• 한국측량학회지
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• 제28권1호
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• pp.169-178
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• 2010

본 논문에서는 지구표면의 99% 지역의 3차원 DEM 정보를 제공하고 있는 ASTER DEM 과 SRTM DEM의 실용가능성과 정확도를 분석하기 위해 1:5000 수치지형도에서 추출한 등고선을 통해 DEM을 생성하여 ASTER DEM과 SRTM DEM의 정확도를 평가하고자 한다. 먼저 이를 위하여 한반도 지형특성을 고려하여 명지(안양), 산악지역과 평지가 적절하게 분포하고 있는 지역(진안), 산악지역(속초)을 연구대상지역으로 선정하였다. 또한 대상지역의 1:5000 수치지형도를 통해 DEM을 생성하고 통일한 지역의 ASTER DEM과 SRTM DEM을 취득하여 상호 중첩비교가 용이하도록 수치지형도 DEM과 동일한 15m의 해상도로 변환하였다. DEM의 정확도툴 평가하기 위해 수치지형도의 등고선을 기반으로 구축된 DEM을 기준으로 ASTER DEM과 SRTM DEM의 RMSE, 상관계수, scatter plot을 이용하였다. 분석결과 수치지형도 DEM과 ASTER DEM, SRTM DEM 모두 높은 정확도를 나타내었으나, 상대적으로 SRTM DEM보다 더 넓은 범위의 자료를 제공하는 ASTER DEM이 높은 정확도를 보여 향후 다양한 분야에서의 활용이 기대된다.

• 한국관개배수논문집
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• 제14권1호
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• pp.80-88
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• 2007

The Shuttle Radar Topography Mission (SRTM) obtained elevation data on a near-global scale to generate the most complete high-resolution digital topographic database of Earth. SRTM consisted of a specially modified radar system that flew onboard the Space shuttle SRTM consisted of a specially modified radar system that flew onboard the Space Shuttle Endeavour during an 11-day mission on February 2000. Since 2004, in a GLCF (Global Land Cover Facility, http;//glcf.umiacs.umd.edu/) web-site, products of SRTM including 1Km and 90m resolutions for outside US and a 30m resolution for the US have been provided. This study is to assess the accuracy of SRTM-DEM in comparing with NGIS-DEM generated from NGIS digital topographic map(1:25,000) in Guem river watershed. For the Geum river watershed, SREM-DEM elevation ranged from 0 to 1,605m and NGIS-DEM ranged from 6 to 1,610m, and the average elevation of SRTM-DEM was 226.7m and 218.9m for NGIS-DEM, respectively. NGIS-DEM was subtracted from SRTM in three zones -Zone I (0~100m), Zone II (100~400m), Zone III (over 400m)- to estimate difference between SRTM and NGIS-DEM. As the results, the differences of these DEM were 5.2m (11.6%) in Zone I, 8.8m (3.8%) in Zone II, 12.5m (2.1%) in Zone III. Although there were differences between SRTM-DEM and NGIS-DEM, SREM-DEM would be possible to be utilized as DEM data for the region where DEM is not prepared.

• 한국측량학회지
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• 제29권2호
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• pp.193-199
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• 2011

백두산과 같은 중요 지형의 지형적 환경적 모니터링을 수행하기 위하여 SPOT-5 스테레오 위성영상을 이용하여 제작된 DEM의 정확한 보정이 필요하다. 기준 DEM으로 SRTM DEM을 사용하여 SPOT-5 DEM을 보정하였다. SPOT-5 DEM과 SRTM DEM은 단일 강체 변환식으로 변환하는 경우 오차를 많이 내포하였다. 따라서 본 연구에서는 대상지역에 골고루 기준점을 추출하고, 기준점으로부터 지역적 변환식을 추정하였다. 제안된 방법의 정확도를 평가하기 위하여, 축척기반과 S1FT기반의 변환식을 이용한 DEM과 비교하였다.

• 한국지리정보학회지
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• 제13권4호
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• pp.157-169
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• 2010

본 연구에서는 원격탐사기법으로 구축된 SRTM(The Shuttle Radar Topography Mission) DEM의 격자기반 분포형 강우-유출모형의 적용성을 분석하였다. 충주댐유역에 대하여 격자해상도 500m의 SRTM DEM과 수치지형도로부터 구축한 TOPO DEM을 구축하였고, 모형의 적용을 위하여 Stream-burning 기법으로 전처리하였다. 두 DEM으로부터 표고, 흐름방향, 수문학적 경사, 추출된 유역셀의 개수, 종단형상을 비교한 결과 SRTM DEM과 TOPO DEM이 매우 유사한 특성을 나타내는 것으로 분석되었다. 6개 강우사상을 대상으로 격자기반 분포형 강우-유출모델 KIMSTORM을 이용한 분석결과에서도 첨두유출과 유출용적의 상대오차 평균값이 각각 0.91%, 0.29%로 차이를 보이지 않았다. 분석결과로부터 SRTM DEM이 TOPO DEM과 같이 격자기반 강우-유출모형 적용시 만족할 수 있는 결과를 도출할 수 있는 지형자료임을 나타내었다.

• 한국측량학회지
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• 제28권5호
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• pp.555-560
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• 2010

백두산화산의 재 활동 여부와 관련한 연구가 최근 지구과학자들 사이에서 활발히 진행되고 있다. 그러나 우리나라는 이러한 연구에 직접적으로 참여하기 힘들고 백두산을 현장에서 지속적으로 모니터링하기 힘들다. 본 연구는 백두산 모니터링을 위한 기본 단계로써 SPOT-5 스테레오 위성영상을 이용한 백두산 DEM을 제작하고자 하였다. 제작한 DEM은 현지관측 기준점 없이 제작되었으므로 매우 부정확하다. 따라서 제작 DEM 보정을 위해, SRTM(Shuttle Radar Topography Mission) DEM을 이용한 SIFT(Scale-Invariant Feature Transform) 매칭방법을 제안하였다. 그 결과, SPOT 위성영상으로 제작한 DEM은 SRTM DEM에 비해 더욱 자세한 지형 정보를 제공할 수 있었다. 그리고 보정 전 DEM에 비해 SIFT 방법으로 보정한 DEM이 더 양호한 결과를 나타내었다.

• 한국농공학회논문집
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• 제55권6호
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• pp.101-112
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• 2013

Shuttle Radar Topography Mission Digital Elevation Model (SRTM DEM) offers opportunities to make advances in many research areas including hydrology by providing near-global scale elevation measurements at a uniform resolution. Its wide coverage and complimentary online access especially benefits researchers requiring topographic information of hard-to-access areas. However, SRTM DEM also contains inherent errors, which are subject to propagation with its manipulation into analysis outputs. Sensitivity of hydrologic analysis to the errors has not been fully understood yet. This study investigated their impact on estimation of hydrologic derivatives such as slope, stream network, and watershed boundary using Monte Carlo simulation and spatial moving average techniques. Different amount of the errors and their spatial auto-correlation structure were considered in the study. Two sub-watersheds of Geum and Deadong River areas located in South and North Korea, respectively, were selected as the study areas. The results demonstrated that the spatial presentations of stream networks and watershed boundaries and their length and area estimations could be greatly affected by the SRTM DEM errors, in particular relatively flat areas. In the Deadong River area, artifacts of the SRTM DEM created sinks even after the filling process and then closed drainage basin and short stream lines, which are not the case in the reality. These findings provided an evidence that SRTM DEM alone may not enough to accurately figure out the hydrologic feature of a watershed, suggesting need of local knowledge and complementary data.

• 한국측량학회지
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• 제36권1호
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• pp.17-24
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• 2018

DEM (Digital Elevation Model) is a useful dataset which represents the earth surface. Beside many applications, production and frequent update of DEM is a costly task. Recently global satellite based DEMs are available which has huge potential for application. To check the accuracy, this study compares two global DEMs: AW3D30 (Advanced Land Observing Satellite World 3D 30m) and SRTM30 (Shuttle Radar Topography Mission Global 30m) with reference resampled LiDAR DEM 30m in a test area around Chuncheon, Korea. The comparison analysis was based on statistics of each DEM, their difference, profiles, slope, basin and stream orders. As a result, it is found that SRTM30 and AW3D30 were much similar but inconsistent in the test area compared to the LiDAR30 DEM. In addition, SRTM30 shows less difference with LiDAR30 compared to the AW3D30 DEM. But, DEMs should be very carefully examined for area which has temporal or season changes. For basin and stream analysis, global DEMs can be used only for regional scale analysis not local large scales.

• 한국지반환경공학회 논문집
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• 제13권5호
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• pp.59-68
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• 2012

본 연구의 목적은 홍수범람해석을 위한 하천지형 구축기법을 연구하는 것이다. 청도천을 대상으로 1:5,000수치지형도와 WMS를 통해 무료로 제공되는 DEM인 ASTER과 SRTM를 이용하여 하천지형을 구축하였으며, 범람해석에는 HEC-RAS 및 HEC-GeoRSA를 적용하였다. 빈도별 기법에 따른 홍수범람해석을 모의하였으며, 1:5,000수치지형도를 기준으로 홍수심과 홍수면적을 비교하였다. 중규모 이하 자연유역을 대상으로 기법별로 구축된 하천지형은 큰 차이가 없었으며, 범람해석시 ASTER DEM을 이용한 해석결과는 침수면적의 경우 산간지역의 경우 다소 크게 산정되었다. SRTM DEM의 경우에는 타기법에 비하여 적절한 홍수 범람해석 결과가 산정되어 향후 실무에서 활용이 가능할 것으로 기대된다.

• 한국지하수토양환경학회지:지하수토양환경
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• 제22권6호
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• pp.120-128
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• 2017

The aim of this study is to analyze the accuracy of SRTM Ver 3.0 and ASTER GDEM Ver 2 over Korea. To enable this, accuracy analysis was performed by using precise DEM which was made with multiple aerial image matching and national base map benchmark. The result of this study identified both SRTM and ASTER have different features. The height of the SRTM was found to be higher (3.8 m on average) at lower elevation and lower (8.4 m on average) at higher elevation. In contrast, the ASTER was found to be lower than the actual height at both lower and higher elevation (2.92 m, 4.51 m on average). The cause of this height bias according to the elevation is due to the differences in data acquisition and processing methods of DEM. It was identified however that both SRTM and ASTER were within allowable limits of error. In addition, RMSE of the SRTM was smaller than the ASTER in comparison to benchmark, and also the bias trend both at higher and lower terrain were similar to the precise DEM which was made with multiple aerial image matching. Therefore, the reliability of SRTM can be considered to be higher.

• 대한원격탐사학회지
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• 제33권1호
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• pp.69-77
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• 2017

S The need for an automated geo-positioning approach for near real-time results and to boost cost-effectiveness has become increasingly urgent. Following this trend, a new approach to automatically compensate for the bias of the rational function model (RFM) was proposed. The core idea of this approach is to remove the bias of RFM only using tie points, which are corrected by matching with the digital elevation model (DEM) without any additional ground control points (GCPs). However, there has to be a additional evaluation according to the quality of DEM because DEM is used as a core element in this approach. To address this issue, this paper compared the quality effects of DEM in the conduct of the this approach using the Shuttle Radar Topographic Mission (SRTM) DEM with the spatial resolution of 90m. and the National Geographic Information Institute (NGII) DEM with the spatial resolution of 5m. One KOMPSAT-2 stereo-pair image acquired at Busan, Korea was used as experimental data. The accuracy was compared to 29 check points acquired by GPS surveying. After bias-compensation using the two DEMs, the Root Mean Square (RMS) errors were less than 6 m in all coordinate components. When SRTM DEM was used, the RMSE vector was about 11.2m. On the other hand, when NGII DEM was used, the RMSE vector was about 7.8 m. The experimental results showed that automated geo-positioning approach can be accomplished more effectively by using NGII DEM with higher resolution than SRTM DEM.