| DOI: | 10.5194/tc-14-2795-2020
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| 论文题名: | Warm-air entrainment and advection during alpine blowing snow events |
| 作者: | Aksamit N.O.; Pomeroy J.W.
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| 刊名: | Cryosphere
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| ISSN: | 19940416
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| 出版年: | 2020
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| 卷: | 14, 期:9 | | 起始页码: | 2795
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| 结束页码: | 2807
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| 语种: | 英语
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| 英文关键词: | advection
; air temperature
; alpine environment
; blowing snow
; complex terrain
; energy balance
; entrainment
; hydrological cycle
; snow accumulation
; snowpack
; sublimation
; updraft
; wind velocity
; Alberta
; Canada
; Rocky Mountains
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| 英文摘要: | Blowing snow transport has considerable impact on the hydrological cycle in alpine regions both through the redistribution of the seasonal snowpack and through sublimation back into the atmosphere. Alpine energy and mass balances are typically modeled with time-averaged approximations of sensible and latent heat fluxes. This oversimplifies nonstationary turbulent mixing in complex terrain and may overlook important exchange processes for hydrometeorological prediction. To determine if specific turbulent motions are responsible for warm-and dry-air advection during blowing snow events, quadrant analysis and variable interval time averaging was used to investigate turbulent time series from the Fortress Mountain Snow Laboratory alpine study site in the Canadian Rockies, Alberta, Canada, during the winter of 2015-2016. By analyzing wind velocity and sonic temperature time series with concurrent blowing snow, such turbulent motions were found to supply substantial sensible heat to near-surface wind flows. These motions were responsible for temperature fluctuations of up to 1?C, a considerable change for energy balance estimation. A simple scaling relationship was derived that related the frequency of dominant downdraft and updraft events to their duration and local variance. This allows for the first parameterization of entrained or advected energy for time-averaged representations of blowing snow sublimation and suggests that advection can strongly reduce thermodynamic feedbacks between blowing snow sublimation and the near-surface atmosphere. The downdraft and updraft scaling relationship described herein provides a significant step towards a more physically based blowing snow sublimation model with more realistic mixing of atmospheric heat. Additionally, calculations of return frequencies and event durations provide a field-measurement context for recent findings of nonstationarity impacts on sublimation rates. © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. |
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| 资源类型: | 期刊论文
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| 标识符: | http://119.78.100.158/handle/2HF3EXSE/164386
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| Appears in Collections: | 气候变化与战略
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作者单位: | Centre for Hydrology, University of Saskatchewan, Saskatoon, Canada; Institute for Mechanical Systems, Eth Zurich, Zurich, Switzerland
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| Recommended Citation: | |
Aksamit N.O.,Pomeroy J.W.. Warm-air entrainment and advection during alpine blowing snow events[J]. Cryosphere,2020-01-01,14(9)
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