4.6 Article

Spatial patterns of snow distribution in the sub-Arctic

期刊

CRYOSPHERE
卷 16, 期 8, 页码 3269-3293

出版社

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

关键词

-

资金

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

向作者/读者索取更多资源

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.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.6
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据