Abstract Evaluation of the use of very high resolution aerial imagery for accurate ice-wedge polygon mapping (Adventdalen, Svalbard)
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Evaluation of the use of very high resolution aerial imagery for accurate ice-wedge polygon mapping (Adventdalen, Svalbard)

机译:评估使用非常高分辨率的航空影像进行精确的冰楔形多边形制图(Adventdalen,斯瓦尔巴特群岛)

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AbstractThe main objective of this paper is to verify the accuracy of delineating and characterizing ice-wedge polygonal networks with features exclusively extracted from remotely sensed images of very high resolution. This kind of mapping plays a key role for quantifying ice-wedge degradation in warming permafrost. The evaluation of mapping a network is performed in this study with two sets of aerial images that are compared to ground reference data determined by fieldwork on the same network, located in Adventdalen, Svalbard (78°N). One aerial dataset is obtained from a photogrammetric survey with RGB+NIR imagery of 20cm/pixel, the other from an UAV (Unmanned Aerial Vehicle) survey that acquired RGB images of 6cm/pixel of spatial resolution. Besides evaluating the degree of matching between the delineations, the morphometric and topological features computed for the differently mapped versions of the network are also confronted, to have a more solid basis of comparison. The results obtained are similar enough to admit that remotely sensed images of very high resolution are an adequate support to provide extensive characterizations and classifications of this kind of patterned ground.Graphical abstractDisplay OmittedHighlightsMapping ice-wedge polygons from remotely sensed imagery permits monitoring large network extensions.Evaluation of the mappings requires a confrontation with ground-reference data.Validation is performed with aerial imagery and ground data in Adventdalen, Svalbard.High delineation matchings and morphometric/topological similarities indicate the adequacy of VHR imagery for mapping ice-wedge networks.
机译: 摘要 本文的主要目的是验证用从遥感影像中专门提取的特征来描绘和表征冰楔形多边形网络的准确性。高分辨率。这种映射对于量化变暖多年冻土中的冰楔退化起着关键作用。在这项研究中,使用两套航拍图像进行网络映射评估,将这两组航拍图像与同一个网络(位于斯瓦尔巴特群岛Adventdalen(78°N))的野外工作确定的地面参考数据进行比较。一个航空数据集是通过摄影测量法获得的,其中RGB + NIR图像为20cm /像素,而另一个则是通过UAV(无人机)测量获得的,其空间分辨率为6cm /像素。除了评估轮廓之间的匹配程度外,还应对为网络的不同映射版本计算的形态特征和拓扑特征,以具有更坚实的比较基础。获得的结果足够相似,以至于承认高分辨率的遥感图像足以为这种带图案的地面提供广泛的表征和分类。 < / ce:abstract> 图形摘要 省略显示 突出显示 < ce:simple-para id =“ sp0080” view =“ all”> 通过遥感图像映射冰楔多边形,可以监视大型网络扩展。 映射的评估需要与地面参考数据相抵触。 通过航空影像进行验证斯瓦尔巴特群岛Adventdalen的地面和地面数据。 高轮廓匹配和形态/拓扑相似性表明VHR图像足以映射冰楔网络。

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