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DOI | 10.5194/tc-13-3045-2019 |
Effect of snow microstructure variability on Ku-band radar snow water equivalent retrievals | |
Rutter N.; J. Sandells M.; Derksen C.; King J.; Toose P.; Wake L.; Watts T.; Essery R.; Roy A.; Royer A.; Marsh P.; Larsen C.; Sturm M. | |
发表日期 | 2019 |
ISSN | 19940416 |
EISSN | 13 |
起始页码 | 3045 |
结束页码 | 3059 |
卷号 | 13期号:11 |
英文摘要 | Spatial variability in snowpack properties negatively impacts our capacity to make direct measurements of snow water equivalent (SWE) using satellites. A comprehensive data set of snow microstructure (94 profiles at 36 sites) and snow layer thickness (9000 vertical profiles across nine trenches) collected over two winters at Trail Valley Creek, NWT, Canada, was applied in synthetic radiative transfer experiments. This allowed for robust assessment of the impact of estimation accuracy of unknown snow microstructural characteristics on the viability of SWE retrievals. Depth hoar layer thickness varied over the shortest horizontal distances, controlled by subnivean vegetation and topography, while variability in total snowpack thickness approximated that of wind slab layers. Mean horizontal correlation lengths of layer thickness were less than a metre for all layers. Depth hoar was consistently ~ 30 % of total depth, and with increasing total depth the proportion of wind slab increased at the expense of the decreasing surface snow layer. Distinct differences were evident between distributions of layer properties; a single median value represented density and specific surface area (SSA) of each layer well. Spatial variability in microstructure of depth hoar layers dominated SWE retrieval errors. A depth hoar SSA estimate of around 7 % under the median value was needed to accurately retrieve SWE. In shallow snowpacks < 0:6 m, depth hoar SSA estimates of ±5 %-10 % around the optimal retrieval SSA allowed SWE retrievals within a tolerance of ±30 mm. Where snowpacks were deeper than ~ 30 cm, accurate values of representative SSA for depth hoar became critical as retrieval errors were exceeded if the median depth hoar SSA was applied. © 2019 Copernicus GmbH. All rights reserved. |
学科领域 | radar; snow cover; snow water equivalent; snowpack; spatial variation; Canada; Valley Creek [Pennsylvania] |
语种 | 英语 |
scopus关键词 | radar; snow cover; snow water equivalent; snowpack; spatial variation; Canada; Valley Creek [Pennsylvania] |
来源期刊 | The Cryosphere
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/118808 |
作者单位 | Department of Geography and Environmental Sciences, Northumbria University, Newcastle upon Tyne, United Kingdom; CORES Science and Engineering Limited, Burnopfield, United Kingdom; Climate Research Division, Environment and Climate Change Canada, Toronto, Canada; School of GeoSciences, University of Edinburgh, Edinburgh, United Kingdom; Département des Sciences de l'Environment, Université du Québec À Trois-Rivières, Canada; Département de Géomatique Appliquée, Université de Sherbrooke, Canada; Department of Geography, Wilfrid Laurier University, Canada; Geophysical Institute, University of Alaska, Fairbanks, United States |
推荐引用方式 GB/T 7714 | Rutter N.,J. Sandells M.,Derksen C.,et al. Effect of snow microstructure variability on Ku-band radar snow water equivalent retrievals[J],2019,13(11). |
APA | Rutter N..,J. Sandells M..,Derksen C..,King J..,Toose P..,...&Sturm M..(2019).Effect of snow microstructure variability on Ku-band radar snow water equivalent retrievals.The Cryosphere,13(11). |
MLA | Rutter N.,et al."Effect of snow microstructure variability on Ku-band radar snow water equivalent retrievals".The Cryosphere 13.11(2019). |
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