• 전자공학회논문지A
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• 제32A권3호
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• pp.1-9
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• 1995

In the B-ISDN using satellite between geo-satellites and earth stations, the laser having high security and broad band width has to be used as a carrier for transmitting massive information of visual, vocal, and high rate data. In this paper, by computer simulation we analyzed the number of optical detector array of optical satellite communication downlink in case of using channel coding and no channel coding for BISDN between geo-satelites and earth stations under clear weather condition. It was supposed that 1 watt semiconductor laser was used and as modulation method, the binary FSK was used. The data rate of 10Gbps was used for B-ISDN. Also, hardly affected by atmospheric absorption 1.55$\mu$m wave-length was used to reduce influence of dispersion and chirp generated at a high speed transmission. We analyzed the received power, SNR and BER. The number of optical detector array was determined to satisfy for the BER less than 10$^{-7}$. Also, we ananlyzed the possibility of reducting the number of optical detector array in case of using channel coding. the number of optical detector array is one in the region where the elevation nangle is between 38$^{\circ}$ and 90$^{\circ}$ and two where the elevation angle is between 33$^{\circ}$ and 37$^{\circ}$ and three where the elevation angle is between 30$^{\circ}$ and 32$^{\circ}$ and increases per one as the elevation angle decreases per 1.deg.. So in the region where the elevation angle is 25$^{\circ}$, the number of optical detector arrays is eight. In case of using channel coding, the number of optical detector arrays decreases to five in the region where the elevation angle is 25$^{\circ}$. Therefore, we remaark the advantage of the channelcoding to decrease the size of received antenna and the number ob optical detector arrays.

• 대한토목학회논문집
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• 제29권4B호
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• pp.365-376
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• 2009

조위발생빈도분포가 상이한 우리나라 해역에 위치한 해안구조물의 마루높이를 설정하는 문제에 있어서 조위의 합리적인 취급이 중요하다. 권혁민 등(2005, 2006)은 해역별 기대월파확률 계산결과로서 조위발생빈도분포의 편차가 크면 클수록 작아지는 경향이 명백함을 보였다. 이는 년 단위 조위의 발생빈도분포가 년 최대파고 급의 파 발생빈도분포와 년 중 언제든 조우 할 수 있다는 가정을 내포하고 있다. 본 연구에서는 파와 조위의 조우 가능성을 년 최대 파급의 파가 발생할 수 있는 여름철 또는 겨울철을 대상으로 계절별 일 최대 조위발생빈도분포를 불확정요소로 취급하여 계산했다. 계산결과, 우리나라 전해역의 기대월파확률이 1%미만으로 수렴됨이 확인되어 이를 시나리오로 제안하고자 한다. 본 시나리오에 의하면 기대월파확률이 동일하도록 마루높이의 설정이 우리나라 전 해역을 대상으로 가능함을 확인하였다. 본 연구에서 마루높이는 전 해역에 대하여 계절별 일 최대조위의 평균값으로부터 설정이 가능한 것으로 추정된다.

• Journal of Advanced Research in Ocean Engineering
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• 제3권2호
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• pp.53-58
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• 2017

This study introduces the case of pipelines installed in subsea conditions and buried offshore. Such installations generate pore water pressure under the seabed because of cyclic wave excitation, which is an environmental load, and consistent cyclic wave loading that reduce the soil shear strength of the seabed, possibly leading to liquefaction. Therefore, in view of the liquefaction of the seabed, stability of the subsea pipelines should be examined via calculations using a simple method for buried subsea pipelines and floating structures. Particularly, for studying the possible liquefaction of the seabed in regard to subsea pipelines, high waves of a 10- and 100-year period and the number of occurrences that are affected by the environment within a division cycle of 90 s should be applied. However, when applying significant wave heights (HS), the number of occurrences within a division cycle of 3 h are required to be considered. Furthermore, to research whether dynamic vertical load affect the seabed, mostly a linear wave is used; this is particularly necessary to apply for considering the liquefaction of the seabed in the case of pile structure or subsea pipeline installation.

• International Journal of Naval Architecture and Ocean Engineering
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• 제2권3호
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• pp.127-131
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• 2010

A two-layer fluid with free surface is simulated in the time domain by a two-dimensional potential-based Numerical Wave Tank (NWT). The developed NWT is based on the boundary element method and a leap-frog time integration scheme. A whole domain scheme including interaction terms between two layers is applied to solve the boundary integral equation. The time histories of surface elevations on both fluid layers in the respective wave modes are verified with analytic results. The amplitude ratios of upper to lower elevation for various density ratios and water depths are also compared.

• The Korean Journal of Ecology
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• 제13권4호
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• pp.321-329
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• 1990

An investigation was performed to elucidate wave character of the timber line on the middle slope of the west side of Paektusan. The Betula ermanii forest, which composes the timber line on about 2, 060m elevation of sea level, is the pure community of B. ermanii. Diffraction pattern of wave distribution of B. eramnii due to boundary condition of alpine temperature gradient was found out on the timber line. Interference patterns of waves of B. ermanii communities produced by environment conditions such as soil layers, whids, snow and relief were shown on a specific area. These facts indicate that the B. ermanii individuals have wave and particle duality, the complementarity principle.

• 산업기술연구
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• 제8권
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• pp.3-11
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• 1988

Shock pressure of wave breaking on vertical wall is studied experimentally with beaches, which have four different slopes (1/4.02, 1/7.05, 1/10, 1 /13.5). This results is summerized as follows: 1. Maximum impact presures are occured where the wave break directly on the wall rather than breaking in front of the wall. 2. Deep water steepness, and the beach slope are the two Quantities governing the magnitude and location of maximum dimensionless impact pressure from wave breaking directly on the wall, also, the greatest pressure is produced with a beach slope of 1/10. 3. This study is clearly shown that the location of maximum pressure can be presented above still water level under respectively experimental condition. The dimensionless elevation of maximum Pressure is greatest on a beach slope of 1/10.

• 한국수산과학회지
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• 제20권4호
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• pp.370-378
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• 1987

Wave reflection control functions of mound for the foundation of composite and perforated break-waters were investigated through the theoretical considerations. The theory developed is based on a simple summation of components of reflected waves. The applicability of the theory is assured by the comparative studies of the theoretical calculation and experimental data on the sea surface elevation in front of a breakwater. It is found that the reflection is mainly controlled by depth and width of the mound. In the design of composite type perforated breakwaters, the width of perforated part of the upright section can be decreased to less than half of the conventional design width for the same reflection by using the reflection control function of mound part and the reflection can be reduced until less than $30\%$ of that in the composite breakwaters. Using the results, a design method of mounds is proposed, by which the reduction of wave reflection is assured under the given wave conditions.

• 한국해안·해양공학회논문집
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• 제24권3호
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• pp.217-227
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• 2012

2007년 3월 31일에 영광을 비롯한 한반도 서해안에 발생한 이상파랑의 발생 원인을 관측자료와 수치모델을 이용하여 분석하였다. 사용된 자료는 조위 관측소에서 관측된 조위 자료와 AWS의 해면기압 자료로서 모두 1분 간격의 시계열 자료이다. 이러한 시계열 자료를 시간과 주기에 대한 에너지 성분으로 변환시켜줄 수 있는 웨이블렛 변환을 이용하여 이상파랑과 같이 단기적으로 불규칙하게 발생하는 변화를 분석하였다. 분석 결과를 이용하여 이상파랑의 도달시간과 진행방향을 도출하였고, 생성원인을 분석하기 위해 AWS 자료를 통해 기압 점프의 크기와 주기 및 진행방향에 대해 조사하였다. 3시간 간격의 분석일기도에 제시된 기압 분포를 이용하여 서해상에서 기압 점프의 이동 패턴을 유추하였다. 분석된 결과의 타당성을 검증하기 위해 2차원 수치모형을 이용하여 이상파랑에 대한 모의를 수행하였다. 기압 점프의 진행에 따라 발생된 해수면의 변동은 공진작용에 의해 수위가 증가하는 것으로 나타났다. 산정된 수위는 관측값과 비교할 때 과소 산정되는 것으로 나타났으나, 웨이블릿 변환을 통해 분석한 도달순서와 유사하게 수위 관측지역에 도달하는 것으로 산정되었다.

• 대한토목학회논문집
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• 제29권5B호
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• pp.463-472
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• 2009

본 연구에서는 잠제가 설치된 연안역에서 해안의 곡률반경이 잠제 주변 파동장에 미치는 영향을 파악하기 위하여 파 구조물 해빈/해저지반의 상호작용을 해석할 수 있는 3차원 수치모델 LES-WASS-3D를 이용하여 시뮬레이션을 실시하였다. 먼저 기존의 수리모형실험결과와 비교 검토를 통하여 타당성과 유효성을 확인하였으며, 수치실험을 통해 얻어진 수치해석결과로부터 잠제 주변의 파고분포, 평균수위분포, 상층흐름분포, 평균류분포 그리고 연안에서의 처오름 높이분포를 비롯한 잠제 주변의 3차원적 수리특성에 미치는 해안곡률의 영향에 관하여 고찰하였다.

• 한국해양공학회지
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• 제22권5호
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• pp.44-51
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• 2008

The planning and design of coastal structures against wave attack is required to accurately predict wave transformation, wave run-up, and fluid. particlevelocities an a slope. On tire other hand, in tire swash and surf zones of a natural beach, where coastal erosion and accretion occur at tire land-sea boundary, hydrodynamic analysis is essential. In this study, a RBREAK2 numerical model was created based on the nonlinear shallow water equation and laboratory measurements were carried out in terms of tire free surface elevations and velocities for tire cases of regular and irregular waves on 1 : 10 and 1 : 5 impermeable slopes. The data were used to evaluate tire applicability and limitations of tire RBREAK2 numerical model. The numerical mode1 could predict tire cross-shore variation of the wave profile reasonably well, but showed more accurate results for slopes that were steeper than 1 : 10. Except near tire wave crest, tire computed depth averaged velocities could represent tire measured profile below tire trough level fairly well.