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P-Band Radar Retrieval of Permafrost Active Layer Properties: Time-Series Approach and Validation with In-Situ Observations

机译:多年冻土活动层特性的P波段雷达反演:时间序列方法和现场观测验证

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In this paper, a permafrost active layer retrieval algorithm using time-series P-band SAR observations is presented wherein both layer dielectric constants (representing unfrozen water content) and layer thicknesses (representing water table or thaw depths) of the active layer are retrieved. The time-series observations were acquired after the maximum thaw, so that variables such as active layer thickness (ALT) can be assumed constant as they are nearly time-invariant between the data acquisitions. Having these time-invariant variables can reduce the number of unknowns and improve the retrieval accuracy with limited number of observations. Comparison of the retrieval results with in-situ observations suggests that the retrieved ALT values are generally underestimated.
机译:在本文中,提出了使用时间序列P带SAR观测的多年冻土活动层检索算法,其中检索了活动层的层介电常数(代表未冻结的水含量)和层厚度(代表水位或融化深度)。时间序列观测值是在最大解冻后获取的,因此可以将诸如活动层厚度(ALT)之类的变量假定为常量,因为它们在数据获取之间几乎是时间不变的。具有这些时不变的变量可以减少未知数的数量,并在有限数量的观测值的情况下提高检索精度。将检索结果与原位观察结果进行比较表明,检索到的ALT值通常被低估了。

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