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Thickness estimation of supraglacial debris above ice cliff exposures using a high-resolution digital surface model derived from terrestrial photography

机译:使用陆地摄影的高分辨率数字表面模型厚度估计冰峭壁上方的冰峭敞口

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摘要

The thickness of supraglacial debris cover controls how it impacts the ablation rate of underlying glacier ice, yet this quantity remains challenging to measure, particularly at glacier scales. We present a relatively straightforward, and cost-effective method to estimate debris thickness exposed above ice cliffs using simplified geometrical measurements from a high-resolution digital surface model (DSM), derived from a terrestrial photographic survey and a Structure from Motion with Multi-View Stereo workflow (SfM-MVS). As the ice surface relief beneath the debris cover is unknown, we assume it to be horizontal and provide error bounds based on characteristic ice-surface slope at the visible debris/ice interface. Debris thickness around the three sampled ice cliffs was highly variable (interquartile range of 0.80-2.85 m) and negatively skewed with a mean thickness of 2.08 +/- 0.68 m. Manual, and high-frequency radar, determinations of debris thickness in the same area show similar thickness distributions, but statistically different mean debris thickness, due to local heterogeneity. Debris thickness values derived in this study all exceed estimates from satellite surface temperature inversions. Wider application of the method presented here would provide useful data for improving debris thickness approximations from satellite imagery.
机译:Supraglacial碎片覆盖的厚度控制它如何影响底层冰川冰的消融率,但该数量仍然挑战测量,特别是在冰川鳞片上。我们介绍了一种相对简单,并且具有成本效益的方法,以利用来自地面摄影调查的高分辨率数字表面模型(DSM)的简化几何测量来估计冰悬崖上方暴露的碎片厚度,从陆地摄影调查和来自多视图的运动的结构立体声工作流(SFM-MVS)。随着碎屑盖下方的冰表面浮雕未知,我们假设它是水平的,并根据可见碎片/冰界面的特征冰表面斜率提供错误界限。三个取样冰悬崖周围的碎片厚度高度变化(120-2.85米的四分位数范围),并且平均厚度为2.08 +/- 0.68米。手动和高频雷达,相同区域中的碎片厚度的测定显示出类似的厚度分布,而是由于局部异质性而统计学上的平均碎片厚度。本研究中得出的碎屑厚度值均超过卫星表面温度逆的估计。这里呈现的方法的更广泛的应用将提供用于改善卫星图像的碎屑厚度近似的有用数据。

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