• Proceedings of the Korea Water Resources Association Conference
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• 2008.05a
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• pp.367-372
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• 2008

본 연구는 감조하천에서 조위의 영향을 크게 받는 저 평수위의 수위-유량관계곡선식 개발의 한계를 극복하기 위해 조위의 영향을 고려한 다변수 복합 수위-유량관계곡선식을 개발하였다. 곡선식 개발은 수위-수면차-수위차-유량의 관계를 통해 지수형 곡선식을 개발하였다. 여기서 수면차는 조위와 수위와의 차이며, 이때 조석파의 전파시간에 대한 지체시간을 고려하였다. 수위차는 대상 수위관측소의 전 시간과의 수위차이다. 또한 조위에 의해 발생되는 역유량 자료를 이용한 지수형 곡선식을 개발하고자 유량 조정변수를 추가하였다. 개발된 수위-유량관계곡선식을 한강대교에 적용하여 자동유량측정시설에서 측정된 유량자료와 비교 검토한 결과 경향성에서 일치하였으며, (-)유량의 산정도 가능하였다. 분석기간내의 총 유출량 검토 결과 8.3%의 오차를 보여 본 과업에서 제시된 복합 수위-유량관계곡선식의 적정성을 파악할 수 있었다.

• The Bulletin of The Korean Astronomical Society
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• v.34 no.2
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• pp.41.2-41.2
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• 2009

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2003.11a
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• pp.119-120
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• 2003

1990년대 이후 오존이 매년 증가하여 오존주의보 발령횟수도 증가하고 있으며 이로 인하여 시민의 건강과 건축물, 동식물에 대한 피해가 구체적으로 환산된 적은 없지만 대단히 많은 영향을 줄 것이다. 이에 따라 오존의 생성과 관련 있는 전구물질(precursor)에 대한 관측에 대한 기술개발이 급속히 이루어지고 있다. VOCs는 그 종류와 발생원이 복잡ㆍ다양할 뿐만 아니라 시료의 채집과 분석방법에 여러 가지 기술적인 어려움이 있으나, 최근에 VOCs 연구에 대한 국제적인 추세는 환경대기 중에 존재하는 극미량(NMHC)의 개념에서 더 나아가 개별적인 VOC물질에 대한 관리와 연구가 권장되는 상황이다. (중략)

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.7 no.3
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• pp.241-247
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• 1995

A time mean surface velocity field was estimated from AVHRR/SST in the Korea Strait. Time duration of SST data set was not different from tidal period and tidal elimination was investigated. The velocity field was estimated by inverse method and compared with results of ADCP observation and results of Odamaki(1989). In accordance with results. tidal component was eliminated partially in case that there were a little difference between total time interval of 557 data set and tidal period.

• Proceedings of the Korea Water Resources Association Conference
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• 1996.05a
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• pp.689-694
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• 1996

The purpose of this study is to find sedimentation patterns variation in Seamangum coastal sea region. Water circulations are calculated diagnostically from the observed water temperature and salinity data and wind data and tidal residual current. There dimensional movements of injected particles due to currents, tubulence and sinking velocity are tracked by the Euler-lagrange method. Calculated sedimentation patters of riverine material are highly similat to the observed ones.

• Proceedings of the Korean Society of Surveying, Geodesy, Photogrammetry, and Cartography Conference
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• 2003.04a
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• pp.45-54
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• 2003

This paper deal with the GPS performance for determining the ocean tidal loading components(M$_2$, N$_2$, S$_2$, K$_2$) and the availability of permanent GPS stations(CHJU, KANR) established in Korea. We determined the ocean tidal loading components from GPS observation by spectrum analysis and compared to that from global ocean tidal models(GOT00.2, FES99, CRS4.0, NAO99). Through this study, we have a sense that amplitude and phase lags of ocean tidal loading components from observed GPS data was almost equal to value calculated in ocean tide models. The diurnal ocean tide loading constituents are not considered, because unmodeled troposhere effects increase the noise level near the diurnal frequency band and prevent us from obtaining significant results.

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.16 no.1
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• pp.47-55
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• 2004

A SS prediction system using GUI in coastal region has been developed to predict the dispersion of the suspended sediments occurred by dredging. The prediction system uses a finite element hydrodynamic model to calculate water level and velocities and a random-walk particle tracking model to simulate SS dispersion. The system was applied to hindcast the tidal currents and SS concentrations in the Kunsan coastal waters. The simulated tidal currents showed good agreements with the observed currents. The transport model was verified for analytic solutions and field observation showing good agreements.

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.8 no.2
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• pp.204-214
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• 1996

The purpose of this study is to find a variation in traveling patterns of soil and soil diffusion due to construction of the sea dike in Saemangum coastal sea region. Water circulations are calculated diagnostically from the observed water temperature, salinity and wind data, and tidal residual current. Three-dimensional movements of injected particles due to currents, turbulence and sinking velocity are tracked by the Euler-Lagrangian method. Calculated a variation in traveling patterns of soil and soil diffusion due to construction of the sea dike deposited mostly from estuarine area of the Geum River to Gokunsan coastal sea region. This results are believed to be the combined effect of coastal circulation.

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.6 no.4
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• pp.335-339
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• 1994

The Tartar Strait currents of different scales are analysed using results of observations and modeling. The paper focuses on tidal phenomena and general circulation features. It is shown that the areas of maximal tidal currents are located in the regions of stable boundary streams. The stability of the streams under different meteorological conditions and energy concentration in the small areas may be explained by non-linear effects of tide over rough bottom topography.

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.27 no.4
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• pp.228-237
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• 2015

Field observations were conducted to collect hydrodynamic and morphological data, which are needed to account for mechanisms of bathymetry changes caused by physical forcings, in Haeundae beach. In order to quantitatively describe characteristics of wave transformations and current patterns in space in winter and summer, in-situ sensors for measuring waves and current profiles were installed at three locations in the cross-shore direction and also three locations in the along-shore direction. As for the results of wave measurements, waves with main direction from the east dominate in winter while waves are incident from the S and the ESE in summer. Analysis of current data reveals that currents over the study domain are considerably influenced by a pattern of tidal motions, thereby, mainly oscillating in the direction of tidal currents, i.e., east-west directions, in both winter and summer. Currents tend to be influenced by local bathymetry in the shallow water region, with the direction changed along the depth contours and the magnitude reduced as they approach the shoreline. The results analysed from the hydrodynamic data through this study can be further combined with the morphological and bathymetry data, leading to the quantification of seasonal sediment transport rates and sand budget changes.