从密度计算干雪介电常数:一个重要的回顾

F. Di Paolo, B. Cosciotti, S. Lauro, E. Mattei, E. Pettinelli
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引用次数: 8

摘要

探地雷达(GPR)对高山积雪的调查能够快速评估积雪厚度,但需要测量积雪中的波速。这种量通常通过密度测量来评估,使用文献中存在的雪介电常数和密度之间的关系。不幸的是,这些方程提供了不同的结果,并且很少有与不确定性相关的报道,这使得在不同模型之间进行选择非常困难。在目前的工作中,我们比较了所有不确定的方程(当报告时),建议哪个模型在从雪密度测量中提取波速时可以被认为是最可靠的。实验数据的分析也证实了这种选择。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Dry snow permittivity evaluation from density: A critical review
Ground Penetrating Radar (GPR) surveys on alpine snow enable a rapid evaluation of snow thickness but necessitate a measurement of the wave velocity in the snowpack. Such quantity is often evaluated from density measurements, using the relationships connecting snow permittivity and density present in literature. Unfortunately such equations provide different results and are rarely reported with an associated uncertainty, making the choice between different models pretty difficult. In the present work we compare all the equations with uncertainties (when reported), suggesting which model can be considered as the most reliable in the extraction of the wave velocity from snow density measurements. Such choice has also been corroborated by the analysis of experimental data.
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