Sea ice and methane

1) The annual cycle of atmospheric methane in southern high latitudes is extremely highly correlated with Antarctic sea ice extent. 2) The annual cycle of atmospheric methane in the Arctic is highly correlated with Antarctic or Arctic plus Antarctic sea ice extent. 3) We propose the global annual cy...

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Bibliographic Details
Main Authors: Hambler, Clive, Henderson, Peter A.
Format: Article in Journal/Newspaper
Language:unknown
Published: arXiv 2020
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.2012.00839
https://arxiv.org/abs/2012.00839
id ftdatacite:10.48550/arxiv.2012.00839
record_format openpolar
spelling ftdatacite:10.48550/arxiv.2012.00839 2023-05-15T13:44:31+02:00 Sea ice and methane Hambler, Clive Henderson, Peter A. 2020 https://dx.doi.org/10.48550/arxiv.2012.00839 https://arxiv.org/abs/2012.00839 unknown arXiv Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Atmospheric and Oceanic Physics physics.ao-ph Geophysics physics.geo-ph FOS Physical sciences Article CreativeWork article Preprint 2020 ftdatacite https://doi.org/10.48550/arxiv.2012.00839 2022-03-10T15:01:19Z 1) The annual cycle of atmospheric methane in southern high latitudes is extremely highly correlated with Antarctic sea ice extent. 2) The annual cycle of atmospheric methane in the Arctic is highly correlated with Antarctic or Arctic plus Antarctic sea ice extent. 3) We propose the global annual cycle of atmospheric methane is largely driven by Antarctic sea ice dynamics, with relatively stronger influence from other fluxes (probably the biota) in the Northern Hemisphere. 4) We propose degassing during sea ice freeze and temperature dependent solubility in the ocean dominate the annual methane cycle. 5) Results provide evidence that carbon cycle pathways, parameters and predictions must be reassessed. : 27 pages including 2 appendices Article in Journal/Newspaper Antarc* Antarctic Arctic Sea ice DataCite Metadata Store (German National Library of Science and Technology) Antarctic Arctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Atmospheric and Oceanic Physics physics.ao-ph
Geophysics physics.geo-ph
FOS Physical sciences
spellingShingle Atmospheric and Oceanic Physics physics.ao-ph
Geophysics physics.geo-ph
FOS Physical sciences
Hambler, Clive
Henderson, Peter A.
Sea ice and methane
topic_facet Atmospheric and Oceanic Physics physics.ao-ph
Geophysics physics.geo-ph
FOS Physical sciences
description 1) The annual cycle of atmospheric methane in southern high latitudes is extremely highly correlated with Antarctic sea ice extent. 2) The annual cycle of atmospheric methane in the Arctic is highly correlated with Antarctic or Arctic plus Antarctic sea ice extent. 3) We propose the global annual cycle of atmospheric methane is largely driven by Antarctic sea ice dynamics, with relatively stronger influence from other fluxes (probably the biota) in the Northern Hemisphere. 4) We propose degassing during sea ice freeze and temperature dependent solubility in the ocean dominate the annual methane cycle. 5) Results provide evidence that carbon cycle pathways, parameters and predictions must be reassessed. : 27 pages including 2 appendices
format Article in Journal/Newspaper
author Hambler, Clive
Henderson, Peter A.
author_facet Hambler, Clive
Henderson, Peter A.
author_sort Hambler, Clive
title Sea ice and methane
title_short Sea ice and methane
title_full Sea ice and methane
title_fullStr Sea ice and methane
title_full_unstemmed Sea ice and methane
title_sort sea ice and methane
publisher arXiv
publishDate 2020
url https://dx.doi.org/10.48550/arxiv.2012.00839
https://arxiv.org/abs/2012.00839
geographic Antarctic
Arctic
geographic_facet Antarctic
Arctic
genre Antarc*
Antarctic
Arctic
Sea ice
genre_facet Antarc*
Antarctic
Arctic
Sea ice
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.48550/arxiv.2012.00839
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