Sea ice and argon

1) Atmospheric argon on Earth and Mars cycles on a seasonal basis and abiotic factors will be particularly important drivers of this noble gas. 2) It is predicted and confirmed that there is similarity in the seasonality of sea ice and argon, with atmospheric argon in a Hemisphere often increasing...

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Main Author: Hambler, C
Format: Working paper
Language:English
Published: Research Square 2022
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author Hambler, C
author_facet Hambler, C
author_sort Hambler, C
collection OXFORD
description 1) Atmospheric argon on Earth and Mars cycles on a seasonal basis and abiotic factors will be particularly important drivers of this noble gas. 2) It is predicted and confirmed that there is similarity in the seasonality of sea ice and argon, with atmospheric argon in a Hemisphere often increasing fastest when sea ice in that Hemisphere is declining fastest. 3) There is some visual similarity between the detailed phenology of Greenland Sea ice extent and argon in some Northern Hemisphere sites, but formal analysis is required. 4) If causal, the mechanism is unclear but could involve argon bubble formation during freezing and bubble release in the spring melt. 5) Other variables with very similar phenology to sea ice, including high-latitude sea temperatures, should be investigated as potential drivers. 6) Cycling of argon by sea ice would strengthen the argument that seasonal cycling of carbon dioxide is in part driven abiotically.
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spelling oxford-uuid:91b6ffc8-3fa0-4f9c-89f3-216331056f182022-11-10T15:21:23ZSea ice and argonWorking paperhttp://purl.org/coar/resource_type/c_8042uuid:91b6ffc8-3fa0-4f9c-89f3-216331056f18EnglishSymplectic ElementsResearch Square2022Hambler, C1) Atmospheric argon on Earth and Mars cycles on a seasonal basis and abiotic factors will be particularly important drivers of this noble gas. 2) It is predicted and confirmed that there is similarity in the seasonality of sea ice and argon, with atmospheric argon in a Hemisphere often increasing fastest when sea ice in that Hemisphere is declining fastest. 3) There is some visual similarity between the detailed phenology of Greenland Sea ice extent and argon in some Northern Hemisphere sites, but formal analysis is required. 4) If causal, the mechanism is unclear but could involve argon bubble formation during freezing and bubble release in the spring melt. 5) Other variables with very similar phenology to sea ice, including high-latitude sea temperatures, should be investigated as potential drivers. 6) Cycling of argon by sea ice would strengthen the argument that seasonal cycling of carbon dioxide is in part driven abiotically.
spellingShingle Hambler, C
Sea ice and argon
title Sea ice and argon
title_full Sea ice and argon
title_fullStr Sea ice and argon
title_full_unstemmed Sea ice and argon
title_short Sea ice and argon
title_sort sea ice and argon
work_keys_str_mv AT hamblerc seaiceandargon