Performance of MAR (v3.11) in simulating the drifting-snow climate and surface mass balance of Adélie Land, East Antarctica

Drifting snow, or the wind-driven transport of snow particles originating from clouds and the surface below and above 2 m above ground and their concurrent sublimation, is a poorly documented process on the Antarctic ice sheet, which is inherently lacking in most climate models. Since drifting snow...

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Published in:Geoscientific Model Development
Main Authors: Amory, Charles, Kittel, Christoph, Toumelin, Louis, Agosta, Cécile, Delhasse, Alison, Favier, Vincent, Fettweis, Xavier
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/gmd-14-3487-2021
https://gmd.copernicus.org/articles/14/3487/2021/
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spelling ftcopernicus:oai:publications.copernicus.org:gmd90795 2023-05-15T14:02:17+02:00 Performance of MAR (v3.11) in simulating the drifting-snow climate and surface mass balance of Adélie Land, East Antarctica Amory, Charles Kittel, Christoph Toumelin, Louis Agosta, Cécile Delhasse, Alison Favier, Vincent Fettweis, Xavier 2021-06-09 application/pdf https://doi.org/10.5194/gmd-14-3487-2021 https://gmd.copernicus.org/articles/14/3487/2021/ eng eng doi:10.5194/gmd-14-3487-2021 https://gmd.copernicus.org/articles/14/3487/2021/ eISSN: 1991-9603 Text 2021 ftcopernicus https://doi.org/10.5194/gmd-14-3487-2021 2021-06-14T16:22:13Z Drifting snow, or the wind-driven transport of snow particles originating from clouds and the surface below and above 2 m above ground and their concurrent sublimation, is a poorly documented process on the Antarctic ice sheet, which is inherently lacking in most climate models. Since drifting snow mostly results from erosion of surface particles, a comprehensive evaluation of this process in climate models requires a concurrent assessment of simulated drifting-snow transport and the surface mass balance (SMB). In this paper a new version of the drifting-snow scheme currently embedded in the regional climate model MAR (v3.11) is extensively described. Several important modifications relative to previous version have been implemented and include notably a parameterization for drifting-snow compaction of the uppermost snowpack layer, differentiated snow density at deposition between precipitation and drifting snow, and a rewrite of the threshold friction velocity above which snow erosion initiates. Model results at high resolution (10 km) over Adélie Land, East Antarctica, for the period 2004–2018 are presented and evaluated against available near-surface meteorological observations at half-hourly resolution and annual SMB estimates. The evaluation demonstrates that MAR resolves the local drifting-snow frequency and transport up to the scale of the drifting-snow event and captures the resulting observed climate and SMB variability, suggesting that this model version can be used for continent-wide applications. Text Antarc* Antarctic Antarctica East Antarctica Ice Sheet Copernicus Publications: E-Journals Antarctic East Antarctica The Antarctic Geoscientific Model Development 14 6 3487 3510
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Drifting snow, or the wind-driven transport of snow particles originating from clouds and the surface below and above 2 m above ground and their concurrent sublimation, is a poorly documented process on the Antarctic ice sheet, which is inherently lacking in most climate models. Since drifting snow mostly results from erosion of surface particles, a comprehensive evaluation of this process in climate models requires a concurrent assessment of simulated drifting-snow transport and the surface mass balance (SMB). In this paper a new version of the drifting-snow scheme currently embedded in the regional climate model MAR (v3.11) is extensively described. Several important modifications relative to previous version have been implemented and include notably a parameterization for drifting-snow compaction of the uppermost snowpack layer, differentiated snow density at deposition between precipitation and drifting snow, and a rewrite of the threshold friction velocity above which snow erosion initiates. Model results at high resolution (10 km) over Adélie Land, East Antarctica, for the period 2004–2018 are presented and evaluated against available near-surface meteorological observations at half-hourly resolution and annual SMB estimates. The evaluation demonstrates that MAR resolves the local drifting-snow frequency and transport up to the scale of the drifting-snow event and captures the resulting observed climate and SMB variability, suggesting that this model version can be used for continent-wide applications.
format Text
author Amory, Charles
Kittel, Christoph
Toumelin, Louis
Agosta, Cécile
Delhasse, Alison
Favier, Vincent
Fettweis, Xavier
spellingShingle Amory, Charles
Kittel, Christoph
Toumelin, Louis
Agosta, Cécile
Delhasse, Alison
Favier, Vincent
Fettweis, Xavier
Performance of MAR (v3.11) in simulating the drifting-snow climate and surface mass balance of Adélie Land, East Antarctica
author_facet Amory, Charles
Kittel, Christoph
Toumelin, Louis
Agosta, Cécile
Delhasse, Alison
Favier, Vincent
Fettweis, Xavier
author_sort Amory, Charles
title Performance of MAR (v3.11) in simulating the drifting-snow climate and surface mass balance of Adélie Land, East Antarctica
title_short Performance of MAR (v3.11) in simulating the drifting-snow climate and surface mass balance of Adélie Land, East Antarctica
title_full Performance of MAR (v3.11) in simulating the drifting-snow climate and surface mass balance of Adélie Land, East Antarctica
title_fullStr Performance of MAR (v3.11) in simulating the drifting-snow climate and surface mass balance of Adélie Land, East Antarctica
title_full_unstemmed Performance of MAR (v3.11) in simulating the drifting-snow climate and surface mass balance of Adélie Land, East Antarctica
title_sort performance of mar (v3.11) in simulating the drifting-snow climate and surface mass balance of adélie land, east antarctica
publishDate 2021
url https://doi.org/10.5194/gmd-14-3487-2021
https://gmd.copernicus.org/articles/14/3487/2021/
geographic Antarctic
East Antarctica
The Antarctic
geographic_facet Antarctic
East Antarctica
The Antarctic
genre Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
op_source eISSN: 1991-9603
op_relation doi:10.5194/gmd-14-3487-2021
https://gmd.copernicus.org/articles/14/3487/2021/
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container_title Geoscientific Model Development
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