4.6 Article

Spatial patterns of snow distribution in the sub-Arctic

Journal

CRYOSPHERE
Volume 16, Issue 8, Pages 3269-3293

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/tc-16-3269-2022

Keywords

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Funding

  1. Office of Biological and Environmental Research in the U.S. Department of Energy's Office of Science

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The spatial distribution of snow has a significant impact on sub-Arctic and Arctic climate, hydrology, and ecology. However, the understanding and modeling of snow distribution is limited, leading to uncertainties in snow cover representations. Through intensive field studies and modeling, the random forest model proved to be successful in capturing the complexity and variability of snow characteristics.
The spatial distribution of snow plays a vital role in sub-Arctic and Arctic climate, hydrology, and ecology due to its fundamental influence on the water balance, thermal regimes, vegetation, and carbon flux. However, the spatial distribution of snow is not well understood, and therefore, it is not well modeled, which can lead to substantial uncertainties in snow cover representations. To capture key hydroecological controls on snow spatial distribution, we carried out intensive field studies over multiple years for two small (2017-2019; similar to 2.5 km(2)) sub-Arctic study sites located on the Seward Peninsula of Alaska. Using an intensive suite of field observations (> 22 000 data points), we developed simple models of the spatial distribution of snow water equivalent (SWE) using factors such as topographic characteristics, vegetation characteristics based on greenness (normalized different vegetation index, NDVI), and a simple metric for approximating winds. The most successful model was random forest, using both study sites and all years, which was able to accurately capture the complexity and variability of snow characteristics across the sites. Approximately 86 % of the SWE distribution could be accounted for, on average, by the random forest model at the study sites. Factors that impacted year-to-year snow distribution included NDVI, elevation, and a metric to represent coarse microtopography (topographic position index, TPI), while slope, wind, and fine microtopography factors were less important. The characterization of the SWE spatial distribution patterns will be used to validate and improve snow distribution modeling in the Department of Energy's Earth system model and for improved understanding of hydrology, topography, and vegetation dynamics in the sub-Arctic and Arctic regions of the globe.

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