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Spatiotemporal Variability of Arctic Soil Moisture Detected from High-Resolution RADARSAT-2 SAR Data

机译:利用高分辨率RADARSAT-2 SAR数据检测的北极土壤水分的时空变化

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摘要

Various methods are used to determine soil moisture information from synthetic aperture radar (SAR) data, but none specific to High Arctic regions and their unique physical characteristics. This research presents a method for determining, at high spatial and temporal resolutions, surface soil moisture and its changes through time in the Canadian High Arctic. An artificial neural network (ANN) is implemented using input variables derived from RADARSAT-2 SAR data and previously modelled surface roughness information. The model is applied to SAR data collected at various incidence angles and acquisition dates across two study sites on Melville Island, Nunavut. The model results in absolute soil moisture errors of approximately 15% (r2 = 0.46) for the primary study sites and 12% (r2 = 0.26) for the verification study area. The ANN model is accurate for modelling (i) the spatial distribution of soil moisture and (ii) the changes in moisture through time across the study areas, two characteristics that are very important for inputs to hydrologic or climate models. In addition, the models appear to be scalable when applied at coarser spatial resolutions, showing potential for large-area mapping or modelling.
机译:可以使用多种方法从合成孔径雷达(SAR)数据确定土壤湿度信息,但没有一种方法专门针对高北极地区及其独特的物理特性。这项研究提出了一种在高时空分辨率下确定加拿大高北极地区表层土壤水分及其随时间变化的方法。人工神经网络(ANN)使用从RADARSAT-2 SAR数据和先前建模的表面粗糙度信息得出的输入变量来实现。该模型应用于在努纳武特州梅尔维尔岛的两个研究地点以不同入射角和采集日期收集的SAR数据。该模型导致主要研究地点的绝对土壤湿度误差约为15%(r2 = 0.46),而对于验证研究区域则为12%(r2 = 0.26)。 ANN模型对于以下方面是准确的:(i)研究区域内土壤水分的空间分布和(ii)水分随时间的变化,这两个特征对于输入水文或气候模型非常重要。此外,在较粗糙的空间分辨率下应用时,这些模型似乎具有可伸缩性,显示了大面积映射或建模的潜力。

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