• Journal of the Korean Society of Surveying, Geodesy, Photogrammetry and Cartography
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• v.12 no.1
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• pp.43-52
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• 1994

This paper outlines a new approach to the line generalization when preparing small scale map on the basis of existing large scale digital map. Line generalizations are conducted based on Douglas algorithm using 1/25,000 scale topographic maps of southeastern JEJU island which produced by National Geographic Institute to analyze the fitness to the original and problems of graphical representation. Compare to the same scale map which was generated by manual method, a verity of small, but sometimes significant errors ＆ modification of topological relationship have been detected. The research gives full details of three algorithms that operationalize the smallest visible object method, together with some empirical results. A comparison of the results produced by the new algorithms with those produced by manual generalization and Douglas method of data reduction is provided. Also this paper presents the preliminary results of an relationships between the size of smallest visual object and requiring data storages for each algorithms.

• Korean Journal of Agricultural and Forest Meteorology
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• v.11 no.1
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• pp.13-18
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• 2009

Accurate solar radiation data are critical to evaluate major physiological responses of plants. For most upland crops and orchard plants growing in complex terrain, however, it is not easy for farmers or agronomists to access solar irradiance data. Here we suggest a simple method using a sun-slope geometry based topographical coefficient to estimate daily solar irradiance on any sloping surfaces from global solar radiation measured at a nearby weather station. An hourly solar irradiance ratio ($W_i$) between sloping and horizontal surface is defined as multiplication of the relative solar intensity($k_i$) and the slope irradiance ratio($r_i$) at an hourly interval. The $k_i$ is the ratio of hourly solar radiation to the 24 hour cumulative radiation on a horizontal surface under clear sky conditions. The $r_i$ is the ratio of clear sky radiation on a given slope to that on a horizontal reference. Daily coefficient for slope correction is simply the sum of $W_i$ on each date. We calculated daily solar irradiance at 8 side slope locations circumventing a cone-shaped parasitic volcano(c.a., 570m diameter for the bottom circle and 90m bottom-to-top height) by multiplying these coefficients to the global solar radiation measured horizontally. Comparison with the measured slope irradiance from April 2007 to March 2008 resulted in the root mean square error(RMSE) of $1.61MJ\;m^{-2}$ for the whole period but the RMSE for April to October(i.e., major cropping season in Korea) was much lower and satisfied the 5% error tolerance for radiation measurement. The RMSE was smallest in October regardless of slope aspect, and the aspect dependent variation of RMSE was greatest in November. Annual variation in RMSE was greatest on north and south facing slopes, followed by southwest, southeast, and northwest slopes in decreasing order. Once the coefficients are prepared, global solar radiation data from nearby stations can be easily converted to the solar irradiance map at landscape scales with the operational reliability in cropping season.

• 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.

• Proceedings of the Korea Water Resources Association Conference
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• 2021.06a
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• pp.174-174
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• 2021

지표면에서 소규모의 요철로 이루어진 미세지형 (Micro Topography)은 자연 지형의 일반적인 특징이다. 지표면에서의 흐름해석 시 이러한 미세지형에 의한 효과를 정확히 고려하기 위해서는 고해상도의 지형격자를 사용하여야 하나, 대부분의 지표유출모델은 미세지형이 존재하지 않는 저해상도의 거친 표면으로 간주함으로써 바닥 마찰 효과를 증가시켜 미세지형에 의한 영향을 대략적으로만 반영한다. 본 연구에서는 보다 정확한 강우-유출 및 유사-유출 해석을 목적으로 고해상도의 지형격자를 사용하여 미세지형을 포함한 건조 및 반건조 지대에서의 흐름을 수치적으로 모의하였다. 미세지형의 형태는 마루와 골 사이가 직선으로 이루어진 파동의 형태로 이상화 하였으며, 파동의 진폭과 파장을 조절하여 다양한 형태의 미세지형을 고려하였다. 수치모형은 흐름의 움직임에 대한 Saint-Venant 방정식과 침식 및 유사이송에 대한 Hairsine-Rose 방정식을 함께 계산하는 통합모형인 tRIBS-FEaST를 사용하였다. 수치 모의 결과에서 나타난 미세지형의 핵심 영향은 최대 유량 및 유사량 도달시간의 지연, 유사 입자 크기별 유사-유출량 증감, 그리고 하천 유출(stream flow)의 생성이었다. 또한, 미세지형의 형태에 따라 미세지형과 강우-유출 및 유사-유출 사이에 비례 혹은 반비례 관계가 성립함을 보였다. 수치 모의 결과를 종합적으로 검토하여 미세지형이 강우-유출과 유사-유출에 미치는 영향에 대해 논의하였으며, 기존 Manning 거칠기 계수를 통한 해석 방법의 적부를 판단하였다.

• Spatial Information Research
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• v.19 no.1
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• pp.13-19
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• 2011

As an urbanization is in progress, the change of the planimetric features and topography including high-rise residential buildings commonly occur. The change of the planimetric features and topography causes occurrence of the strong wind and wind speed increase or decrease due to the effect of planimetric features and topography on the windward side even though the wind blows with the same speed. In the design standard, this change by wind speed is defined as the velocity pressure exposure coefficient, the value of coefficient is estimated and reflected by ground surface roughness, but in a reality, ground surface roughness is determined in accordance with the subjective judgement of designer and then the velocity pressure exposure coefficient is estimated, moreover the research and data for classification of ground surface roughness are insufficient. In this paper, we will estimate the velocity pressure exposure coefficient by the quantified method for classifying ground surface roughness by using GIS according to the height of a building targeting area where high-rise residential buildings are built lately. When the structure subjected to wind load is designed, reasonability of design and safety of structure will be more improved by using the estimation method of velocity pressure exposure coefficient presented in this study.

• Journal of Korean Society for Geospatial Information Science
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• v.18 no.4
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• pp.79-86
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• 2010

This research is a thing about reverse operation about the solar power for location decision and increasing efficiency of the solar power generation equipments. The purpose of this research is reverse operation about the amount of sunshine using the climate and spatial elements. Following the result of correlation analysis, the wind-speed and cloud-amount factor are excluded, because the correlation and significance coefficients are out of value. Each outcome of regression analysis using the other four climate elements, and regression analysis using spatial elements is what the amount of sunshine and the solar altitude are the most influence to the insolation-modeling. Doing the regression analysis based on the precedent result make the result that climate elements have bigger coefficient of regression than spatial elements. This outcome means the climate elements are more influence than spatial elements.

• Proceedings of the Korea Water Resources Association Conference
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• 2011.05a
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• pp.415-415
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• 2011

수문학 또는 하천유출은 크게 기후학적은 인자 (온도, 바람, 상대습도 등)나 지형학적 인자 (지표면 경사, 흙의 종류, 하천의 면적, 하천의 길이 등)들에 의해 결정된다. 지형학적 인자들 중인 하천의 면적 그리고 주하천의 길이에 의한 영향은 비첨두홍수량의 과 수문곡선의 모양에 크게 관여되어 있다. 일반적으로 유역형상이 좁고 주하천의 길이(유로연장)가 긴 하천의 경우 단위면적당 유출량과 시간과의 그래프에서 수문곡선은 넓고 낮은 형태 모습을 지니지만 유역의 형상이 넓고 주하천의 길이기 짧은 하천은 수문곡선이 좁고 높은 형태의 모습을 가진다. 이러한 유역형상의 차이에 따라 Horton (1932)은 유역의 면적과 주하천의 길이의 비로 형상계수 (Shape Factor)의 공식을 제시하였다. 유역면적에 비해 유로연장이 길면 형상계수가 작아지고 첨두홍수량이 작아지는 반면 유역면적에 비해 유로연장이 짧을수록 형상계수가 커져 첨두홍수량이 커지는 형상을 발견할 수 있다. 형상계수와 비첨두홍수량의 상관관계를 알아보기 위하여 상수 전용댐 안전성 대책 및 치수능력 증대 방안연구 (2008) 보고서에서 적용한 유역들을 비교하였다. 이 보고서에 있는 38개의 유역들 중에서 형상계수가 0< <1 인 유역들을 선택한 후 형상계수와 지속시간별 비첨두홍수량의 관계 그리고 유역면적과 지속시간별 비첨두홍수량의 관계를 도시하였다. 추세선에 의한 결정계수인 $R^2$ 의 값을 비교하여 형상계수와 비첨두홍수량과의 관계를 조명하였다. 또한, 형상계수에 따른 순간단위도의 첨두시간 및 첨두유량을 비교하기 위하여 유역면적이 $300m^2$내외이며, 서로 다른 형상계수를 갖는 유역을 선정하여 연구를 진행하였다. 대상유역의 관측값을 이용하여 Nash모형을 적용한 순간단위도를 산정하였으며, 형상계수에 따른 첨두시간 및 첨두유량의 비교분석을 수행하였다.

• Journal of the Korean earth science society
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• v.34 no.1
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• pp.69-80
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• 2013

Terrain data is one of important basic data in various areas of Earth science. Recently, finer DEM data is available, which necessary to develop a method that deals with such huge data efficiently. This study was conducted on the lossless compression of DEM data and efficient partial reconstruction of terrain information from compressed data. In this study, we compressed the wavelet coefficients of DEM, obtained from integer wavelet transform (IWT) by entropy encoding. CDF (Cohen-Daubechies-Feauveau) 3.5 wavelet showed the best compression ratio of about 45.4% and the optimum decomposition level was 3. Results also showed that a small region of terrain could be restored from the inverse wavelet transform with a part of the wavelet coefficients that are related to such region instead of whole reconstruction. We discussed the potential applications of the terrain data compression for precise gravity terrain correction.

• Journal of Korea Game Society
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• v.14 no.4
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• pp.45-52
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• 2014

We cannot load the entire data for high-resolution terrain model to the GPU memory since its size is too big. Out-of-core approaches are commonly used to solve the problem. However, due to limited bandwidth of the secondary storage, it is difficult to render the terrain in real-time. A method that compresses the DEM data with wavelet transform on GPU, and renders the decoded data is suggested. However, it is inefficient since it has to sample the values from textures, convert them to vertices, and generate a mesh periodically. We propose a method to store the approximation coefficients of wavelet compression as vertex attributes and render the terrain by decoding the data on geometric shader. It can reduce the amount of transferring terrain texture since approximation coefficients are given as an attribute of the vertex. Also, it generate meshes without additional upload of terrain texture.

• Proceedings of the Korean Society of Surveying, Geodesy, Photogrammetry, and Cartography Conference
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• 2002.10a
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• pp.195-199
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• 2002

SAR(Synthetic Aperture Radar) 영상은 경사촬영을 수행하므로 지형의 기복에 따른 영향을 많이 받는다. 따라서 SAR영상을 이용하여 여러 가지 정보들을 추출하여 이용하기 위해서는 전처리 과정으로서 지형의 기복에 따른 여러 가지 왜곡들을 보정해야 한다. 이에 본 연구에서는 RADARSAT SAR 영상을 이용하여 궤도모델링, 정사보정을 수행하고 역산란계수, 국부입사각 계산 등을 통해 지형기복에 따른 방사왜곡보정을 수행하였다.