首页> 外文期刊>ISPRS Journal of Photogrammetry and Remote Sensing >Sequential digital elevation models of active lava flows from ground-based stereo time-lapse imagery
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Sequential digital elevation models of active lava flows from ground-based stereo time-lapse imagery

机译:来自地面立体时移图像的活跃熔岩流的顺序数字高程模型

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We describe a framework for deriving sequences of digital elevation models (DEMs) for the analysis of active lava flows using oblique stereo-pair time-lapse imagery. A photo-based technique was favoured over laser-based alternatives due to low equipment cost, high portability and capability for network expansion, with images of advancing flows captured by digital SLR cameras over durations of up to several hours. However, under typical field scale scenarios, relative camera orientations cannot be rigidly maintained (e.g. through the use of a stereo bar), preventing the use of standard stereo time-lapse processing software. Thus, we trial semi-automated DEM-sequence workflows capable of handling the small camera motions, variable image quality and restricted photogrammetric control that result from the practicalities of data collection at remote and hazardous sites. The image processing workflows implemented either link separate close-range photogrammetry and traditional stereo-matching software, or are integrated in a single software package based on structure-from-motion (SfM). We apply these techniques in contrasting case studies from Kilauea volcano, Hawaii and Mount Etna, Sicily, which differ in scale, duration and image texture. On Kilauea, the advance direction of thin fluid lava lobes was difficult to forecast, preventing good distribution of control. Consequently, volume changes calculated through the different workflows differed by ~10% for DEMs (over ~30m~2) that were captured once a minute for 37 min. On Mt. Etna, more predictable advance (~3 m h~(-1) for ~3 h) of a thicker, more viscous lava allowed robust control to be deployed and volumetric change results were generally within 5% (over ~500 m~2). Overall, the integrated SfM software was more straightforward to use and, under favourable conditions, produced results comparable to those from the close-range photogrammetry pipeline. However, under conditions with limited options for photogrammetric control, error in SfM-based surfaces may be difficult to detect.
机译:我们描述了一个框架,用于导出数字高程模型(DEM)的序列,以使用倾斜立体对延时图像对活动熔岩流进行分析。基于照片的技术比基于激光的替代品更受青睐,因为它具有较低的设备成本,较高的便携性和网络扩展能力,并且数码单反相机可以在长达数小时的时间内捕获先进的流量图像。但是,在典型的场标场景下,不能严格保持相对的摄像机方向(例如,通过使用立体声条),从而阻止了使用标准的立体声延时处理软件。因此,我们试用了半自动化的DEM序列工作流程,该工作流程能够处理由于偏远和危险场所的数据收集实用性而导致的小摄像机运动,可变图像质量和严格的摄影测量控制。实施的图像处理工作流要么链接单独的近距离摄影测量法和传统的立体匹配软件,要么被集成到基于动感结构(SfM)的单个软件包中。我们将这些技术与来自夏威夷基拉韦厄火山和西西里岛埃特纳火山的案例研究进行了对比,这些案例在规模,持续时间和图像纹理上都不同。在基拉韦厄,很难预测稀薄的熔岩裂片的前进方向,这妨碍了控制的良好分布。因此,对于在37分钟内每分钟捕获一次的DEM(约30m〜2以上),通过不同的工作流程计算出的体积变化相差约10%。在山上埃特纳火山,较厚的,粘性更大的熔岩的更可预测的推进(〜3 m h〜(-1,〜3 h),可以进行稳健的控制,体积变化结果通常在5%之内(〜500 m〜2以上)。总体而言,集成的SfM软件更易于使用,并且在有利的条件下所产生的结果可与近距离摄影测量管线的结果相媲美。但是,在摄影测量控制选项有限的情况下,基于SfM的表面中的错误可能很难检测到。

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