Sea ice and carbon dioxide

1) The annual cycles of atmospheric CO₂ at Mauna Loa and Point Barrow (Alaska) are statistically almost completely explained by changes in Arctic sea ice volume and extent. 2) The annual cycles of atmospheric CO₂ at the South Pole and at Palmer Station are statistically largely explained by changes...

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Main Authors: Hambler, C, Henderson, PA
Format: Report
Language:English
Published: 2020
Subjects:
Online Access:https://ora.ox.ac.uk/objects/uuid:640a0c7e-6b55-4aff-a9cc-f47f6b490254
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spelling ftuloxford:oai:ora.ox.ac.uk:uuid:640a0c7e-6b55-4aff-a9cc-f47f6b490254 2024-10-06T13:42:43+00:00 Sea ice and carbon dioxide Hambler, C Henderson, PA 2020-09-25 https://ora.ox.ac.uk/objects/uuid:640a0c7e-6b55-4aff-a9cc-f47f6b490254 eng eng https://ora.ox.ac.uk/objects/uuid:640a0c7e-6b55-4aff-a9cc-f47f6b490254 info:eu-repo/semantics/openAccess Working paper 2020 ftuloxford 2024-09-06T07:47:35Z 1) The annual cycles of atmospheric CO₂ at Mauna Loa and Point Barrow (Alaska) are statistically almost completely explained by changes in Arctic sea ice volume and extent. 2) The annual cycles of atmospheric CO₂ at the South Pole and at Palmer Station are statistically largely explained by changes in Antarctic sea ice extent. 3) Results are consistent with a monthly CO₂ flux dependent on the distance from equilibrium of a temperature dependent process. Degassing and calcium carbonate crystal formation during the sea ice freeze likely contribute to the peak net monthly emission rate of CO₂. High solubility of gas in cold sea ice meltwater and dissolution of calcium carbonate likely contribute to the peak net monthly sink rate of CO₂. 4) The global annual mean Lower Tropospheric temperature anomaly has high predictive value for annual CO₂ changes, consistent with marine outgassing (and possibly vertical transport mediated by sea ice). 5) The global carbon cycle is poorly understood, with abiotic factors likely dominating biotic fluxes - and little scope for substantive human involvement in the annual cycle. 6) A new investigative paradigm is required in which atmospheric CO₂ level is a response variable of temperature or an unknown covariate. 7) Climate predictions and attributions must be revisited. 8) The policy implications are as significant as the relationship between sea ice and CO₂ rates. Report Antarc* Antarctic Arctic Barrow Point Barrow Sea ice South pole South pole Alaska ORA - Oxford University Research Archive Antarctic Arctic Palmer Station ENVELOPE(-64.050,-64.050,-64.770,-64.770) Palmer-Station ENVELOPE(-64.050,-64.050,-64.770,-64.770) South Pole
institution Open Polar
collection ORA - Oxford University Research Archive
op_collection_id ftuloxford
language English
description 1) The annual cycles of atmospheric CO₂ at Mauna Loa and Point Barrow (Alaska) are statistically almost completely explained by changes in Arctic sea ice volume and extent. 2) The annual cycles of atmospheric CO₂ at the South Pole and at Palmer Station are statistically largely explained by changes in Antarctic sea ice extent. 3) Results are consistent with a monthly CO₂ flux dependent on the distance from equilibrium of a temperature dependent process. Degassing and calcium carbonate crystal formation during the sea ice freeze likely contribute to the peak net monthly emission rate of CO₂. High solubility of gas in cold sea ice meltwater and dissolution of calcium carbonate likely contribute to the peak net monthly sink rate of CO₂. 4) The global annual mean Lower Tropospheric temperature anomaly has high predictive value for annual CO₂ changes, consistent with marine outgassing (and possibly vertical transport mediated by sea ice). 5) The global carbon cycle is poorly understood, with abiotic factors likely dominating biotic fluxes - and little scope for substantive human involvement in the annual cycle. 6) A new investigative paradigm is required in which atmospheric CO₂ level is a response variable of temperature or an unknown covariate. 7) Climate predictions and attributions must be revisited. 8) The policy implications are as significant as the relationship between sea ice and CO₂ rates.
format Report
author Hambler, C
Henderson, PA
spellingShingle Hambler, C
Henderson, PA
Sea ice and carbon dioxide
author_facet Hambler, C
Henderson, PA
author_sort Hambler, C
title Sea ice and carbon dioxide
title_short Sea ice and carbon dioxide
title_full Sea ice and carbon dioxide
title_fullStr Sea ice and carbon dioxide
title_full_unstemmed Sea ice and carbon dioxide
title_sort sea ice and carbon dioxide
publishDate 2020
url https://ora.ox.ac.uk/objects/uuid:640a0c7e-6b55-4aff-a9cc-f47f6b490254
long_lat ENVELOPE(-64.050,-64.050,-64.770,-64.770)
ENVELOPE(-64.050,-64.050,-64.770,-64.770)
geographic Antarctic
Arctic
Palmer Station
Palmer-Station
South Pole
geographic_facet Antarctic
Arctic
Palmer Station
Palmer-Station
South Pole
genre Antarc*
Antarctic
Arctic
Barrow
Point Barrow
Sea ice
South pole
South pole
Alaska
genre_facet Antarc*
Antarctic
Arctic
Barrow
Point Barrow
Sea ice
South pole
South pole
Alaska
op_relation https://ora.ox.ac.uk/objects/uuid:640a0c7e-6b55-4aff-a9cc-f47f6b490254
op_rights info:eu-repo/semantics/openAccess
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