Study of snow-atmosphere interactions over an Antarctic surface using large eddy simulations coupled with a Lagrangian stochastic model

The need for a better understanding of fluid and morphodynamic processes over Antarctic sea ice motivates the development of detailed models of small-scale snow-atmosphere interactions. At large scales, these interactions drive spatial patterns of snow distribution and snow transport from the margin...

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Main Authors: Comola, Francesco, Giometto, Marco Giovanni, Trujillo Gomez, Ernesto, Leonard, Katherine Colby, Maksym, Ted, Parlange, Marc, Lehning, Michael
Format: Text
Language:unknown
Published: 2016
Subjects:
Online Access:http://infoscience.epfl.ch/record/215698
id ftinfoscience:oai:infoscience.tind.io:215698
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spelling ftinfoscience:oai:infoscience.tind.io:215698 2023-05-15T13:38:50+02:00 Study of snow-atmosphere interactions over an Antarctic surface using large eddy simulations coupled with a Lagrangian stochastic model Comola, Francesco Giometto, Marco Giovanni Trujillo Gomez, Ernesto Leonard, Katherine Colby Maksym, Ted Parlange, Marc Lehning, Michael 2016-02-01T10:42:26Z http://infoscience.epfl.ch/record/215698 unknown http://infoscience.epfl.ch/record/215698 http://infoscience.epfl.ch/record/215698 Text 2016 ftinfoscience 2023-02-13T22:32:01Z The need for a better understanding of fluid and morphodynamic processes over Antarctic sea ice motivates the development of detailed models of small-scale snow-atmosphere interactions. At large scales, these interactions drive spatial patterns of snow distribution and snow transport from the marginal ice to the sea. However, challenges arise when representing the detailed sequence of processes involved, such as aerodynamic entrainment, particle dynamics, feedback on fluid momentum and particle impacts. We use a Lagrangian stochastic model coupled to large eddy simulations to represent particle trajectories in turbulent flows. An immersed boundary method is used to represent the underlying surface and a dynamic surface roughness model is used to account for the drag induced by the subgrid-scale roughness. The model is set up for an Antarctic sea ice floe over which pre- and post-storm snow distributions were measured using a terrestrial laser scanner. The dataset, collected as part of the Sea Ice Physics and Ecosystem Experiment 2, indicates marked changes in the snow distribution as a result of snow drift, providing valuable testing grounds for the model. Model results are in agreement with blowing snow concentrations at different heights and with the observed patterns of erosion and deposition. Text Antarc* Antarctic Sea ice EPFL Infoscience (Ecole Polytechnique Fédérale Lausanne) Antarctic
institution Open Polar
collection EPFL Infoscience (Ecole Polytechnique Fédérale Lausanne)
op_collection_id ftinfoscience
language unknown
description The need for a better understanding of fluid and morphodynamic processes over Antarctic sea ice motivates the development of detailed models of small-scale snow-atmosphere interactions. At large scales, these interactions drive spatial patterns of snow distribution and snow transport from the marginal ice to the sea. However, challenges arise when representing the detailed sequence of processes involved, such as aerodynamic entrainment, particle dynamics, feedback on fluid momentum and particle impacts. We use a Lagrangian stochastic model coupled to large eddy simulations to represent particle trajectories in turbulent flows. An immersed boundary method is used to represent the underlying surface and a dynamic surface roughness model is used to account for the drag induced by the subgrid-scale roughness. The model is set up for an Antarctic sea ice floe over which pre- and post-storm snow distributions were measured using a terrestrial laser scanner. The dataset, collected as part of the Sea Ice Physics and Ecosystem Experiment 2, indicates marked changes in the snow distribution as a result of snow drift, providing valuable testing grounds for the model. Model results are in agreement with blowing snow concentrations at different heights and with the observed patterns of erosion and deposition.
format Text
author Comola, Francesco
Giometto, Marco Giovanni
Trujillo Gomez, Ernesto
Leonard, Katherine Colby
Maksym, Ted
Parlange, Marc
Lehning, Michael
spellingShingle Comola, Francesco
Giometto, Marco Giovanni
Trujillo Gomez, Ernesto
Leonard, Katherine Colby
Maksym, Ted
Parlange, Marc
Lehning, Michael
Study of snow-atmosphere interactions over an Antarctic surface using large eddy simulations coupled with a Lagrangian stochastic model
author_facet Comola, Francesco
Giometto, Marco Giovanni
Trujillo Gomez, Ernesto
Leonard, Katherine Colby
Maksym, Ted
Parlange, Marc
Lehning, Michael
author_sort Comola, Francesco
title Study of snow-atmosphere interactions over an Antarctic surface using large eddy simulations coupled with a Lagrangian stochastic model
title_short Study of snow-atmosphere interactions over an Antarctic surface using large eddy simulations coupled with a Lagrangian stochastic model
title_full Study of snow-atmosphere interactions over an Antarctic surface using large eddy simulations coupled with a Lagrangian stochastic model
title_fullStr Study of snow-atmosphere interactions over an Antarctic surface using large eddy simulations coupled with a Lagrangian stochastic model
title_full_unstemmed Study of snow-atmosphere interactions over an Antarctic surface using large eddy simulations coupled with a Lagrangian stochastic model
title_sort study of snow-atmosphere interactions over an antarctic surface using large eddy simulations coupled with a lagrangian stochastic model
publishDate 2016
url http://infoscience.epfl.ch/record/215698
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Sea ice
genre_facet Antarc*
Antarctic
Sea ice
op_source http://infoscience.epfl.ch/record/215698
op_relation http://infoscience.epfl.ch/record/215698
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