In situ effective snow grain size mapping using a compact hyperspectral imager
In situ effective snow grain size mapping using a compact hyperspectral imager
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DOI:
10.1017/jog.2020.68
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发表时间:
2021-02-01
影响因子:
3.4
通讯作者:
Hammonds, Kevin
中科院分区:
文献类型:
--
作者:
Donahue, Christopher;Skiles, S. McKenzie;Hammonds, Kevin
Effective snow grain radius (r(e)) is mapped at high resolution using near-infrared hyperspectral imaging (NIR-HSI). The NIR-HSI method can be used to quantify r(e) spatial variability, change in r(e) due to metamorphism, and visualize water percolation in the snowpack. Results are presented for three different laboratory-prepared snow samples (homogeneous, ice lens, fine grains over coarse grains), the sidewalls of which were imaged before and after melt induced by a solar lamp. The spectral reflectance in each similar to 3 mm pixel was inverted for r(e) using the scaled band area of the ice absorption feature centered at 1030 nm, producing r(e) maps consisting of 54 740 pixels. All snow samples exhibited grain coarsening post-melt as the result of wet snow metamorphism, which is quantified by the change in r(e) distributions from pre- and post-melt images. The NIR-HSI method was compared to r(e) retrievals from a field spectrometer and X-ray computed microtomography (micro-CT), resulting in the spectrometer having the same mean r(e) and micro-CT having 23.9% higher mean r(e) than the hyperspectral imager. As compact hyperspectral imagers become more widely available, this method may be a valuable tool for assessing r(e) spatial variability and snow metamorphism in field and laboratory settings.