• Journal of Broadcast Engineering
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• v.2 no.1
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• pp.65-73
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• 1997

This paper propose a new triangular mesh approximation method using wavelet coefficients for large terrain data. Using spatio-freguency localization characteristics of wavelet coefficients, we determine the complexity of terrain data and approximate the data according to the complexity. This proposed algorithm is simple and requires low computational cost due to its top-down approach. Because of the similarity between the mesh approximation and data compression procedures based on wavelet transform, we combine the mesh approximation scheme with the Embedded Zerotree Wavelet (EZW) coding scheme for the effective management of large terrain data. Computer simulation results demonstrate that the proposed algorithm is very prospective for the 3-D visualization of terrain data.

• Spatial Information Research
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• v.19 no.2
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• pp.19-28
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• 2011

Three dimensional modeling for seafloor topography is essential to monitoring displacements in underwater structures as well as all sorts of disasters along the shore. MBES is a system that is capable of high-density water depth measurement for seafloor topography and is in broad uses for gathering 3D data and detecting displacements. MBES data, however, contain random errors that take place in the equipment offset and surveying process and require systematic researches on the correction of wrong depth measurements. Thus this study set out to propose a post-processing technique to eliminate an array of random errors taking place after equipment offset correction and basic noise correction in the MBES system and analyze its applicability to seafloor topography modeling by applying it to the subject area.

• Proceedings of the KSRS Conference
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• 2006.03a
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• pp.41-44
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• 2006

본 연구에서 3차원 지형공간정보의 구축 및 처리, 가시화를 위하여 개인용 PC와 임베디드 단말기의 포켓 PC환경에서 자료 호환 및 동시 운영이 가능한 실시간 3차원 GIS의 Prototype의 설계 및 구현과 적용 실험을 하고자 한다 OpenGL(Open Graphic Library)과 OpenGL|ES (Embedded System)를 활용하여 도시경관을 구성하는 주요객체인 지형, 건물, 교통, 식생 등을 통합적으로 저작 및 3D 객체 모델링 및 렌더링이 통합 및 개별 운영 시스템을 설계하고 구현하였다. 구현 단계에서 개인용 PC 운영환경에서는 기능성 향상에 중점을 두어 공간 데이터베이스 설계, 텍스처 영상 매핑처리, 대용량의 3차원 공간정보 처리 및 관리, 가시화, 렌더링, 모델링 기능들을 제공하며, PDA 휴대용 단말운영환경을 지원하는 모바일 시스템에서는 실시간 모바일 저작기능과 렌더링 기능에 주안점을 두어 개발하였다. 한편 연구 결과로 구현된 시스템은 원도우 XP 기반의 개인용 PC와 PDA 단말기 상에서 3D 객체 자료구조가 호환되어 향후 다양한 응용이 가능할 것으로 생각된다.

• Proceedings of the Korea Water Resources Association Conference
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• 2009.05a
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• pp.853-857
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• 2009

2차원 흐름해석 모형인 SMS(Surface-Water Modeling System)와 RAMS(River Analysis Modeling System)를 이용한 유속장 모의를 통해 Manning 조도계수와 와점성계수에 대한 민감도 분석을 수행하여 흐름특성은 Manning 조도계수에 큰 영향을 받음을 알 수 있었다. 본 연구에서는 Manning 조도계수의 변화를 통하여 실측치에 근사한 유속 분포의 모의결과를 도출하고자 현장실측을 통해 취득한 자료를 이용하여 2차원 수치모형의 모의결과와 비교하였다. 국가하천 형산강 본류 중 안강수위관측소에서 부조수위관측소 사이 약 4.3 km 의 구간을 모의구간으로 선정하였으며, $2006{\sim}2007$년에 걸쳐 취득된 현장실측자료를 바탕으로 매개변수 추정 및 모의결과와 비교하였다. 대상구간에 대한 모의결과의 정확도를 개선하기 위하여 하도의 지형특성 등을 고려하여 모의구간을 다수의 구획으로 구분한 후 수심 및 하도 평면선형을 고려한 Manning 조도계수를 차등적으로 할당하여 모의하였다. 이상의 과정을 통해 모의결과의 정확도 제고가 가능함을 관찰할 수 있었다.

• Journal of the Korean Society of Surveying, Geodesy, Photogrammetry and Cartography
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• v.27 no.3
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• pp.393-400
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• 2009

Recently demand for the 3D modeling technology to reconstruct real world is getting increasing. However, existing geospatial data are mainly based on the 2D space. In addition, most of the geospatial data provide geometric information only. In consequence, there are limits in various applications to utilize information from those data and to reconstruct the real world in 3D space. Therefore, it is required to develop efficient 3D mapping methodology and data for- mat to establish geospatial database. Especially digital elevation model(DEM) is one of the essential geospatial data, however, DEM provides only spatially distributed 3D coordinates of the natural and artificial surfaces. Moreover, most of DEMs are generated without considering terrain properties such as surface roughness, terrain type, spatial resolution, feature and so on. This paper suggests adaptive and flexible geospatial data format that has possibility to include various information such as terrain characteristics, multiple resolutions, interpolation methods, break line information, model keypoints, and other physical property. The study area was categorized into mountainous area, gently rolling area, and flat area by taking the terrain characteristics into account with respect to terrain roughness. Different resolutions and interpolation methods were applied to each area. Finally, a 3D digital map derived from aerial photographs was integrated with the geospatial data and visualized.

• Journal of the Korean Society of Surveying, Geodesy, Photogrammetry and Cartography
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• v.29 no.4
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• pp.343-349
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• 2011

Seabed topography and marine site survey should be performed first in the design and construction of marine structures. We could successfully acquire the seafloor topography information can be obtained by bathymetric survey and side scan sonar and the sediment layer thickness and 3D bedrock depth by seismic reflection. It is necessary to apply carry out the integrated interpretation to each other in the ocean civil Eng. In this paper, we have obtained information on the sea bottom topography and water depth at the same time using interferometer technique and on the basement depth by seismic reflection. We have performed to assess the proposed method on the seafloor topographic survey with bedrock.

• Economic and Environmental Geology
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• v.34 no.6
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• pp.595-600
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• 2001

Recently, interests in subsidence hazard have been increased due to the underground construction such as subway construction and managements of abandoned mines. GIS analysis of subsidence hazard has a lot of advantages in handling of spatial data and managing database. For better result of GIS analysis, there are some necessities of modifying previous subsidence theory and model. To take surface profile into account allows the application of complicated topology. Furthermore. for 3-dimensional analysis. two subsidence profile curves that are perpendicular to each other should be considered simultaneously. Through these modifications, the model for subsidence analysis using GIS can be established. With ideal case of cavities and other conditions, GIS analysis was accomplished and meaningful results were produced. More realistic properties of cavity. soil layers, groundwater condition and topology will enable GIS analysis method to produce more reliable result and to widen the area of applications.

• 한국방재학회:학술대회논문집
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• 2011.02a
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• pp.56-56
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• 2011

본 연구에서는 파랑의 변형을 예측하는 방법 중 하나인 고유함수전개법을 이용하여 축대칭 형태의 지형 위를 통과하는 파랑의 소멸파 성분을 검토하였다. 기울기와 곡률이 변하는 지역에 고유함수 전개법을 적용하여 해석할 때 필요한 적절한 구간의 수와 소멸파 성분의 개수를 산정하였다. 고유함수전개법을 이용하여 파랑의 변화를 예측하는 연구는 Bremmer(1951)가 전자기파에 적용하면서 처음 제시한 후 Takano(1960)가 파랑 변형 연구에 적용하면서 본격적으로 진행되었다. 이밖에 Kirby and Dalymple(1983), Liu et al.(1992), Cho and Lee(2000), Bender and Dean(2003), 조용식과 이창훈(1998) 및 강규영 등(2007)에 의해 국내 외로 많은 연구가 진행되었다. 그러나 기존의 연구의 대부분이 연직 2차원 지형에 대하여 수행되어 왔다. 3차원 지형에 대한 고유함수전개법은 Bender and Dean(2005)에 의해 처음으로 시작되었다. 그러나 그들의 연구에서는 수렴해를 얻기 위한 구간 및 소멸파 개수에 관한 구체적인 검토가 이루어지지 않았다는 한계가 있다. 그러나 실제 해저 지역은 다양한 지형의 영향을 받게 된다. 따라서 본 연구에서는 축대칭 지형에 대하여 수렴해를 얻기 위해 구간을 나누어 해의 수렴성을 확인하여 적절한 구간의 수를 결정한 후 소멸파의 수를 변화시키면서 소멸파가 파랑의 변형에 미치는 영향을 검토하였다. 천해역 및 중간수심 영역을 구간의 수와 소멸파 성분의 수에 변화를 주면서 수렴성 검사를 한 결과, 천해 영역에서는 소멸파 성분의 영향이 적게 나타났으나 중간수심 영역에서는 적절한 개수의 소멸파를 고려해야 보다 정확한 예측을 할 수 있음을 알 수 있었다.

• Journal of Korean Society for Geospatial Information Science
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• v.15 no.4
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• pp.3-9
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• 2007

Recently, the efforts of systematic understanding and utilization of geographic phenomenon for human life as a important factor among activity of mankind are increasing. It is necessary to express topography connected with space. Especially, the technology of geographic analysis using DEM can supply the information rapidly and accurately about elevation and terrain slope of the subject area under the necessity of high 3D quality geographic information. In this study, creating more precise DEM derived from LiDAR data, quantitative analysis on the subject area about elevation and terrain slope is done under comparison with Digital Topographic map Scale 1:1000. LiDAR data is more detailed than Digital Topographic map to express the elevation of the subject area ($39.89{\sim}77.48m$), and terrain slope by analysis using DEM derived from LiDAR data come out minutely about 90%. It can be concluded that the LiDAR data is very applicable and accurate for 3D topographic terrain slope analysis.

• Journal of the Korean Geographical Society
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• v.46 no.3
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• pp.331-350
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• 2011

Advances in computer technology enabled us to simulate the integrated effects of various geomorphic processes on landscape evolution. This review introduces a theoretical framework for 2-dimensional numerical landscape evolution models (NLEMs) which have recently been used for various research purposes. In particular much attention is paid to the approaches deployed to model major geomorphic processes on a geological time scale in previous research. NLEMs can simulate landscape evolution by numerically solving the partial differential equation which represents the relationship among the geomorphic system components (GSCs). Simple process specifications of the relationships among GSCs on a long-term time scale in terms of quantification and attempts to combine processes represent the initial research on NLEMs. Later researchers have taken these simple NLEMs and elaborated on them. Introducing the theories of NLEMs in this review is expected to help researchers trying to utilize or develop NLEMs.