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1.
TerraSAR-X/TanDEM-X获取高精度数字高程模型技术研究   总被引:1,自引:1,他引:0       下载免费PDF全文
以双星系统(TerraSAR-X/TanDEM-X)下的bistatic数据模式为例研究了差分干涉获取高精度DEM产品的融合算法和技术流程.针对不同观测几何条件下(升降轨,不同入射角)观测数据的畸变和缺失,提出一种迭代的顾及垂直基线、阴影和叠影的数据融合新方法重建高分辨率高精度的数字高程模型,并对TanDEM-X融合的DEM在不同地物属性特征下(山区及高楼林立的城区)的精度进行定量分析.本文采用了两对覆盖珠海、澳门区域的升降轨TerraSAR-X/TanDEM-X干涉对进行融合处理,并通过收集的高精度Lidar数据进行精度比较分析.此外,本文还定量分析了TanDEM-X的DEM对常规DInSAR技术的改进,并与SRTM、ASTER的结果进行对比.结果表明:提出的升降轨融合方法较单一轨道平台能够较好地改正或减弱由于几何畸变引起的高程信息缺失或错误,通过与Lidar数据的对比发现TanDEM-X的融合DEM在山区的精度较高,其残差的标准差为3.5 m,较单一轨道(升、降轨)分别降低8%和22%,能够通过迭代的方法获取高分辨率(可达2~5m)、高精度的地形信息;而针对城区密集建筑物的复杂地形来说,融合的DEM的精度稍低,残差的标准差为11.8m,但较单一轨道(升、降轨)来说有较大改进,其残差标准差分别降低了28%和22%;而在分布较为稀疏的居民区,融合的DEM能够较Lidar数据获取更好的建筑物高度及外形信息,此时的残差标准差可达5m.同时,TanDEM-X的融合DEM作为外部DEM能够较SRTM和ASTER来说更好地去除地形信息,尤其在山区及高程建筑密集分布的城区,从而利于后续的相位解缠和形变信息的精确获取和解译,为更高精度的时序InSAR形变监测提供有利条件.  相似文献   

2.
汶川地震后,震中地区地表形态遭到很大破坏.在该地区开展科学研究急需高精度数字高程模型支持,重建震区数字高程模型十分必要.本文以高精度重建该地区数字高程模型为目标,综合ALOS PRISM获取的三轨立体像对、ALOS PALSAR雷达影像和欧空局发布的汶川地震ENVISAT雷达影像等资料,采用光学遥感立体测图技术、InSAR技术,并融合已有全球数字高程模型,研究建立覆盖此地区15m分辨率的数字高程模型.在利用中国地壳运动监测网络和陆态网络工程项目实测的GPS数据进行高程精度分析后表明:ALOS PRISM DEM精度优于10 m(95%置信度);ALOS PALSAR DEM精度优于10 m(95%置信度),而ENVSAT ASAR DEM在平原、丘陵地区精度优于20 m(95%置信度).研究证明:ALOS PRISM能进行高精度的地形测量,ALOS PALSAR在山区仍可获得高精度数字高程模型,ENVISAT ASAR在平原地区的精度较高.因此融合光学、雷达遥感技术完全满足获取高精度、高分辨率震区数字高程模型的需要,这为在困难地区建立高精度数字高程模型提供了一个很好的途径.  相似文献   

3.
为了更好地保证从中山站到DomeA的南极内陆冰盖考察,该考察路线沿线的地形信息是必需的.虽然Radarsat南极制图计划fRAMP)能提供迄今为止最高精度的全南极数字高程模型(DEM),其最高水平分辨率为200m,但其真正的水平分辨率根据源数据的比例尺和区域覆盖密度不同而不同.对于冰架和内陆冰盖地区,水平精度约为5km.在东南极内陆冰盖地区和远离山脉地区该DEM的垂直精度估计为±50m,因此更高精度的地形数据还不存在.为了满足将来对地形信息更高精度的要求,由于ASTER光学影像具有高的空间分辨率05m),而ICESat/GLAS测高数据有较高的高程精度(13.8cm),因此本文融合ASTER立体数据和ICESat/GLAS测高数据提取了该考察路线高精度数字高程模型.首先选择一些测高数据点作为ASTER提取DEM过程中的高程控制,以减少匹配错误.由于从75°~81°S范围没有合格的ASTER立体数据覆盖,并且在该范围内ICESat轨道覆盖度大,观测数据比较密集,因此在该区域仅使用ICESat测高数据提取DEM,最后生成覆盖整条路线的DEM.分析结果表明DEM精度得到很大的提高,DEM的绝对垂直精度某些地区优于15m,除了影像009—001外,其余所有结果精度都在30m以内.其内部精度优于15m,某些情况下优于7m.生成的结果达到1:50000制图标准.结果表明在南极地区,综合利用各种遥感数据提取南极地区冰面地形信息是一种经济有效的手段.  相似文献   

4.
对于易发生地表形变的区域,传统DEM模型如SRTM,逐渐失去其时效特性,不能准确的描述地质特征,亟待更新重建.本文基于合成孔径雷达干涉测量(InSAR)采用SAR影像复数据相位信息提取地面三维信息的新技术,介绍了合成孔径雷达干涉测量数字高程模型建立的原理和方法.在此基础上,选取研究区,获取了Envisat ASAR SLC雷达影像数据,采用InSAR算法对研究区的数字高程模型进行了重建.并在研究区的形变区内外分别选取控制点,对重建DEM和SRTM进行比较分析.结果表明:对于易发生形变的特殊区域,传统DEM因失去其时效性,无法准确的描述地形特征;合成孔径雷达干涉测量可以作为此类地区DEM定期重建的有效手段.最后对重建的DEM实现三维可视化,提高了读图效率和成图质量.  相似文献   

5.
目前国内外广泛采用的坡度-等效剪切波速关系模型中,坡度主要基于30″分辨率数字高程数据的提取.DEM分辨率对坡度的提取具有重要影响,且对于不同地区、地貌单元的影响不同.本文以我国东北地区1″、3″、30″分辨率DEM为基础,分别提取研究区域内公里网格点的百分比坡度,分析不同分辨率下提取坡度差异的原因.区分平原、丘陵和山...  相似文献   

6.
张国庆  梁伟锋 《地震》2023,(1):93-104
利用EGM96全球重力场模型对ALOS AW3D30全球数字高程模型的高程系统进行转换,结合实测GNSS数据,分析ALOS AW3D30模型在青藏高原东北缘地区的精度。利用实测重力数据计算青藏高原东北缘地区的自由空气异常,并与EGIEN-6C4自由空气异常模型进行对比,分析其精度。结果表明:青藏高原东北缘地区ALOS AW3D30模型与264个GNSS测点的差异标准差为3.4 m,该地区ALOS AW3D30精度优于4 m;青藏高原东北缘地区自由空气重力异常整体呈负值,局部为正值,变化范围为-177×10-5~166×10-5 m·s-2,实测重力异常与模型结果空间分布基本一致,存在局部差异;EIGEN-6C4自由空气重力异常变化范围为-163×10-5~142×10-5 m·s-2,实测结果与模型结果差异为-119×10-5~63×10-5 m·s-2,平均值为-20×10-5<...  相似文献   

7.
利用无人机低空航测技术,对宣化盆地南缘断裂带崞村南部区段断裂带陡坎进行高分辨率数字地形影像采集与识别应用。通过结合当地地形地貌与无人机低空遥感分辨率高、实时性好、自主性强等特点,开展本次低空航测遥感技术在活动断裂带区域识别应用,结合实地野外踏勘实例对断层陡坎完成验证。结果显示,该区域断层陡坎位于宣化盆地南缘处黄土台地上,在3 km×1.5 km的遥感影像采集矩形区域内分辨率达0.8 m/pix以上。利用photoscan软件得到数字正射影像(DOM)和数字高程模型(DEM)数据,解译得到高度为数米至十余米不等断层陡坎。综合证明,应用低空航测观测技术可有效识别确定活动断层陡坎位置、量化观测陡坎等有关地形地貌现象,结合传统野外现场踏勘,能够实现构造宏观信息向精准信息追踪,完成应用低空航测技术识别断层空间位置及活动信息。  相似文献   

8.
首先分析了获取数字高程模型(DEM)的高分遥感立体测量、合成孔径雷达干涉测量技术、激光雷达测距技术和运动重建技术等技术手段,以及现阶段高空间分辨率数字高程模型(VHR DEM)提取技术的主要特点,实际应用中需根据研究区地形地貌特点选择合适的VHR DEM获取技术;然后,结合最新研究成果着重阐述了VHR DEM在活断层识别及几何结构分析、同震位移与累积位移获取和古地震研究等领域的最新应用;最后指出,VHR DEM由于其高精度、高空间分辨率的特点,正逐步改变传统活断层的研究方法,使得对活断层的研究进入到了前所未有的精细化水平.   相似文献   

9.
长白山天池火山喷发物地形地貌特征初步研究   总被引:4,自引:0,他引:4  
借助数字高程模型(简称DEM)的地形分析技术,得出了能够突出沟谷信息的长白山天池火山锥形立体地形图.利用坡度分析、高程剖面分析、三维透视等DEM技术方法,对更新世以来的长白山天池火山喷发物空间分布范围进行了地形地貌分析,并与前人已有的野外地质调查结果进行对比,总结出了研究区内喷发物的地形地貌特征,据此推测了前人未涉及地区的喷发物的窄问分布范围.这为开展长白山天池火山的大比例尺火山地质填图,特别是对于某些全新世火山喷发物范围和界限的厘定提供了遥感学依据.  相似文献   

10.
为高效获取民乐-永昌断裂西段活动构造研究的定量参数,利用ERDAS软件,基于SPOT6立体像对提取高分辨率点云数据,经过滤波和插值生成2m分辨率的数字高程模型(DEM);DEM数据线性高程精度达1m。基于DEM数据提取的高地貌面上的3条廊带剖面显示,区域存在明显的褶皱变形,后续通过高精度差分GPS实测河流阶地纵剖面进一步揭示T2阶地存在高度约2.0m的构造抬升。廊带剖面和河流阶地纵剖面显示断裂-褶皱变形整体走向为311°,与小震精定位反演拟合断层参数和震源机制解结果相近,其位置也与地震应急科考资料显示现场情况吻合。上述结果表明,民乐-永昌隐伏断裂西段民乐—大马营段存在明显的构造变形,支持该断裂为2003年民乐-山丹MS6.1和5.8级地震发震断层的认识。立体像对对于活动构造研究具有重要的作用,可为室内确定构造变形的空间位置和野外详细考察提供重要指导。  相似文献   

11.
In order to better support Antarctic inland ice sheet expedition from Zhongshan Station to Dome A, the topographic data are necessary. At present, although the entire Antarctic DEM provided by RAMP (Radarsat Antarctic Mapping Project) was estimated at the highest horizontal (spatial) resolution of about 200 m, the real horizontal resolution of the DEM varies from place to place depending on the density and scale of the original source data. For ice shelves and the inland ice sheet, the horizontal resolution is about 5 km; the vertical accuracy is estimated to be ±50 m in interior East Antarctic ice sheet and away from the mountain ranges. Therefore, more accurate topographic data are unavailable in Antarctica. In order to meet the requirements of high-accuracy topographic information for further researches, this paper mainly addresses a fusion study of ASTER stereo pairs and ICESat/GLAS altimetry data for extraction of high-accuracy DEM in East Antarctica, based on the high horizontal resolution (15 m) of ASTER and vertical accuracy (13.8 cm) of ICESat/GLAS. First, some altimetry data were selected as vertical control points to reduce errors of image correlation matching during the extraction of ASTER-based DEM. Second, ice sheet altimetry data derived from ICESat were used to generate DEM ranging from 75° to 81°S because existing ASTER data do not cover this area and high density of the coverage of ICESat altimetry data. Finally, the DEM in coverage of the expedition route was produced. The analysis of result reveals that the DEM accuracy is improved significantly. The absolute vertical accuracy of DEM is higher than 15 m in some cases and higher than 30 m for all the areas along the expedition route except from the 009-001 scene; the interior accuracy is higher than 15 m and higher than 7 m in some cases. It can meet the requirements of topographic map at 1:50000 scale, which is an economic and advantageous method to produce the topographic products. Supported by National Natural Science Foundation (Grant No. 40606002), Surveying and Mapping in Chinese Antarctic Expedition Area (Grant No. 1469990711109-1), National Key Technology R & D Program (Grant No. 2006BAD18B01), and GLA12 dataset of ICESat/GLAS in National Snow and Ice Data Center (NSIDC)  相似文献   

12.
传统的利用震后单幅合成孔径雷达(SAR)影像对建筑物的震害特征分析大多基于街区范围, 很少基于其成像几何结构. 本文基于高分辨率SAR影像上的建筑物成像几何结构, 分析了建筑物单体的震害特点, 建立了利用距离向线性灰度累加的方法提取规则未倒塌建筑物的叠掩区和阴影区及倒塌建筑物的倒塌区, 并在此基础上进行各几何特征区域的纹理特征, 如同质度、 不相似度和熵的计算及其组合特征分析, 由此建立了基于SAR影像建筑物成像几何结构的震害分析方法. 采用该方法对2010年玉树MS7.1地震震后玉树县城区的高分辨率SAR影像进行分析, 结果表明: 叠掩、 阴影和二次散射亮线是进行建筑物震害解译的有效几何结构特征, 其中叠掩区和阴影区的影像纹理特征具有较好的震害识别能力; 与传统的简单特征统计方法相比, 考虑建筑物SAR影像成像几何结构的特征统计法, 可以显著提高建筑物的震害识别能力.   相似文献   

13.
Sang‐Hyeok Kang 《水文研究》2009,23(11):1642-1649
In urban areas with a high building density, features such as roads, buildings and river dykes significantly affect flow dynamics and flood propagation. This should therefore be accounted for in the model set‐up. While 2D hydraulic models of densely urban areas are at the forefront of current research into flood inundation mechanisms, these models are constrained by inadequate parameters of topography and insufficient data. In order to solve these problems, topographic information obtained from digital elevation model (DEM) is directly programmed into the urban inundation model for a densely urban area, without exchanging the input data. In this paper, the extraction of building area is described using a tight coupling approach within a GIS environment, and its influence on the extent of flood inundation with a high building density is estimated. Copyright © 2009 John Wiley & Sons, Ltd.  相似文献   

14.
With the development of photogrammetry technology and the popularity of unmanned aerial vehicles (UAVs)technology in recent years, using UAV photogrammetry technology to rapidly acquire high precision and high resolution topographic and geomorphic data on the fault zone has gradually become an important technical means. This paper first summarizes the basic principle and workflow of a new digital photogrammetry technology, SfM (Structure from Motion), which is simple, efficient and low cost. Using this technology, we conducted aerial image acquisition and data processing for a typical fault landform on the northern of Caka Basin in Qinghai. The digital elevation model (DEM)with 6.1cm/pix resolution is generated and the density of point cloud is as high as 273 points/m2. The coverage area is 0.463km2. Further, the terrain and slope data parallel to the fault direction are extracted by topographic analysis method, and combined with the contour map and the slope diagram generated by the DEM, a fine interpretation and quantitative study of complex multilevel geomorphic surfaces is carried out. Finally, based on the results of sophisticated interpretation of geomorphology, we got the vertical displacements of the T1 terrace to the T3 terrace as (1.01±0.06)m, (1.37±0.13)m and (3.10±0.11)m, and the minimum vertical displacements of the T4 terrace and the T5 terrace as (3.77±0.14)m and (5.46±0.26)m, respectively, through the topographic profile data extracted by DEM. Such vertical displacement parameters are difficult to obtain directly by traditional remote sensing images, which shows the great application prospect of UAV photogrammetry technology in the quantitative study of active tectonics.  相似文献   

15.
The horizontal accuracy of topographic data represented by digital elevation model (DEM) resolution brings about uncertainties in landscape process modeling with raster GIS. This paper presents a study on the effect of topographic variability on cell-based empirical estimation of soil loss and sediment transport. An original DEM of 10m resolution for a case watershed was re-sampled to three realizations of higher grid sizes for a comparative examination. Equations based on the USLE are applied to the watershed to calculate soil loss from each cell and total sediment transport to streams. The study found that the calculated total soil loss from the watershed decreases with the increasing DEM resolution with a linear correlation as spatial variability is reduced by cell aggregation. The USLE topographic factors (LS) extracted from applied DEMs represent spatial variability, and determine the estimations as shown in the modeling results. The commonly used USGS 30m DEM appears to be able to reflect essential spatial variability and suitable for the empirical estimation. The appropriateness of a DEM resolution is dependent upon specific landscape characteristics, applied model and its parameterization. This work attempts to provide a general framework for the research in the DEM-based empirical modeling.  相似文献   

16.
Abstract

A digital elevation model (DEM) derived from a stereo pair of WorldView-2 (WV-2) images was assessed against ground-truth GPS point datasets. Two assessment methods were used: (a) vertical accuracy assessment and (b) hydrological assessment of surface runoff variables. Three agricultural plots with different topographic slopes were selected to perform a vertical accuracy assessment, followed by a comparative assessment of a set of hydrological variables. The results show an overall vertical accuracy of 0.45 m, confirming the potential of WV-2 stereo images to extract elevation information at high spatial resolution. Concerning plot-scale micro-topographic features, the WV-2 DEM performed better on the plot with rolling slopes (5–10%), extracting variables such as the total length and drainage area of flow paths with relative errors lower than 20%. However, some limitations were detected in the extraction of variables such as terrain slope, drainage points of flow paths and terrain depressions in areas of flatter slopes (<5%).
Editor Z.W. Kundzewicz; Associate editor D. Gerten  相似文献   

17.
本文基于不同计算窗口大小的改进局部方差方法, 判定地震后遥感影像上的目标物, 如损毁建筑物、 完好建筑物的最佳空间尺度。 对航片、 QuickBird影像进行了系列实验分析, 得到了在QuickBird影像中城区完好建筑物最佳空间分辨率在2~3 m, 损毁建筑物最佳空间分辨率2~4 m, 航片中城区完好建筑物最佳空间分辨率为3~4 m。 最佳空间分辨率与目标地物的尺度紧密相关, 不同尺度大小的地物具有不同的最优空间尺度。 最佳空间尺度的选择在处理海量高空间分辨率影像时通过重采样选取最佳空间分辨率, 可以有效减少图像运算时间, 在地震灾害快速评估中具有一定的应用意义。  相似文献   

18.
The resolution of a digital elevation model (DEM) is a crucial factor in watershed hydrologic and environmental modelling. DEM resolution can cause significant variability in the representation of surface topography, which further affects quantification of hydrologic connectivity and simulation of hydrologic processes. The objective of this study is to examine the effects of DEM resolution on (1) surface microtopographic characteristics, (2) hydrologic connectivity, and (3) the spatial and temporal variations of hydrologic processes. A puddle‐to‐puddle modelling system was utilized for surface delineation and modelling of the puddle‐to‐puddle overland flow dynamics, surface runoff, infiltration, and unsaturated flow for nine DEM resolution scenarios of a field plot surface. Comparisons of the nine modelling scenarios demonstrated that coarser DEM resolutions tended to eliminate topographic features, reduce surface depression storage, and strengthen hydrologic connectivity and surface runoff. We found that reduction in maximum depression storage and maximum ponding area was as high as 97.56% and 76.36%, respectively, as the DEM grid size increased from 2 to 80 cm. The paired t‐test and fractal analysis demonstrated the existence of a threshold DEM resolution (10 cm for the field plot), within which the DEM‐based hydrologic modelling was effective and acceptable. The effects of DEM resolution were further evaluated for a larger surface in the Prairie Pothole Region subjected to observed rainfall events. It was found that simulations based on coarser resolution DEMs (>10 m) tended to overestimate ponded areas and underestimate runoff discharge peaks. The simulated peak discharge from the Prairie Pothole Region surface reduced by approximately 50% as the DEM resolution changed from 2 to 90 m. Fractal analysis results elucidated scale dependency of hydrologic and topographic processes. In particular, scale analysis highlighted a unique constant–threshold–power relationship between DEM scale and topographic and hydrologic parameters/variables. Not only does this finding allow one to identify threshold DEM but also further develop functional relationships for scaling to achieve valid topographic characterization as well as effective and efficient hydrologic modelling. Copyright © 2016 John Wiley & Sons, Ltd.  相似文献   

19.
This study is focused on the evaluation of a Digital Elevation Model (DEM) for Tokyo, Japan from data collected by the recently launched TerraSAR add-on for Digital Elevation Measurements (TanDEM-X), satellite of the German Aerospace Center (DLR). The aim of the TanDEM-X mission is to use Interferometric SAR techniques to generate a consistent high resolution global DEM dataset. In order to generate an accurate global DEM using TanDEM-X data, it is important to evaluate the accuracy at different sites around the world. Here, we report our efforts to generate a high-resolution DEM of the Tokyo metropolitan region using TanDEM-X data. We also compare the TanDEM-X DEM with other existing DEMs for the Tokyo region. Statistical techniques were used to calculate the elevation differences between the TanDEM-X DEM and the reference data. Two high-resolution LiDAR DEMs are used as independent reference data. The vertical accuracy of the TanDEM-X DEM evaluated using the Root Mean Square Error (RMSE) is considerably higher than the existing global digital elevation models. However, the local area DEM generated by Geospatial Information Authority of Japan (GSI DEM) showed the highest accuracy among all non-LiDAR DEM’s. The vertical accuracy in terms of RMSE estimated using the 2 m LiDAR as reference is 3.20 m for TanDEM-X, 2.44 m for the GSI, 7.00 m for SRTM DEM and 10.24 m for ASTER-GDEM. We also compared the accuracy of TanDEM-X with the other DEMs for different types of land cover classes. The results show that the absolute elevation error of TanDEM-X is higher for urban and vegetated areas, likewise to those observed for other global DEM’s. This is probably because the radar signals used by TanDEM-X tend to measure the first reflective surface that is encountered, which is often the top of the buildings or canopy. Hence, the TanDEM-X based DEM is more akin to a Digital Surface Model (DSM).  相似文献   

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