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DOI10.5194/tc-11-2075-2017
Wind enhances differential air advection in surface snow at sub-meter scales
Drake S.A.; Selker J.S.; Higgins C.W.
发表日期2017
ISSN19940416
卷号11期号:5
英文摘要Atmospheric pressure gradients and pressure fluctuations drive within-snow air movement that enhances gas mobility through interstitial pore space. The magnitude of this enhancement in relation to snow microstructure properties cannot be well predicted with current methods. In a set of field experiments, we injected a dilute mixture of 1ĝ€% carbon monoxide (CO) and nitrogen gas (N2) of known volume into the topmost layer of a snowpack and, using a distributed array of thin film sensors, measured plume evolution as a function of wind forcing. We found enhanced dispersion in the streamwise direction and also along low-resistance pathways in the presence of wind. These results suggest that atmospheric constituents contained in snow can be anisotropically mixed depending on the wind environment and snow structure, having implications for surface snow reaction rates and interpretation of firn and ice cores. © 2017 Author(s). This work is distributed under the Creative Commons Attribution 3.0 License.
学科领域advection; array; atmospheric plume; atmospheric pressure; boundary layer; carbon monoxide; ice core; nitrogen; pressure gradient; sensor; snow cover; snowpack; wind forcing
语种英语
scopus关键词advection; array; atmospheric plume; atmospheric pressure; boundary layer; carbon monoxide; ice core; nitrogen; pressure gradient; sensor; snow cover; snowpack; wind forcing
来源期刊Cryosphere
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/119339
作者单位College of Earth, Ocean and Atmospheric Sciences, Oregon State University, Corvallis, 97333, United States; Biological and Ecological Engineering, Oregon State University, Corvallis, 97333, United States
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Drake S.A.,Selker J.S.,Higgins C.W.. Wind enhances differential air advection in surface snow at sub-meter scales[J],2017,11(5).
APA Drake S.A.,Selker J.S.,&Higgins C.W..(2017).Wind enhances differential air advection in surface snow at sub-meter scales.Cryosphere,11(5).
MLA Drake S.A.,et al."Wind enhances differential air advection in surface snow at sub-meter scales".Cryosphere 11.5(2017).
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