• Journal of the korean society of oceanography
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• 제34권1호
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• pp.22-35
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• 1999

The response of the tidal waves to friction effect is investigated in terms of deformation of Kelvin and Poincare modes, The 1st Poincare mode does not exist over the low frequency region less than the critical frequency of omega ${\omega}$${\sqrt{2f}}$, with ${\gamma}$/f=0.0, but the mode comes to exist in the presence of friction. When friction exists and its magnitude increases, the wave number increases, indicating that the wave length of the Poincare mode becomes increasingly short with increasing friction. The damping coefficient gradually increases with increasing friction over the high frequency region, but the trend is reversed over the low frequency region. In case of Kelvin wave the present study substantiates the characters of Kelvin wave examined by Mofjeld (1980) and Lee (1988). Based on the examination of frictional effects on the tidal wave propagation, the co-oscillating tides in the Yellow Sea are examined by considering both the head opening and bottom friction effects. As friction is introduced and increased in addition to partial opening at bay head, the location of the amphidromic point near the Shantung Peninsula moves more southwestward. This southwestward movement of the amphidromic point is increasingly compatible with the observed location of Ogura's or Nishida's tidal chart of the M$_2$ tide.

• Journal of the korean society of oceanography
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• 제39권1호
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• pp.35-45
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• 2004

Based on the MASNUM wave-current coupled model, the temperature and salinity structures along $36^{\circ}N$ in the Yellow Sea are simulated and compared with observations. Both the position and strength of the simulated thermocline are similar to data analysis. The wave-induced mixing is strongest in winter and plays a key role in the formation of the upper mixed layer in spring and summer. Numerical experiments suggest that in the coastal area, wave-induced mixing and tidal mixing control the vertical structure of temperature and salinity.

• 한국해양공학회지
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• 제20권4호
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• pp.43-49
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• 2006

Detailed investigations were carried out on the stability of the dredged soil bed against wave actions, aimedat establishing the design method of artificial tidal flats using dredged soil. The soil was dredged at Nagoya port, Japan, and has a mean grain size of 0.013mm. Basic features of artificial dredged soil bed against wave actions were explained from a series of model experiments in a wave flume. The two types of section shapes were employed; one is a horizontal bed and the other is a sloped one. Changes of the bed profile, shear strength, grain size distribution and water content, according to the wave actions, were measured in detail. The cumulative effect of the wave actions, over about one week, was investigated. A dredged soil bed moves withthe wave actions with relatively small wave height. It should be especially. noted that the clay component is dissolved and flown out, away from the surface layer, and consequently the surface layer hardens, as if it is covered with sand. Wren the wave height is gradually increased, the bed is not liquefied and the shear strength of the dredged bed is increased by a wave-induced dissipation of pore pressures in the bed and a decrease of clay component by the wave-induced leakage.

• 한국해양공학회:학술대회논문집
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• 한국해양공학회 2002년도 춘계학술대회 논문집
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• pp.257-262
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• 2002

Numerical model introduced in this study combines wave refraction-diffraction, breaking, bottom friction, lateral mixing, and critical shear stress and three sub-models for simulating waves, currents, and bottom change were briefly discussed. Simulations of beach processes and harbor sedimentation were also described at the coast neighboring Bangpo Harbor, Anmyundo, Chungnam, where the area has suffered from accumulation of drifting sand in a small fishing harbor with a wide tidal range. We also made model test for the case of a narrow tidal range at Nakdong river's estuary area to understand the effect of water level variation on the littoral drift. Simulations are conducted in terms of incident wave direction and tidal level. Characteristics of wave transformation, nearshore current, sediment transport, and bottom change are shown and analyzed. We found from the simulation that the tidal level impact to the sediment transport is very important and we should apply the numerical model with different water level to analyze sediment transport mechanism correctly. Although the model study gave reasonable description of beach processes and harbor sedimentation mechanism, it is necessary to collect lots of field observation data, including waves, tides and bottom materials, etc. for better prediction.

• 한국해안·해양공학회논문집
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• 제30권6호
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• pp.286-297
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• 2018

본 연구에서는 황해역 파랑 특성을 파악하기 위해 KOGA-W01 파랑관측자료를 분석하고, 이를 바탕으로 파랑 후측모의 실험을 수행하였다. 파랑관측자료 분석에 따르면, 파랑관측지점이 연안역에 비교적 가까이 위치해 있음에도 불구하고 fetch length가 짧아 심해파 출현율이 높은 것으로 나타났다. 이에 본 연구에서는 Chun and Ahn(2017a, b)의 계산영역을 황해역으로 확장하여 파랑계산을 수행하였는데, 황해역에서의 정확한 파랑계산을 위해 조석 및 조류의 효과도 함께 고려하였다. 계산결과를 관측결과와 비교하여 파랑 후측모의의 정확도를 검증하였다. 본 연구의 전반적인 계산 결과의 정확도는 만족할 수준이지만, 계산영역 크기 한계로 S계열의 너울성 장주기파를 제대로 재현하지 못해 황해역 유의파주기의 정확도가 낮게 나타났다. 그러나 이들 장주기파의 파랑에너지가 크지 않아, 극치 파랑분석에의 영향은 작아 극치파랑의 유의파주기는 잘 재현하고 있는 것으로 나타났다.

• 한국멀티미디어학회논문지
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• 제15권2호
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• pp.258-265
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• 2012

우리나라는 매년 남해안 지역에 크고 작은 해일로 많은 인명과 재산 피해를 겪고 있다. 그러나 폭풍해일에 대한 많은 연구들이 진행되어 왔지만, 실제 생활현장에서 적용 가능한 해일탐지 및 예방시스템에 대한 연구가 필요하다. 본 연구에서는 현장 적용이 가능한 상황을 고려하여 CCTV 영상을 이용한 시간당 월파 횟수와 연안 범람의 위험성을 근사적으로 탐지할 수 있는 방재시스템을 제안한다. 그리고 연안범람의 위험이 감지되면 제안된 GIS기반 해일예방시스템은 관리자에게 신속하게 범람지역을 알려준다. 본 제안의 CCTV 영상분석은 맑은 날의 영상과 태풍 "뎬무" 진입시 연구실에서 촬영한 동영상을 기반으로 분석하였다.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 1982년도 제24회 수공학 연구발표회 논문초록집
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• pp.3-24
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• 1982

The relations between tidal fluctuation and freshwater discharge are stuied dy use of observed data in the estuarine region of the Nagdong Rivre. Damping modulus which represents the resistance to propagation of tidal wave is estimated, and it is verified that when the fresh water discharge is lower than 300 m/sec., the elevation of mean-water-level at Gupo is the same as mean sea-water-level.

• 환경영향평가
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• 제11권1호
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• pp.51-66
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• 2002

The purpose of this study is to analyze the geomorphological environment changes of tidal flat in the Cheonsu Bay. Especially, it centers on the changes in the sedimentary environment using remote sensing data. Multi-temporal Landsat data and topographic maps were used in this study. The results are summarized as follows: the tidal flat of Cheonsu Bay changes in many ways depending on the direction of the tidal current. In the neighborhood of Ganwoldo, the scale of the tidal flat has continuously been expanded due to the superiority of sedimentation after a tide embankment was built. When we analyzed the grain size of sediments and implemented in-situ field survey, it was found that the innermost part of the bay consists of a mud flat, with the midway part mixed flat, and the nearest part to the sea sand flat. On the other hand, in the neighborhood of Seomot isle and its beach, sedimentation is superior in the eastern part whereas erosion is superior in the western part. In other words, the western coast of the beach is contacted with the open seas and under much influence of ocean wave. The eastern coast is placed at the entrance of the bay and has sand bar and tidal flat developed due to submarine deposits that are accumulated on the sea floor by the tidal current. In conclusions, remote sensing methods can be effectively applied for quantitative analysis of geomorphological changes in tidal flat, and it is expected that the proposed schemes can be applied to another geomorphological environments such as beach, sand dune, and sand wave.

• 대한원격탐사학회지
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• 제25권3호
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• pp.225-231
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• 2009

The characteristics of morphological shapes, wave heights, tidal ranges and sediment sizes are observed and compared between intertidal beach and mudflat. The Mohang sand beach, southwest coast of Korea, is located just next to the large mudflat and has tidal range over 5 meters. Wave measurements are conducted at each entrance of the beach and mudflat as well as at the outside waters representing the incident waves to these different coastal environments. The morphological characteristics are also examined including the sediment size and the slope of the bathymetry, For the observation of morphological shapes, camera monitoring technique is used to measure the spatial information of intertidal bathymetry. The water lines moving on the intertidal flat/beach durinq a flood indicate depth contours between low and high water lines. The water lines extracted from the consecutive images are rectified to get the ground coordinates of each depth contours and integrated to provide three dimensional information of intertidal topography. The wave data show that sand beach is in the condition of severer wave forcing but tidal range is almost identical in both environment. The slope of the mudflat is much milder than the sand beach with finer sediment.

• 대한토목학회논문집
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• 제28권3B호
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• pp.307-313
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• 2008

방조제 건설로 인한 조석확폭 현상이 목포 북항은 물론 목포북항과 좁은 수로로 연결된 청계만에서도 발생되고 있다. 이러한 조석확폭 현상은 조간대를 증가시키고 특히 폭풍우시 수위 증가와 침수구간의 확대를 초래한다. 본 연구에서의 모의 과정은 광역에서의 풍파 모의와 협역에서의 풍파 범람 모의로 구성된다. 비선형 완경사 방정식이 바람에 의한 풍파는 물론 해일과 범람도 모의하도록 개선되었다. 개발된 모형은 청계만에 적용되었으며 목포 북항에는 청계만에서 발생하는 풍파로 인하여 발생할 수 있는 범람 형태를 파악하기 위하여 적용되었다.