The Seasonal Snow Cover Dynamics: Review on Wind-Driven Coupling Processes

The temporal evolution of seasonal snow cover and its spatial variability in environments such as mountains, prairies or polar regions is strongly influenced by the interactions between the atmospheric boundary layer and the snow cover. Wind-driven coupling processes affect both mass and energy flux...

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Main Authors: Rebecca Mott, Vincent Vionnet, Thomas Grünewald
Format: Article
Language:English
Published: Frontiers Media S.A. 2018-12-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/feart.2018.00197/full
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author Rebecca Mott
Rebecca Mott
Vincent Vionnet
Thomas Grünewald
author_facet Rebecca Mott
Rebecca Mott
Vincent Vionnet
Thomas Grünewald
author_sort Rebecca Mott
collection DOAJ
description The temporal evolution of seasonal snow cover and its spatial variability in environments such as mountains, prairies or polar regions is strongly influenced by the interactions between the atmospheric boundary layer and the snow cover. Wind-driven coupling processes affect both mass and energy fluxes at the snow surface with consequences on snow hydrology, avalanche hazard, and ecosystem development. This paper proposes a review on these processes and combines the more recent findings obtained from observations and modeling. The spatial variability of snow accumulation across multiple scales can be associated to wind-driven processes ranging from orographic precipitation at large scale to preferential-deposition of snowfall and wind-induced transport of snow on the ground at smaller scales. An overview of models of varying complexity developed to simulate these processes is proposed in this paper. Snow ablation is also affected by wind-driven processes. Over continuous snow covers, turbulent fluxes of latent and sensible heat, as well as blowing snow sublimation, modify the mass, and energy balance of the snowpack and their representation in numerical models is associated with many uncertainties. As soon as the snow cover becomes patchy in spring local heat advection induces the development of stable internal boundary layers changing heat exchange toward the snow. Overall, wind-driven processes play a key role in all the different stages of the evolution of seasonal snow. Improvements in process understanding particularly at the mountain-ridge and the slope scale, and processes representations in models at scales up to the mountain range scale, will be the basis for improved short-term forecast and climate projections in snow-covered regions.
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spelling doaj.art-2d75ecf5c3614edda8b368d43af30dd92022-12-21T22:38:20ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632018-12-01610.3389/feart.2018.00197409470The Seasonal Snow Cover Dynamics: Review on Wind-Driven Coupling ProcessesRebecca Mott0Rebecca Mott1Vincent Vionnet2Thomas Grünewald3WSL Institute for Snow and Avalanche Research SLF, Davos, SwitzerlandInstitute of Meteorology and Climate Research, Atmospheric Environmental Research (KIT/IMK-IFU), Garmisch-Partenkirchen, GermanyCentre for Hydrology, University of Saskatchewan, Saskatoon, SK, CanadaWSL Institute for Snow and Avalanche Research SLF, Davos, SwitzerlandThe temporal evolution of seasonal snow cover and its spatial variability in environments such as mountains, prairies or polar regions is strongly influenced by the interactions between the atmospheric boundary layer and the snow cover. Wind-driven coupling processes affect both mass and energy fluxes at the snow surface with consequences on snow hydrology, avalanche hazard, and ecosystem development. This paper proposes a review on these processes and combines the more recent findings obtained from observations and modeling. The spatial variability of snow accumulation across multiple scales can be associated to wind-driven processes ranging from orographic precipitation at large scale to preferential-deposition of snowfall and wind-induced transport of snow on the ground at smaller scales. An overview of models of varying complexity developed to simulate these processes is proposed in this paper. Snow ablation is also affected by wind-driven processes. Over continuous snow covers, turbulent fluxes of latent and sensible heat, as well as blowing snow sublimation, modify the mass, and energy balance of the snowpack and their representation in numerical models is associated with many uncertainties. As soon as the snow cover becomes patchy in spring local heat advection induces the development of stable internal boundary layers changing heat exchange toward the snow. Overall, wind-driven processes play a key role in all the different stages of the evolution of seasonal snow. Improvements in process understanding particularly at the mountain-ridge and the slope scale, and processes representations in models at scales up to the mountain range scale, will be the basis for improved short-term forecast and climate projections in snow-covered regions.https://www.frontiersin.org/article/10.3389/feart.2018.00197/fullseasonal snowmountainssnow-atmosphere interactionswindsnowfallsnow drift
spellingShingle Rebecca Mott
Rebecca Mott
Vincent Vionnet
Thomas Grünewald
The Seasonal Snow Cover Dynamics: Review on Wind-Driven Coupling Processes
Frontiers in Earth Science
seasonal snow
mountains
snow-atmosphere interactions
wind
snowfall
snow drift
title The Seasonal Snow Cover Dynamics: Review on Wind-Driven Coupling Processes
title_full The Seasonal Snow Cover Dynamics: Review on Wind-Driven Coupling Processes
title_fullStr The Seasonal Snow Cover Dynamics: Review on Wind-Driven Coupling Processes
title_full_unstemmed The Seasonal Snow Cover Dynamics: Review on Wind-Driven Coupling Processes
title_short The Seasonal Snow Cover Dynamics: Review on Wind-Driven Coupling Processes
title_sort seasonal snow cover dynamics review on wind driven coupling processes
topic seasonal snow
mountains
snow-atmosphere interactions
wind
snowfall
snow drift
url https://www.frontiersin.org/article/10.3389/feart.2018.00197/full
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