• 한국수산과학회지
• /
• 제30권1호
• /
• pp.16-30
• /
• 1997

Application of digital filter to the wave analysis is studied using the observed data by wave gauge. Sea wave data obtained from wave gauge always include long wave frequency components. In order to estimate the sea wave parameters, we must re-analyzed wave data by using a digital filter and the concept of mean sea level correction method. By the wave by wave analysis and spectral methods, sea wave parameters on the basis of wave data obtained by the conventional method and digital filter are compared. The best-fitted design filter determined by the necessary conditions of frequency responses, can be obtained by calculating various transfer functions. Thus, to get the best the digital filter design, both Butterworth filter and Savitzky-Golay filter of digital filter are used in the frequency and time domain, respectively. Three cases of observation wave data are calculated by applying digital filter. The components of different frequency bands in the surf zone are coexisted in three cases. The wave data for wind wave components is computed using the digital filter the surf zone and off-surf zone, and based on the filtered data, wave parameters are calculated by the spectral analysis and wave by wave analysis methods, respectively. As a results, when sea wave data observed by wave gauge are analyzed, the Savitzky-Golay method is recommended which can well appear cut-off frequency by experimental choosing filter length in the time domain. The better mean sea level correction method is the Butterworth filter in the frequency domain.

• 드라이브 ㆍ 컨트롤
• /
• 제12권2호
• /
• pp.7-13
• /
• 2015

In this study, we suggested the wave power generator using horizontal motions of the wave for use in the coastal sea. The length of the horizontal movement of the wave in the vicinity of the sea surface is larger than the length of the vertical reciprocating movement of the wave, hence the proposed device has a wave power transmission plate. In addition, because the motion of the wave is maximum to the sea surface, by arranging the buoyancy tanks at the top of the wave power transmission plate, it is always capable of vertical movement in accordance with the sea surface. To confirm the usefulness of the proposed wave power generator, we constructed a mathematical model of the wave power generator and carried out simulation using bondgraph. Furthermore, the efficiency was verified by measuring the degree of electrical energy production through a preliminary experiment.

• 대한조선학회논문집
• /
• 제42권3호
• /
• pp.212-219
• /
• 2005

Real sea waves in a towing wave basin have been generated using random periodic motion of the segmented wave makers and the wave reflections of sidewalls. Theoretically, the real sea waves can be described by the superposition of many random oblique waves. This paper introduces numerical real sea wave generation in a rectangular wave basin using spectral method that uses a superposition of orthogonal functions which have to satisfy the Laplace equation. Oblique regular waves, long crested irregular waves and real sea waves were simulated and met the requirement of sidewall wave reflection and wave absorption. MLM (Maximum Likelihood Method) and Spatial Fourier Transform were used in order to obtain propagated wave direction characteristics. The estimated results proved the usefulness of the method and the performances showed reasonable directional patterns comparing with generating patterns.

• Journal of Advanced Marine Engineering and Technology
• /
• 제33권1호
• /
• pp.166-174
• /
• 2009

Gijang Sea is located on the southeastern coast of Korea. This study establishes a basic system to identify optimal sites for the wave power generation. To achieve this goal, the field measurements were made at the field site in front of Dong-am fishing port at Gijang. In addition, we analyzed the offshore wave data at the Donghae buoy operated by Korea Meteorological Administration(KMA) and compared the data with the wave characteristics in Gijang Sea. The main results were as follows. In winter, the wave direction in Gijang Sea ranged between east and south($90{\sim}180^{\circ}$). The main wave direction was east($90^{\circ}$). The Significant wave heights and periods were under 2 m and $5{\sim}15$ sec, respectively. A comparison of water depth and wave direction constitutes one(condition) of the important parameters for selecting the optimal site for the wave power generation.

• Ocean and Polar Research
• /
• 제29권1호
• /
• pp.9-31
• /
• 2007

Most seismic sea waves in the East Sea originate from earthquakes occurring near the Japanese west coast. While the waves propagate in the East Sea, they are deformed by refraction, diffraction and scattering. Though the Boussinesq equation is most applicable for such wave phenomena, it was not used in numerical modelling of seismic sea waves in the East Sea. To examine characteristics of seismic sea waves in the East Sea, numerical models based on the Boussinesq equation are established and used to simulate recent tsunamis. By considering Ursell parameter and Kajiura parameter, it is proved that Boussinesq equation is a proper equation for seismic sea waves in the East Sea. Two models based on the Boussinesq equation and linear wave equation are executed with the same initial conditions and grid size ($1min{\times}1min$), and the results are compared in various respects. The Boussinesq equation model produced better results than the linear model in respect to wave propagation and concentration of wave energy. It is also certified that the Boussinesq equation model can be used for operational purpose if it is optimized. Another Boussinesq equation model whose grid size is $40sec{\times}30sec$ is set up to simulate the 1983 and 1993 tsunamis. As the result of simulation, new propagation charts of 2 seismic sea waves focused on the Korean east coast are proposed. Even though the 1983 and 1993 tsunamis started at different areas, the propagation paths near the Korean east coast are similar and they can be distinguished into 4 paths. Among these, total energy and propagating time of the waves passing over North Korea Plateau(NKP) and South Korea Plateau(SKP) determine wave height at the Korean east coast. In case of the 1993 tsunami, the wave passing over NKP has more energy than the wave over SKP. In case of the 1983 tsunami, the huge energy of the wave passing over SKP brought about great maximum wave heights at Mukho and Imwon. The Boussinesq equation model established in this study is more useful for simulation of seismic sea waves near the Korean east coast than it is the Japanese coast. To improve understanding of seismic sea waves in shallow water, a coastal area model based on the Boussinesq equation is also required.

• 한국해양공학회:학술대회논문집
• /
• 한국해양공학회 2006년 창립20주년기념 정기학술대회 및 국제워크샵
• /
• pp.121-126
• /
• 2006

Modern Ocean wave forecasting systems predict the mean sea state, as characterized by the wave spectrum, in a box of size ${\Delta}x{\Delta}y$ surrounding a grid point at location x. It is shown that this approach also allows the determination of deviations from the mean sea state, i.e. the probability distribution function of the surface elevation. Hence, ocean wave forecasting may provide valuable information on extreme sea states.

• 한국항해항만학회지
• /
• 제27권2호
• /
• pp.111-119
• /
• 2003

해상수송의 안전성을 개선하는 하나의 수란으로서, 해상풍 정보로부터 예정 항로상에서 조우하게될 파랑정보를 높은 정밀도로 예측하여 단시간에 본선에 제공할 수 있는 시스템을 개발할 필요가 있다. 본 연구에서는 이의 제1단계로서 대양에서의 다방향 불규칙파 예측을 위한 파랑추산모델을 제시하였다. 검토방법으로는 과거 실제 해역에서 발생한 황천에 기인한 선박 침몰사고를 대상으로 선박의 항행 일정에 따른 해상풍의 분석 및 파랑추산시뮬레이션을 수행하였으며, 이로부터 사고 선박이 조우한 해상을 평가하고 모델의 재현성 및 정도를 검토하였다. 연구비 결과, 사고 선박은 침몰사고의 원인이 Okhotsk해에서 발달한 저기압에 의해 급속히 성장한 고파랑 해역을 회피하지 못하여 발생한 것에 있음을 명백히 하였으며, 본 계산에 이용한 제3세대 파랑추산모델(WAM)로부터의 결과는 실제 관측 파랑의 유의파고, 주기, 방향 스펙트럼 등 항행관련의 파랑제원과 잘 부합되었으며, 실용 선박에서의 예측시스템 구축에 적용성이 양호한 것으로 나타났다.

• 수산해양교육연구
• /
• 제12권2호
• /
• pp.199-212
• /
• 2000

It is very important to investigate the hull response of a fishing vessel in the sea to ensure the safe navigation and fishing operation in rough sea by preserving excellent sea keeping qualities. For this purpose, the author measured various responses of three stem trawlers in waves using real sea experimental measuring system. The author analyzed the experimental data using the statistical and spectral analyzing method to get the characteristics of the motion responses of the vessels according to the wave height and the ship's speed. The results obtained can be summarized as follows ; (1) Rather higher response of the pitch motion due to the wave height appeared in the head sea and the bow sea than any other wave direction without relevance to ship's size. In case of the roll motion, the beam sea and the quartering sea have a high response value. The period of peak of the pitch motion and the roll motion according to the wave height in each vessel has almost same value respectively. (2) The change of response of the pitch motions deeply depend on the ship's speed in the head sea and the bow sea, but not in the other wave direction. (3) The change of response of the roll motions in the beam sea, the quartering sea and the following sea are affected by the influence of the ship's speed in 5k't to 8k't, but not related to the ship's speed in out of that range.

• 한국항해항만학회:학술대회논문집
• /
• 한국항해항만학회 2003년도 춘계공동학술대회논문집
• /
• pp.147-156
• /
• 2003

해상수송의 안전성을 개선하는 하나의 수단으로서, 해상풍 정보로부터 예정 항로상에서 조우하게될 파랑정보를 높은 정밀도로 예측하여 단시간에 본선에 제공할 수 있는 시스템을 개발할 필요가 있다. 본 연구에서는 이의 제1단계로서 대양에서의 다방향 불규칙 예측을 위한 파랑추산모델을 제시하였다. 검토방법으로는 과거 실제 해역에서 발생한 황천에 기인한 선박 침몰사고를 대상으로 선박의 항행 일정에 따른 해상풍의 분석 및 파랑추산시뮬레이션을 수행하였으며, 이로부터 사고 선박이 조우한 해상을 평가하고 모델의 재현성 및 정도를 검토하였다.연구의 결과, 사고 선박은 침몰사고의 원인이 Okhotsk해에서 발랄한 저기압에 의해 급속히 성장한 고파랑 해역을 회피하지 못하여 발생한 것에 있음을 명백히 하였으며, 본 계산에 이용한 제3세대 파랑추산모델(WAM)로부터의 결과는 실제 관측 파랑의 유의파고, 주기, 방향 스펙트럼 등 항행관련의 파랑제원과 잘 부합되었으며, 실용 선박에서의 예측시스템 구축에 적용성이 양호한 것으로 나타났다.

• 물과 미래
• /
• 제10권1호
• /
• pp.101-117
• /
• 1977

The statatistical characteristics and spectra of sea waves at Mookho were analysed by several statistical methods. As the results, the following conclusions are obtained: 1. Values of surface elevation of sea wave are better fitted to Gram Charlier distribution than Gaussian distribution. This proves that sea waves have not only characters of irregularity but also non-linearity. 2. Distribution of maxima of surface elevation practically follows the distribution of Cartwright and Longuet-Higgins, also spectral width parameter is found to be increased with the increase of root mean square of surface elevation. 3. Sea wave may have spectrum of broad frequency band, however distributions of wave heights and periods follow the Rayleigh distribution which is derived from the assumption of narrow frequency band. 4. Ratios among mean wave heights from observed data show good agreements with theoretical values from Rayleigh distribution. 5. Spectral density and spectral width parameter increase with increase of wind velocity. And wave period at optimum band gas higher value than significant wave period by about 10 percent.