• Title/Summary/Keyword: Simulating wave nearshore(SWAN)

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Analysis of Wave Distribution at Nakdong River Estuary Depending on the Incident Wave Directions Based on SWAN Model Simulation (SWAN 모델을 이용한 낙동강 하구역의 입사파향별 파랑분포 특성)

  • Park, Soon;Yoon, Han-Sam;Park, Hyo-Bong;Ryu, Seung-Woo;Ryu, Cheong-Ro
    • Journal of the Korean Society for Marine Environment & Energy
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    • v.12 no.3
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    • pp.188-196
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    • 2009
  • This study conducted numerical simulations to analyze the wave characteristics(distribution) depending on the directional changes of waves in the Nakdong river estuary by using SWAN(Simulating WAves Nearshore) model. The results from the tests are summarized as below. The wave height rates are generally highly distributed with the incident waves from the S, SSE, SSW, SE, SW in sequence. When the waves from the S, SSW, SSE directions are predominant, the bigger waves were observed in front of sandbars. According to the results of the wave steepness against the wave direction, at the east coast of Gadeok island(northwest of Nakdong estuary), where has mild seabed slopes, the wave height rates distribute in the range of 0.4~0.6; the wave height rates over the west coastal region of Dadeapo(southeast of Nakdong estuary) are 0.5~0.6. The wave height rate tends to be rapidly decreased over the east region of Nakdong river estuary rather than its west region.

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Study on Development of Surge-Tide-Wave Coupling Numerical Model for Storm Surge Prediction (해일-조석-파랑을 결합한 폭풍해일 수치모델 개발에 관한 연구)

  • Park, Jong-Kil;Kim, Myung-Kyu;Kim, Dong-Cheol;Yoon, Jong-Sung
    • Journal of Ocean Engineering and Technology
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    • v.27 no.4
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    • pp.33-44
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    • 2013
  • IIn this study, a wave-surge-tide coupling numerical model was developed to consider nonlinear interaction. Then, this model was applied and calculations were made for a storm surge on the southeast coast. The southeast coast was damaged by typhoon "Maemi" in 2003. In this study, we used a nearshore wind wave model called SWAN (Simulating WAves Nearshore). In addition, the Meyer model was used for the typhoon model, along with an ocean circulation model called POM (Princeton Ocean Model). The wave-surge-tide coupling numerical model could calculate exact parameters when each model was changed to consider the nonlinear interaction.

Analysis of Long-Term Wave Distribution at Jeju Sea Based on SWAN Model Simulation (SWAN모델을 이용한 제주해역 장기 파랑분포 특성 연구)

  • Ryu Hwangjin;Hong Keyyong;Shin Seung-Ho;Song Museok;Kim Do Young
    • Journal of the Korean Society for Marine Environment & Energy
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    • v.7 no.3
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    • pp.137-145
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    • 2004
  • Long-term wave distribution at Jeju sea is investigated by a numerical simulation based on the thirdgeneration wave model SWAN (Simulating WAves Nearshore). The Jeju sea which retains relatively high wave energy density among Korean coastal regions is considered to be a suitable site for wave power generation and the efficiency of wave power generation is closely related to local wave characteristics. The monthly mean of a large-scale long-term wave data from 1979 to 2002, which is provided by Korea Ocean Research & Development Institute. is used as the boundary condition of SWAN model simulation with 1km grid. An analysis of wave distribution concentrates on the seasonal variation and spatial distribution of significant wave heights, mean wave directions and mean wave periods. Significant wave heights are higher in winter and summer and the west sea of Jeju appears relatively higher than east's. The highest significant wave height occurs at the northeast sea in winter and the second highest significant wave height appears at the southeast sea in summer, while the significant wave heights in spring and autumn are relatively low but homogeneous. The distribution of wave directions reveals that except the rear region influenced by wave refraction, the northwest wave direction is dominant in summer and the southeast in winter. Wave periods are longer in summer and winter and the west sea of Jeju appears relatively longer than east's. The longest wave period occurs at the west sea in winter, and in summer it appears relatively homogeneous with a little longer period at the south sea.

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Review on Application of Wave Model for Calculation of Freeboard in Hydraulic Structure (수공구조물 여유고 산정을 위한 파랑모형의 적용성 검토)

  • Kim, Kyoung-Ho;Lee, Ho-Jin
    • Journal of Ocean Engineering and Technology
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    • v.21 no.1 s.74
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    • pp.25-30
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    • 2007
  • Most of dams and reservoirs were made from natural materials, such as soil, sand and gravel. This type of hydraulic structure has the danger of collapse by overflow during a flood. Freeboard is the vertical distance between the crest of the dam and the full supply level in the reservoir. It must be sufficient to prevent overtopping from over flow. Thus, freeboard determination involves engineering judgment, statistical analysis, and consideration of the damage that would result from the overtopping of a hydraulic structure. This study attempts to calculate the wave height in dam, which is needed for the determination of the freeboard of the dam. Chung-ju dam is selected as the study area. Using the empirical formulas, the wave heights in dam were calculated, and the results were compared with those by the SWAN model, which is a typical wave model. The difference between the calculated results from the empirical formulas and those by the SWAN model is considerably large. This is because empirical equations consider only fetch or fetch and wind velocity, while the SWAN model considers depth and topography data as well.

Examinations on the Wave Hindcasting of the Abnormal Swells in the East Coast (동해안 이상 너울 추산에 관한 고찰)

  • Kim, Tae-Rim;Lee, Kang-Ho
    • Journal of Ocean Engineering and Technology
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    • v.22 no.6
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    • pp.13-19
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    • 2008
  • Abnormally large swells that appeared on the coast of the East Sea in October in 2005 and 2006 were simulated using SWAN model to examine the accuracy of the model for future forecasting Seawind data calculated based on the weather chart ant bottom topography were used for input data, and the model was operated more than 20 days before the observed swells to avoid the problems from the cold start of the model. The comparisons with observed wind and wave data were unsatisfactory and neededmore improvement in terms of swell component in the wave model as well as the quality of seawind data. The satellite wind and wave data can be good candidates for future comparison of the wave model results in the East Sea.

SWAN을 이용한 파랑-바람 공존장에서의 파랑 특성에 관한 연구

  • Jeong, Jae-Hun;Lee, Seung-Geon
    • Proceedings of the Korean Institute of Navigation and Port Research Conference
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    • 2007.12a
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    • pp.127-128
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    • 2007
  • 파랑이 외해로부터 연안으로 내습하면서 발생되는 파랑 변형, 즉, 굴절, 회절, 천수 그리고 쇄파 동에 의한 변형을 일으킨다. 이러한 파랑변형을 일으키는 주된 물리적 인자는 수심의 변화이지만 태풍과 같은 강한 바람이 부는 해역에서는 바람인자를 반드시 고려해야만 한다. 본 연구에서는 바람효과가 고려된, 에너지 스펙트럼 모형 (SWAN; Simulating WAve Nearshore) 을 이용한 수치실험을 수행하였다. 그리고 해석해 및 Karlsson 모형에 대한 수치 해와 비교를 통해 모델의 검증을 실시하였다. 또한 부산항 설 해역을 대상으로 태풍 매미 내습 시 입사 파랑 조건을 적용하였으며 실제 관측 치와 바람효과의 유무에 따른 수치 계산치를 비교한 결과, 바람효과를 고려한 계산결과가 실제 관측치와의 양호한 일치를 나타내었다.

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Sensitivity of Input Parameters in the Spectral Wave Model

  • Park, Hyo-Bong
    • Journal of Ocean Engineering and Technology
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    • v.23 no.2
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    • pp.28-36
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    • 2009
  • Many researches have been done to define the physical parameters for the wave generation and transformation over a coastal region. However, most of these have been limited to the application of particular conditions, as they are generally too empirical. To yield more reasonable wave estimation using a spectral wave model, it is important to understand how they work for the wave estimation. This study involved a comprehensive sensitivity test against the spectral resolution and the physical source/sink terms of the spectral wave model using SWAN and TOMAWAC, which have the same physical background with several different empirical/theoretical formulations. The tests were conducted for the East Anglian coast, UK, which is characterized by a complex bathymetry due to several shoals and offshore sandbanks. For the quantitative and qualitative evaluation of the models' performance with different input conditions, the wave elements and spectrums predicted at representative sites the East Anglia coast were compared/analyzed. The spectral resolution had no significant effect on the model results, but the lowest resolution on the frequency and direction induced underestimations of the wave height and period. The bottom friction and depth-induced breaking terms produced relatively high variations in the wave prediction, depending on which formulation was applied. The terms for the quadruplet and whitecapping had little effect on the wave estimation, whereas the triads tended to predict shorter and higher waves by energy transferring to higher frequencies.

Optimization of SWAN Wave Model to Improve the Accuracy of Winter Storm Wave Prediction in the East Sea

  • Son, Bongkyo;Do, Kideok
    • Journal of Ocean Engineering and Technology
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    • v.35 no.4
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    • pp.273-286
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    • 2021
  • In recent years, as human casualties and property damage caused by hazardous waves have increased in the East Sea, precise wave prediction skills have become necessary. In this study, the Simulating WAves Nearshore (SWAN) third-generation numerical wave model was calibrated and optimized to enhance the accuracy of winter storm wave prediction in the East Sea. We used Source Term 6 (ST6) and physical observations from a large-scale experiment conducted in Australia and compared its results to Komen's formula, a default in SWAN. As input wind data, we used Korean Meteorological Agency's (KMA's) operational meteorological model called Regional Data Assimilation and Prediction System (RDAPS), the European Centre for Medium Range Weather Forecasts' newest 5th generation re-analysis data (ERA5), and Japanese Meteorological Agency's (JMA's) meso-scale forecasting data. We analyzed the accuracy of each model's results by comparing them to observation data. For quantitative analysis and assessment, the observed wave data for 6 locations from KMA and Korea Hydrographic and Oceanographic Agency (KHOA) were used, and statistical analysis was conducted to assess model accuracy. As a result, ST6 models had a smaller root mean square error and higher correlation coefficient than the default model in significant wave height prediction. However, for peak wave period simulation, the results were incoherent among each model and location. In simulations with different wind data, the simulation using ERA5 for input wind datashowed the most accurate results overall but underestimated the wave height in predicting high wave events compared to the simulation using RDAPS and JMA meso-scale model. In addition, it showed that the spatial resolution of wind plays a more significant role in predicting high wave events. Nevertheless, the numerical model optimized in this study highlighted some limitations in predicting high waves that rise rapidly in time caused by meteorological events. This suggests that further research is necessary to enhance the accuracy of wave prediction in various climate conditions, such as extreme weather.

Wave Energy Distribution at Jeju Sea and Investigation of Optimal Sites for Wave Power Generation (파력발전 적지 선정을 위한 제주 해역 파랑에너지 분포특성 연구)

  • HONG KEY-YONG;RYU HWANG-JIN;SHIN SEUNG-HO;HONG SEOK-WON
    • Journal of Ocean Engineering and Technology
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    • v.18 no.6 s.61
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    • pp.8-15
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    • 2004
  • Wave power distribution is investigated to determine the optimal sites for wave power generation at Jeju sea which has the highest wave energy density in the Korean coastal waters. The spatial and seasonal variation of wave power per unit length is calculated in the Jeju sea area based on the monthly mean wave data from 1979 to 2002 which is produced by the SWAN wave model simulation in prior research. The selected favorable locations for wave power generation are compared in terms of magnitude of wave energy density and distribution characteristics of wave parameters. The results suggest that Chagui-Do is the most optimal site for wave power generation in the Jeju sea. The seasonal distribution of wave energy density reveals that the highest wave energy density occurs in the northwest sea in the winter and it is dominated by wind waves, while the second highest one happens at south sea in the summer and it is dominated by a swell sea. The annual average of wave energy density shows that it gradually increases from east to west of the Jeju sea. At Chagui-Do, the energy density of the sea swell sea is relatively uniform while the energy density of the wind waves is variable and strong in the winter.

A Study on the Numerical Calculation for Shallow Water Waves Considering the Wind Direction Characteristics of Typhoon (태풍의 풍향특성을 고려한 천해파 산정에 관한 연구)

  • Lee, Kyung-Seon;Kim, Jung-Tae;Ryu, Cheong-Ro
    • Journal of Ocean Engineering and Technology
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    • v.21 no.1 s.74
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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.