• 한국해양공학회지
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• 제20권3호
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• pp.61-66
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• 2006

The estuary has a very complex coastline and bottom topography. Before the close of floodgate, the Keum river estuary was deposited with sediment from the Keum river, created bythe construction of the Keum river estuary dike. So, a periodical dredging is necessary to assure water depth for boat entry and departure to Kunsan port. Theof this study is to find the change of tidal current of M2tide and the topography before and after construction at the Geum River estuary dike. The change of water depth is investigated by digitizing the sea map (No.305) of Kunsan port, which was edited by National Oceanographic Research Institute. The calculated co-range and co-tidal charts of M2tide before the dike construction are similar to the observed ones. Therefore, the amplitude and phase after construction at Geum River estuary dike increases compared to before construction at Geum River estuary dike. The scour occurred in the A-A' section.

• 한국해양공학회:학술대회논문집
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• 한국해양공학회 2004년도 학술대회지
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• pp.137-142
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• 2004

There has been considerable controversy over the change of coastal topography and shoreline by coastal erosion in Gohyun Bay, Geojedo. In this study, we analyzed aerial photographs and surveyed coastal topography and shoreline. Changes between years were identified using a GIS overlay analysis and field surveys with DGPS, Total Station and Echo Sounder. As a result, we were able to identify changes by coastal erosion in the area of Gohyun Bay, Geojedo.

• 한국측량학회지
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• 제33권6호
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• pp.497-506
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• 2015

Gravity variations due to the 2011 Tohoku (M9.0) earthquake, which occurred at the plate boundaries near the northeastern coast of Japan, were estimated through the GRACE spherical harmonic (Stokes) coefficients derived from the CSR. About -5 μGal gravity variation by the GRACE data was found in the back-arc basin area with respect to a reference gravity model. The mean gravity variations in the back-arc basin area and the Japan Trench area were -4.4 and -3.2 μGal in order. The small negative gravity variations around the Japan Trench area can be interpreted by both crustal dilatation and the seafloor topography change in comparison with the large negative gravity variations in the back-arc basin area by co-seismic crustal dilatation of the landward plate. From the results of the gravity variations, vertical displacements generated from relatively short wavelength caused by the earthquake were estimated by use of multi-beam bathymetric measurements obtained from JAMSTEC. The maximum seafloor topography changes of about ±50 m were found at west side of the Japan Trench axis by the earthquake. The seafloor topography change by the megathrust earthquake can be considered as the results of the landslide of the seafloor throughout the landward side.

• 한국한의학연구원논문집
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• 제1권1호
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• pp.273-287
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• 1995

Moire topography, a simple technique for three-dimensional quantitation, was used to provide interference fringe photographs of the human back with sufficient accuracy to be used for detecting patient with asymmetry due to scoliosis, the disease of cervix and lumbar, muscle dysfunction. Contour lines are a suitable and widely accepted method of describing a three-dimensional surface. In the moire technique, contour lines of an object are produced as interference fringes while the object is illuminated by a spotlight through a special grating. The fringe pattern is produced by the interference of the grating and its shadow on the object. A photograph of a moire pattern on the human back will permit an assessment of the overall body shape and the symmetry of the back. This study uses shadow moire topography. Moire topography provides a non-invasive technique for quantifying the shape of the human body. In the use of moire topography for the Oriental Medicine Diagnosis, the strength of moire lies in the ablility to detect change due to deformity of human body.

• 한국콘텐츠학회논문지
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• 제7권3호
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• pp.168-175
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• 2007

기상이변으로 매년 발생하는 홍수는 산사태를 유발한다. 그리고 지진으로 인해 발생하는 지형의 변화는 기존의 수치지도로 지형분석이 불가능하게 된다. 본 논문은 지형의 변화가 발생하였을 경우 신속하게 항공사진을 수치화 한 후 수치표고모형을 생성하고 그 활용방안에 관한 연구를 수행하였다. 항공사진을 수치화 하여 수집된 입체영상으로 수치표고모형의 생성이 가능하였으며 생성된 수치표고모형의 표준편차는 0.864m로 다소 높게 나타났으나 실제 지형을 반영하고 있는 것으로 나타났다. 연구결과 지형변화가 발생했을 경우 항공사진으로 수치표고모형의 생성이 가능할 것으로 보인다.

• 한국안광학회지
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• 제8권1호
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• pp.11-15
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• 2003

이 연구의 목적은 근시와 정시에서 근거리 작업의 결과로서 각막 지도의 변화를 조사한 것이다. 18세에서 24세 사이의 30명의 대학생을 무작위로 선택하였다. 그들은 각각 15명씩의 두 굴절 그룹으로 분류하였다. 즉 근시와 정시로 하였다. 각 피검자의 각박 지도는 Eye-Sys Videokeratography system으로 측정하였다. 측정은 근거리 작업의 30분 전후에 수행하였다(복사한 N10 교체를 20cm 근거리에서 수행함). 자극 받은 케라토 미터와 반경선 케라토미터 지도 프로그램은 자료의 분석에 사용하였다. 우리의 결과들은 단지 정시를 위한 근거리 작업 후 각막 지도의 중심 부위(3 mm)의 가장 연명한 경선에서 유의성 변화(P<0.005)의 발견을 제외하고는 근시와 정시 모두에 근거리 작업의 결과로서 자극된 케라토 미터와 반경선 나타남은 유의성을 가지는 변화는 없는 것으로 나타났다. 우리는 각막 지도는 근시와 정시 모두에서 근거리 작업의 결과로서 의미 있는 변화가 없다는 것을 결론지었다.

• 보존과학회지
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• 제38권4호
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• pp.347-359
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• 2022

Gongsanseong Fortress was registered of a World Heritage Site in 2015 as a representative cultural heritage from the Woongjin Baekje period, and it has been used throughout the entire period from Baekje Kingdom to the Joseon Dynasty. Within Gongsanseong Fortress, the area around Ssangsujeong is presumed the site of royal palace of the Woongjin Baekje. Also, the excavated culture layers of the Baekje Kingdom, the Unified Silla period, and the Joseon Dynasty were confirmed. In this study, paleotopography was modeled by digitally converting the elevation data obtained through surveying the excavation process, and the use of the topography in the Ssangsujeong area was considered by examining the variations in the topography according to the periods. As a result, the topography of the slope around the peak changed by periods, and the topography did not change on the flat land. The topography between the Baekje Kingdom and the Unified Silla period appeared to be almost identical, and it seems that the space of the Baekje period was maintained as it is. Also, during the Joseon Dynasty, it is confirmed that flat surfaces in the previous period were used. However, sediments on the slopes flowed down, reducing the area of the flatland, and architectural techniques that could utilize the natural topography of the changed slope were applied to interpret it as having a different topography from the previous period. In order to model and interpret the paleotopography, excavation data, geological and topographic analysis, and digital data must be secured. It is expected that location conditions and ancient human life can be identified if the analysis technique in the study is applied to other archaeological sites in the future.

• 한국측량학회지
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• 제20권3호
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• pp.303-311
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• 2002

최근에 GIS 기법을 이용하여 수문 분석에 필요한 지형 매개변수를 분석하는 연구가 활발히 진행되고 있는 실정이다. 지형 분석에 이용되는 DEM은 수치 지형도의 등고선 자료를 이용하여 효과적으로 구축될 수 있다. 따라서 DEM의 응용성이 여러 분야에서 점차 증가되고 있는 실정이다. 본 연구에서는 지형 매개변수 추출시 DEM 격자크기가 경사와 배수 유역에 어떤 영향을 주는지를 분석하고자 20m∼100m 격자 크기의 DEM이 평창강과 주방천 유역에 적용되었다. 본 연구에서는 DEM 격자크기에 따른 경사변화에 대한 회귀 방정식을 도출하였다. 그 결과 DEM 격자크기가 증가함에 따라 경사가 줄어들며, 배수 유역면적은 거의 변화하지 않는다는 것을 알 수 있었다.

• 한국광학회지
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• 제9권1호
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• pp.9-14
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• 1998

그림자식 무아레 무늬의 절대차수를 결정할 수 있는 새로운 방법으로 카메라와 광원의 위치좌표는 변화시키지 않고 사방격자의 피치 간격을 일정한 비율로 변화시키는 방법과, 사방격자의 피치간격은 변화시키지 않고 광원과 카메라 사이의 평면위치좌표를 변화시켜서 주기적인 무아레 무늬를 얻었다. 그 결과 사방격자에 의한 큰 주기의 무아레 무늬와 직선격자에 의한 작은 주기의 무아레 무늬를 비교함으로써 직선격자에 의한 무아레 무늬의 절대차수를 결정할 수 있음을 확인하였다.

• 한국해안해양공학회:학술대회논문집
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• 한국해안해양공학회 1997년도 정기학술강연회 발표논문 초록집 Annual Meeting of Korean Society of Coastal and Ocean Engineers
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• pp.39-44
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• 1997

As wind waves generated in deep water approach nearshore zone, they experience various physical phenomena caused by bathymetric variations, nonlinear interactions among different wave components and interferences with man-made coastal structures. Among these, the bathymetric variations may play a significant role in the change of wave climate. The accurate calculation of reflection and transmission coefficients of incident waves over a bottom topography is indispensible for the proper and economical design of coastal structures. (omitted)