Snow accumulation, albedo and melt patterns following road construction on permafrost, Inuvik–Tuktoyaktuk Highway, Canada

J. Hammar, I. Grünberg, S. Kokelj, Jurjen van der Sluijs, J. Boike
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Abstract

Abstract. Roads constructed on permafrost can have a significant impact on the surrounding environment, potentially inducing permafrost degradation. These impacts arise from factors such as snow accumulation near the road, which affects the soil's thermal and hydrological regime, and road dust that decreases the snow's albedo, altering the timing of snowmelt. However, our current understanding of the magnitude and the spatial extent of these effects is limited. In this study we addressed this gap by using remote sensing techniques to assess the spatial effect of the Inuvik to Tuktoyaktuk Highway (ITH) in Northwest Territories, Canada, on snow accumulation, snow albedo and snowmelt patterns. With a new, high resolution snow depth raster from airborne laser scanning, we quantified the snow accumulation at road segments in the Trail Valley Creek area using digital elevation model differencing. We found increased snow accumulation up to 36 m from the road center. The magnitude of this snow accumulation was influenced by the prevailing wind direction and the embankment height. Furthermore, by analyzing 43 Sentinel-2 satellite images between February and May 2020, we observed reduced snow albedo values within 500 m of the road, resulting in a 12-days-earlier onset of snowmelt within 100 m from the road. We examined snowmelt patterns before, during and after the road construction using the normalized difference snow index from Landsat-7 and Landsat-8 imagery. Our analysis revealed that the road affected the snowmelt pattern up to 600 m from the road, even in areas which appeared undisturbed. In summary, our study improves our understanding of the spatial impact of gravel roads on permafrost due to enhanced snow accumulation, reduced snow albedo and earlier snowmelt. Our study underscores the important contribution that remote sensing can provide to improve our understanding of the effects of infrastructure development on permafrost environments.
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加拿大伊努维克-图克托亚克图克公路冻土层上修路后的积雪、反照率和融化模式
摘要在冻土层上修建道路会对周围环境产生重大影响,可能导致冻土层退化。造成这些影响的因素包括:道路附近的积雪会影响土壤的热量和水文系统;道路扬尘会降低积雪的反照率,从而改变融雪时间。然而,我们目前对这些影响的程度和空间范围的了解还很有限。在这项研究中,我们利用遥感技术评估了加拿大西北地区伊努维克至图克托亚克图克高速公路(ITH)对积雪、雪反照率和融雪模式的空间影响,从而弥补了这一空白。利用机载激光扫描获得的新的高分辨率积雪深度栅格,我们使用数字高程模型差分法量化了特雷尔谷溪地区各路段的积雪量。我们发现,距离道路中心 36 米以内的积雪有所增加。积雪量的大小受盛行风向和路堤高度的影响。此外,通过分析 2020 年 2 月至 5 月期间的 43 幅哨兵-2 卫星图像,我们观察到道路 500 米范围内的积雪反照率值降低,导致道路 100 米范围内的融雪开始时间提前了 12 天。我们利用 Landsat-7 和 Landsat-8 图像中的归一化差异积雪指数研究了道路建设之前、期间和之后的融雪模式。我们的分析表明,道路对距离道路 600 米以内的融雪模式产生了影响,即使在看似未受干扰的区域也是如此。总之,我们的研究加深了我们对砾石路因积雪增加、雪反照率降低和融雪提前而对永久冻土产生的空间影响的理解。我们的研究强调了遥感技术在提高我们对基础设施建设对永久冻土环境影响的认识方面所能做出的重要贡献。
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