기법의 특성을 확인하기 위해 구형파 전파실험과 태풍 매미로 인한 파랑모의를 수행하였다. 기존의 WAM 모형에 비해 현저히 수치분산을 줄일 수 있었고, 음해법의 이용으로 비교적 큰 시간 격자 간격에서도 안정적으로 계산이 수행되어, 보다 경제적인 수치모의가 가능함을 확인하였다.

• 한국해안·해양공학회논문집
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• 제35권4호
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• pp.67-74
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• 2023

열대성 저기압으로 인한 높은 파도와 폭풍해일은 해안지역에 큰 피해를 준다. 따라서 태풍이 내습하기 전에 정확하게 예측해야 하는데, 기상 강제력은 예측에 중요한 요소이다. 본 연구는 정확한 폭풍해일 및 파랑예측에 요구되는 기상 강제력을 위한 개선방안을 제시한다. 2016년 남해안을 강타한 태풍 차바를 사례연구로 하여, 기상예측모델(MPAS)로 태풍 트랙 및 기상 강제력, 즉, 기상장을 예측했다. 예측된 MPAS 태풍 트랙 정보를 기반으로 한 태풍의 대칭형 및 비대칭형 파라미터 와류 모델을 이용하여 기상 강제력을 생성하는 한편, 베스트 트랙 기반 동일 한 파라미터 모델을 이용하여 기상 강제력을 생성하여, 둘을 비교했다. 또한, MPAS 예측 태풍 트랙 정보 기반 대칭형/비대칭형 와류 파라미터 모델에서 생성된 기상장은 MPAS에서 예측한 기상장과 블렌딩하여 예측기상장을 만들었다. 이렇게 제작된 MPAS 기반 forecast 기상장 4종 및 베스트 트랙 기반 hindcast 기상장 2종을 ADCIRC+SWAN ADCIRC+SWAN에 입력하여 남해안의 파랑 및 폭풍해일을 예측/재현하고 관측치와 비교·검증했다. MPAS 기반 forecast 기상장을 이용하여 예측된 폭풍해일과 파랑은 관측치와 거의 일치했으며, 베스트 트랙을 사용하여 재현한 결과와도 견줄 만했다. 유의파고는, 6종의 기상장을 이용한 실험에서 MPAS 예측 태풍 트랙 기반 대칭형 와류 파라미터 모델로 생성된 기상장과 MPAS 예측 기상장을 블렌딩한 실험이 예측 정확도가 높았으나, 비대칭형 와류 파라미터 모델과 블렌딩을 사용한 경우보다 약간 높은 정도였다. 폭풍해일은, MPAS 예측 태풍 트랙을 이용한 비대칭형 와류 파라미터 모델에서 생성된 기상장을 이용한 실험이 예측 정확도가 높았다. 폭풍해일과 파랑을 정확하게 예측하기 위해서는, 정확한 태풍 트랙 정보와 이 정보가 반영된 비대칭형 와류가 고려된 기상장, 이 태풍 트랙을 생산한 기상장이 필요한 것을 볼 수 있다.

• 한국해안·해양공학회논문집
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• 제21권1호
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• pp.79-90
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• 2009

본 논문에서는 심해부터 천해에 까지 적용가능한 동적결합형 태풍 해일-조석-파랑 수치모델을 태풍 매미에 적용하여 모델의 안정성과 정확성을 검증하였다. 동적결합형 모델은 해수유동 모델인 POM을 수정한 모듈과 심해 풍파모델인 WAM을 심해부터 천해까지 적용가능하도록 수정한 모듈로 구성되어 있다. 수정 POM 모듈에서 조위, 조류 와 해일을 계산하며, 수정 WAM 모듈에서 풍파를 계산하여 상호 계산된 결과를 주고 받도록 결합된 동적결합형 모델이다. 수정 WAM 모듈에서는 잉여응력과 바람에 의한 마찰응력, 해수면 조도계수 등의 계산결과가 POM으로 제공되며 수정 POM 모듈에서는 유속, 조위면 등의 정보가 WAM으로 제공된다. 개발된 수치모델을 태풍 매미에 적용하여 계산된 결과를 관측된 파랑 및 조위자료와 비교하여 정확성을 검증하였다.