globalchange  > 气候变化事实与影响
DOI: 10.5194/hess-21-1137-2017
Scopus记录号: 2-s2.0-85013998173
论文题名:
Developing a representative snow-monitoring network in a forested mountain watershed
作者: Gleason K; E; , Nolin A; W; , Roth T; R
刊名: Hydrology and Earth System Sciences
ISSN: 10275606
出版年: 2017
卷: 21, 期:2
起始页码: 1137
结束页码: 1147
语种: 英语
Scopus关键词: Ablation ; Binary trees ; Classification (of information) ; Forestry ; Landforms ; Satellite ground stations ; Watersheds ; Forested watersheds ; Ground-based stations ; Landscape characteristic ; Monitoring locations ; Physically based modeling ; Snow water equivalent ; Snowpack accumulation ; Statistical modeling ; Snow ; ablation ; ground-based measurement ; monitoring system ; montane forest ; mountain region ; peak flow ; regression analysis ; snow accumulation ; snowpack ; spatial variation ; watershed ; Cascade Range ; McKenzie River ; Oregon ; United States
英文摘要: A challenge in establishing new ground-based stations for monitoring snowpack accumulation and ablation is to locate the sites in areas that represent the key processes affecting snow accumulation and ablation. This is especially challenging in forested montane watersheds where the combined effects of terrain, climate, and land cover affect seasonal snowpack. We present a coupled modeling approach used to objectively identify representative snow-monitoring locations in a forested watershed in the western Oregon Cascades mountain range. We used a binary regression tree (BRT) non-parametric statistical model to classify peak snow water equivalent (SWE) based on physiographic landscape characteristics in an average snow year, an above-average snow year, and a below-average snow year. Training data for the BRT classification were derived using spatially distributed estimates of SWE from a validated physically based model of snow evolution. The optimal BRT model showed that elevation and land cover type were the most significant drivers of spatial variability in peak SWE across the watershed (R2 Combining double low line 0.93, p value < 0.01). Geospatial elevation and land cover data were used to map the BRT-derived snow classes across the watershed. Specific snow-monitoring sites were selected randomly within the dominant BRT-derived snow classes to capture the range of spatial variability in snowpack conditions in the McKenzie River basin. The Forest Elevational Snow Transect (ForEST) is a result of this coupled modeling approach and represents combinations of forested and open land cover types at low, mid-, and high elevations. After 5 years of snowpack monitoring, the ForEST network provides a valuable and detailed dataset of snow accumulation, snow ablation, and snowpack energy balance in forested and open sites from the rain–snow transition zone to the upper seasonal snow zone in the western Oregon Cascades. © 2017 Author(s).
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/79245
Appears in Collections:气候变化事实与影响

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作者单位: College of Earth Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR, United States

Recommended Citation:
Gleason K,E,, Nolin A,et al. Developing a representative snow-monitoring network in a forested mountain watershed[J]. Hydrology and Earth System Sciences,2017-01-01,21(2)
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