• 한국산학기술학회논문지
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• 제17권4호
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• pp.464-473
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• 2016

이산화탄소의 배출 증가와 지구온난화, 엘리뇨 현상, 라니냐 현상 등과 같은 이상기후 현상의 발생빈도 증가로 인하여 전 세계적으로 내륙과 해안의 온도가 상승하고 있다. 지구온난화로 인한 바닷물의 열팽창 그리고 빙하의 해빙 등으로 인한 지구의 해수면은 매년 2.0mm/yr(전 세계 평균값)의 속도로 상승하고 있다. 그러나 해안에 인접한 수리구조물 혹은 해안 수리구조물을 설계할 시 기준이 되는 설계조위는 과거 관측된 조위 값으로부터 4대 분조 및 조화상수를 분석하거나 수치모형 실험에 의해 결정된다. 따라서, 설계조위는 구조물의 설계빈도에 상응하는 해수면의 상승속도를 감안해야 할 필요가 있다고 사료된다. 본 연구에서는 국립해양조사원(Korea Hydrographic and Oceanographic Administration; KHOA)에서 운영하고 있는 46개소의 조위관측소를 대상으로 관측개시일부터 2015년까지 시단위로 조위자료를 수집하였다. 우리나라를 크게 남해동부, 남해서부, 동해남부, 동해중부, 서해남부, 서해중부, 제주로 총 7개의 해역으로 구분하여 월별, 연별 변동추이 및 연평균 상승률 분석을 수행하였다. 향후 국지적 해수면상승의 원인규명 및 설계조위 고려 시 기초자료로 활용가능 할 것으로 판단된다.

• 한국석유지질학회:학술대회논문집
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• 한국석유지질학회 2000년도 제7차 학술발표회 발표논문집
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• pp.14-30
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• 2000

Hierarchically controlled sequence stratigraphic analysis shows that the Lower Ordovician mixed carbonate-siliciclastic Mungok Formation, Korea consists of three depositional sequences: T1, T2, and T3. Sequence boundaries are generally marked by abrupt transition from coarse-grained shallow-water carbonates to fine-grained deeper-water carbonates mixed with fine-grained siliciclastics, and show indication of subaerial exposure such as karstification. Within this sequence stratigraphic framework, facies characteristics indicate that the Mungok sequences were mostly deposited in subtidal ramp environments. High-frequency cycles consist of upward-shallowing facies successions. Cycles of shallow-water and basinal deposits are not represented well, probably due to cycle amalgamation. Cycle stacking patterns do not show a consistent thickness change that reflects a large-scale sea-level change due to unfilled accommodation space. The Mungok sequences show that many factors including relative sea-level change and topography are involved in controlling sequence development on carbonate ramps. The depositional setting evolved from the high-energy ramps in the sequences T1 and T2 into the low-energy ramp in the sequence T3. Topography is interpreted to have been responsible for the different energy regimes of the carbonate ramps in the Mungok sequences. The high ramp gradient in the sequences T1 and T2 seems to be caused by space-time-dissociated differential sedimentation resulting in spatially narrow distribution of sediment filling, which in turn may be related to high rate of relative sea-level change. In contrast, low ramp gradient was maintained in the sequence T3 during slow changes of relative sea level resulting in broad distribution of sediment filling.

• 수산해양교육연구
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• 제25권1호
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• pp.1-11
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• 2013

The aim of this study was estimated the characteristics of the wave propagation by the water level conditions using a numerical modeling method at the Wando sea area. For three cases numerical simulation on the condition of incident and incoming of the deepwater design wave and the season normal wave, the spatial distribution of the incident wave at study area were investigated. And the calculated numerical modeling results were compared with measured field wave data. According to on-site wave data measured for 18 days, the range of the significant wave height and period were 0.10~1.14 m, 4.35~8.74 sec, respectively, and the maximum wave height were 0.15~1.66 m. From the results of numerical model for offshore design wave incident, the wave height attacked from Southern-East direction at this study area were over maximum 10.5 m because of rapidly change of water depth. Numerical modeling by three water level conditions of Approxmate Lowest Low Water Level(Approx. L.L.W), Mean Sea Level(M.S.L) and Approximate Highest High Water Level(Approx. H.H.W) were practiced. From the results for the case of Approx. H.W.L, variations of wave height at the back area of islands were about 1.6 m at maximum value for the case of deepwater design wave incoming. The significant wave heights of winter season were bigger than summer under normal wave condition, the incident wave height over 5.5 m decreased by shielding effect of islands. The change of maximum wave height at summer season were distinct than winter and was about 1.2 m and 0.8 m, respectively.

• 한국가시화정보학회지
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• 제9권4호
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• pp.74-79
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• 2011

In this study the change of free surface vortex is represented at different times according to height of water and with or without curtain wall installation. The air volume fraction is investigated at each condition of water level and the influence about creation of vortex is analyzed. The height of sump intake is taken as 100mm and the water level is divided into 5 steps. The sump model is the TSJ model and the curtain wall is applied by HI standard of America. The results shows that the free surface vortex can be identified on the isotropic surface at air volume fraction 1%~5% and the vortices make an air column from the free surface to the sump intake and are created and destroyed repeatedly. In the higher water level, less air is absorbed into the intake pipe. After curtain wall installation, the suction rate of the air volume fraction is decreased by 6.7%. The result of the vortex motion according to time, works on a cycle.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2017년도 학술발표회
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• pp.182-182
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• 2017

Many small island nations rely on groundwater as their only other source of freshwater in addition to rainwater harvesting. The volume of groundwater resource of small island nations are further limited by their smaller surface area and specific hydrogeology. The rapid growth of population and tourism has led to increasing water demands and pollution of available groundwater resources. The predicted climate change effects pose significant threats to the already vulnerable freshwater lens of small islands in the form of rise in sea level, coastal inundation, saltwater intrusion, varied pattern of precipitation leading to droughts and storm surges. The effects of climate change are further aggravated by manmade stresses like increased pumping. Thus small island water resources are highly threatened under the effects of climate change. But due to the limited technical and financial capacity most of the small island developing states were unable to conduct detailed technical investigations on the effects of climate change on their water resources. In this study, we investigate how well small island countries are preparing for climate change. The current state of freshwater resources, impacts of predicted climate change along with adaptation and management strategies planned and implemented by small island countries are reviewed. Proper assessment and management practices can aid in sustaining the groundwater resources of small islands under climate change.

• 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.

• 물과 미래
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• 제29권5호
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• pp.129-138
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• 1996

Loopnet은 폐합형수계에서 물의 흐름에 관한 시간적 공간적 변화를 계산할 수 있는 부정류 해석프로그램이다. 본 연구에서는 이 모형이 적용하고 있는 Looped Solution 알고리듬을 유도하고, 폐합형수계의 시험하도를 구성하여 이 모형의 안정성 및 정확성을 시험해 보았다. 또한 굴포천 유역을 대상으로 이 모형을 적용하여 수공 구조물, 서해측의 조위와 유역의 홍수 유입 등을 고려한 홍수위를 산정하였다. 그 결과 모형의 안정성 및 정확성 시험에서 신뢰할 만한 결과를 얻을 수 있었으며, 운하의 운영수위는 굴포천 본류와 방수로구간 모두 홍수위 변화에 큰 영향을 미치지 못하였으나, 조도계수는 홍수위 변화에 중요한 물리적 요소 중 하나로 분석되었다.

• Nuclear Engineering and Technology
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• 제52권12호
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• pp.2847-2851
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• 2020

A simple water level measurement method based on wavelength division multiplexing (WDM) is proposed and demonstrated. The measurement principle is based on the change of Fresnel reflection occurring at the end facet of the optical fiber tip (OFT). To increase the spatial resolution of water level sensing, a broadband light source (BLS) and an arrayed waveguide grating (AWG) are employed. The OFTs are multiplexed with the dedicated wavelength channels of AWG. By measuring all of the reflection powers reflected at the OFTs with a proposed on-site reflectometer, the water level can be monitored continuously for a fast emergency response. Moreover, it can be implemented easily with the commercially available optical components and devices with the simple configuration.

• 한국해안·해양공학회논문집
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• 제24권3호
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• pp.179-188
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• 2012

기후변화가 구조물의 안정성에 미치는 영향을 분석하기 위해 여러 수심에서 가상적으로 설계된 직립방파제의 성능을 평가하였다. 성능평가에서는 기후변화영향인 해수면 상승과 파고 증가를 고려한 성능설계법이 사용되었다. 성능설계법의 파랑변형 계산과정에서 많은 시간이 요구되는 문제를 극복하기 위해 범용 SWAN 모형에 인공신경망을 결합하였다. 학습된 인공신경망에 심해유의파고와 심해주파향 그리고 조위가 입력되면 구조물 위치에서 유의파고와 주파향이 신속하게 계산된다. 전반적으로 구조물의 안정성은 기후변화영향으로 감소하였지만 수심에 따라 서로 다른 경향을 보였다. 쇄파대 밖에서는 수심이 증가할수록 해수면 상승의 영향은 감소하고 파고 증가의 영향은 증가하였다. 한편, 쇄파대 내에서는 수심이 감소할수록 파고 증가와 해수면 상승의 영향 모두 감소하였다. 하지만 파고 증가의 영향이 해수면 상승의 영향보다 컸다. 이와 같은 결과를 반영하여 직립방파제의 유지보수 및 보강 대책을 수립해야 할 것이다.

• 한국콘크리트학회:학술대회논문집
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• 한국콘크리트학회 2009년도 춘계 학술대회 제21권1호
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• pp.553-554
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• 2009

광섬유센서 등과 같은 정밀온도센서를 이용하여 기온, 수온 및 수중 지표면 온도를 측정하고, 각각의 온도 변화에 대응하여 교량 세굴 및 수위를 파악할 수 있는 계측시스템을 개발하고 이를 소개한다. 온도계측을 통한 교량 세굴 및 수위 측정 방법은, 온도를 측정할 수 있는 센서를 수중 지표면을 기준으로 일정깊이와 높이로 설치하여 각각의 위치에 따른 온도 변화량을 분석하여 세굴량을 추정하는 시스템이며, 센서를 교각 상부까지 연장할 경우 수심 측정까지도 가능한 방법이다.