migration in sea ice: from observations to modelling

Recent studies have shown that sea ice may act as a source or sink for CO2. Our recent study on O2/Ar in landfast sea ice at Barrow (Alaska) has highlighted the biogeochemical controls on the CO2 budget. However, the importance of the biogeochemical controls remains difficult to estimate due to the...

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Main Authors: Zhou, Jiayun, Moreau, Sébastien, Vancoppenolle, Martin, Conference SOLAS
Other Authors: UCL - SST/ELI/ELIC - Earth & Climate
Format: Conference Object
Language:English
Published: 2012
Subjects:
Online Access:http://hdl.handle.net/2078.1/122302
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spelling ftunivlouvain:oai:dial.uclouvain.be:boreal:122302 2024-05-12T08:01:44+00:00 migration in sea ice: from observations to modelling Zhou, Jiayun Moreau, Sébastien Vancoppenolle, Martin Conference SOLAS UCL - SST/ELI/ELIC - Earth & Climate 2012 http://hdl.handle.net/2078.1/122302 eng eng boreal:122302 http://hdl.handle.net/2078.1/122302 info:eu-repo/semantics/conferenceObject 2012 ftunivlouvain 2024-04-17T17:20:41Z Recent studies have shown that sea ice may act as a source or sink for CO2. Our recent study on O2/Ar in landfast sea ice at Barrow (Alaska) has highlighted the biogeochemical controls on the CO2 budget. However, the importance of the biogeochemical controls remains difficult to estimate due to the concomitant physical processes. Indeed, while biogeochemical processes drive gas production and consumption within the ice, physical processes regulate gas incorporation, transport and rejection. We suggest that modelling an inert gas concentration, such as argon (Ar), in sea ice may better constrain the importance of those physical processes. It would then improve our perception of the balance between physical and biogeochemical processes in the CO2 budget. In this contribution, we present how we tackle the problem of gas migration in sea ice: from observations (O2/Ar and Ar profiles) to 1-D modelling (with our first results of modelled Ar profiles). Conference Object Barrow Sea ice Alaska DIAL@UCLouvain (Université catholique de Louvain)
institution Open Polar
collection DIAL@UCLouvain (Université catholique de Louvain)
op_collection_id ftunivlouvain
language English
description Recent studies have shown that sea ice may act as a source or sink for CO2. Our recent study on O2/Ar in landfast sea ice at Barrow (Alaska) has highlighted the biogeochemical controls on the CO2 budget. However, the importance of the biogeochemical controls remains difficult to estimate due to the concomitant physical processes. Indeed, while biogeochemical processes drive gas production and consumption within the ice, physical processes regulate gas incorporation, transport and rejection. We suggest that modelling an inert gas concentration, such as argon (Ar), in sea ice may better constrain the importance of those physical processes. It would then improve our perception of the balance between physical and biogeochemical processes in the CO2 budget. In this contribution, we present how we tackle the problem of gas migration in sea ice: from observations (O2/Ar and Ar profiles) to 1-D modelling (with our first results of modelled Ar profiles).
author2 UCL - SST/ELI/ELIC - Earth & Climate
format Conference Object
author Zhou, Jiayun
Moreau, Sébastien
Vancoppenolle, Martin
Conference SOLAS
spellingShingle Zhou, Jiayun
Moreau, Sébastien
Vancoppenolle, Martin
Conference SOLAS
migration in sea ice: from observations to modelling
author_facet Zhou, Jiayun
Moreau, Sébastien
Vancoppenolle, Martin
Conference SOLAS
author_sort Zhou, Jiayun
title migration in sea ice: from observations to modelling
title_short migration in sea ice: from observations to modelling
title_full migration in sea ice: from observations to modelling
title_fullStr migration in sea ice: from observations to modelling
title_full_unstemmed migration in sea ice: from observations to modelling
title_sort migration in sea ice: from observations to modelling
publishDate 2012
url http://hdl.handle.net/2078.1/122302
genre Barrow
Sea ice
Alaska
genre_facet Barrow
Sea ice
Alaska
op_relation boreal:122302
http://hdl.handle.net/2078.1/122302
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