• Proceedings of the Korean Institute of Navigation and Port Research Conference
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• 2012.06a
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• pp.65-67
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• 2012

2011년 3월 센다이 앞바다 약 130km지점에서 엄청난 지진해일을 동반한 규모 9.0 초대형 지진이 발생하였다. 많은 지역에서 범람고가 10m를 상회하였으며, 큰 피해가 발생한 곳의 경우 지진해일의 처오름 높이가 23.6m에 달한 곳도 있었다. 이 쓰나미는 지진 발생후 30분만에 첫 번째 지진해일이 해안에 도달하였고, 이 후 수차례 반복하여 내습하였다. 이러한 지진해일의 대책중 하나는 지진해일 발생시 5~10분 이내에 기상청에서 경보를 발령하고 대피 체계를 구축하는 것이다. 이와 같은 이유로 본 연구에서는 지진해일을 검출하기 위한 기저거리 비종속 정밀측위기술을 제안하였다. 원해에서는 기준국과의 위치가 멀기 때문에 DGNSS의 사용이 힘들다. 그러므로 단독 GPS 측위에 영향을 주는 오차를 제거하고 Kalman filter를 이용하여 정확한 위치를 추정한다. 또한 성능 검증을 위한 파랑의 동적특성을 고려한 테스트베드를 개발하였고, 그 유용성을 검증하였다.

• Proceedings of the Korean Institute of Information and Commucation Sciences Conference
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• 1998.11a
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• pp.109-114
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• 1998

본 논문에서는 현재 우리 나라에서 사용하는 해양무선통신을 육상국을 중심으로 주파수, 서비스의 종류, 통신의 종류, 항만의 분포 둥을 조사 분석하였다. 특히 1998년 5월부터 서비스가 시작된 초단파대역의 해양이동전화에 대한 내용을 중점적으로 조사하여 기재하고 있다. 해양이동전화의 경우, 기지국의 위치, 망구축, 번호의 이용과 단말기의 보급, 서비스계획, 주요제원, 서비스의 특징 둥을 조사 분석하여, 새롭게 시작하는 해상이동전화에 대한 이해를 도모하였다. 일본에서는 1979년 3월부터 자동교환접속에 의한 해상이동전화서비스가 시작된 것과 비교해볼 때, 우리 나라의 해상이동전화서비스는 매우 늦은 감이 있지만, 도서지역 주민들에 대한 생활수준의 향상 둥에 많은 기여를 할 것으로 생각된다. 이러한 해상이동전화 서비스의 시작은 지역간 정보통신서비스제공의 불균형을 해소하고 낙후된 해안ㆍ도서지역의 통신서비스개선에 큰 역할을 담당할 것이다.

• Proceedings of the Korea Water Resources Association Conference
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• 2007.05a
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• pp.702-706
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• 2007

본 연구에서는 실측 강수 자료를 적용하여 장기 지하수위의 변동을 수치모의하고, 그 결과를 관측정으로부터 측정된 실측 지하수위와 비교하였다. 모형의 구축은 제주도 한라산 중산간으로부터 해안까지 이르는 유역 면적 $310km^2$의 천미천 유역을 대상으로 하였으며, 2001년 11월 부터 2002년 10월까지 12개월간의 강우에 따른 지하수위의 변동을 평형상태로 해석하였다. 미국 지질조사국 (USGS) 에서 개발한 3차원 유한차분 해석 프로그램인 MODFLOW 모형을 선정하여 적용한 결과를 유역 내의 12개 관측정 측정수위와 비교하였으며, 대상지역에서 14.7m의 평균 오차와 21% 정규 실효치를 나타내었다. 향후 모형 구축 및 모의 결과의 신뢰도를 향상시키기 위해 격자수와 크기의 조절 및 공간적 분포에 따른 대수층의 투수계수와 저류계수의 민감도 분석을 수행하여야 할 것으로 판단되며, 계속 연구 수행 중에 있다.

• Corrosion Science and Technology
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• v.11 no.6
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• pp.242-246
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• 2012

This measurement represents the effectiveness of sacrificial anode cathodic protection (SACP) system in a coastal bridge structure. To verify the cathodic protection (CP) effect, the monitoring sensor (DMS-100) that could measure potential, corrosion rate, current, concrete resistivity, and temperature was embedded. The measurement conducted for three years after CP system was installed. Specifically, due to the fact that fresh water and sea water was repeated in the bridge structure, this bridge structure presented special CP behavior. Measurement factors were CP potential, CP current, concrete resistivity, and depolarization potential. In addition, visual inspection was also carried out. As a result of current and depolarization measurement, CP system was well activated in most piers.

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.4 no.1
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• pp.45-58
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• 1992

A three-dimensional hydrodynamic numerical model is used to compute the annual and seasonal meteorologically-induced residual circulation on the Yellow Sea and the East China Sea continental shelf. The model is formulated having irregular coastal boundaires and non-uniform depth distribution representative of nature. The previous three-dimensional model of the East China Sea (Choi. 19U) has been further refined to resolve the flow over the continental shelf in more detail. The mesh resolution of the present finite difference grid system used is 4 minutes latitude by 5 minutes longitude over the entire shelf. The circulation pattern showing depth and spatial distribution of currents over the Yellow Sea and the East China Sea is presented. Meteorologically-induced currents are subsequently used to compute turn-over times for the three depths (surface. mid-depth. bottom) and the total water column of various regions of the Yellow Sea and the East China Sea.

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.20 no.3
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• pp.268-276
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• 2008

Potential tsunamis generated in Okinawa Trough were simulated for the investigation of the propagation characteristics in the southwestern sea of Korean Peninsula. Shallow waters in the continental shelf of East China Sea and deep waters in Okinawa Trough play an important role in the propagation characteristics of the tsunamis generated in this region. The propagation characteristics can be classified into two phases according to the stage of propagation. In the first phase, the tsunamis propagate both northeast and southwest along the deep water of the trough. In the second phase, the tsunamis enter the continental shelf of the East China Sea at right angles to topographic contour lines. Simulated results show that the tsunamis generated in the Okinawa Trough give a weak influence to the southern and western coasts of Korea due to the special topography of the southwestern sea of Korean Peninsula.

• 한국해양학회지
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• v.28 no.4
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• pp.339-346
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• 1993

Due to the natural increase of human population and the concentration of industrial complexes to coastal area, the uses of nearshore area were increased drastically, and the tendency will not stop for a while. Therefore, the loss of human life and property damages of the present days for a disaster of the same magnitude should be heavy as compared to those of the past. For the better utilization of the sea and the prevention of the frequent marine natural and man-made disaster, and for the preparedness for the ocean pollutions, through ocean researches are required. the circulation, tidal currents, storm surges, sea surface wind, waves and sea fogs of the Yellow Sea should be investigated first from the oceanographic point of view, and then the dispersion and diffusion of spilled oil and pollutants, beach erosion, red tide, and longterm sea level oscillations can be studied. International cooperation is crucial for the investigation of the sea because of the temporal and geographic scales of the oceanic phenomina.

• The Journal of Korean Institute of Communications and Information Sciences
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• v.40 no.7
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• pp.1450-1456
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• 2015

The received signal strengths according to the propagation distance between a transmitting shore station with a 53 m antenna hight and a receiving ship station with about 6m antenna hight from 700 m upto about 20 km are measured at ship's moving velocity of $5{\pm}1m/s$ using a single carrier signal at 150.0625MHz. In this paper, the path loss exponents at the propagation distance from 700 m to 20km are estimated via minimum-mean-square-error method using the measurements of the received signal strength, and the mean of the estimated path loss exponent become 3.79. The estimated propagation path loss exponents is similar to that calculated based on the field-strength values from 2 km to 20 km in Annex 2 of ITU-R P.1546-4, which is measuring results at maritime VHF at 100 MHz carrier frequency. Therefore, the estimated propagation path loss exponent shall be used as the expected path loss exponents for summer in costal area of South Sea of Korea.

• Proceedings of the Korean Institute of Information and Commucation Sciences Conference
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• v.9 no.1
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• pp.1117-1124
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• 2005

The radio field environment is very different according to frequency band, therefore communication condition is equation that VHF is passed by direct radiation and HF is via reflect radiation in ionosphere. Load a ship according to the enforcement regulations of the ships safety act have specificated the radio equipment that should be operating. This paper have analysed by the simulation program about radio field environment for research the communications condition, which is VHF & HF band in domestic coastal. We have Predicted to radio field environment and communications condition using the data of analysis and domestic radio regulation regard to coast navigational ship. Therefore have proposed the necessity for rationally plan on improvement the radio regulation and network cooperation of VHF radio station.

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.8 no.2
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• pp.137-145
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• 1996

Effects of nonlinear terms on the generation of M$_2$ tide residual elevation and M$_4$ tide in the Yellow Sea and the East China Sea are investigated using a depth-integrated two-dimensional nonlinear M$_2$tidal model. The model domain (117$^{\circ}$E-130$^{\circ}$E, 24$^{\circ}$N-41$^{\circ}$N) covers the whole region of the Yellow Sea and the East China Sea with grid resolution of 1/6$^{\circ}$ in longitude and 1/8$^{\circ}$in latitude. A radiational boundary condition is used along the open boundaries. Calculations show that advection terms yield negative residual elevation, while shallow-water terms in continuity equation yield positive residual elevation. The contribution of both advection terms and shallow-water terms to tile generation of the M$_4$ constituent is more than 90 percents, but that of quadratic bottom friction terms to the M$_4$ constituent is comparatively small.