Near‐Surface Stratification Due to Ice Melt Biases Arctic Air‐Sea CO 2 Flux Estimates
Air-sea carbon dioxide (CO2) flux is generally estimated by the bulk method using upper ocean CO2 fugacity measurements. In the summertime Arctic, sea-ice melt results in stratification within the upper ocean (top ∼10 m), which can bias bulk CO2 flux estimates when the seawater CO2 fugacity is taken...
Published in: | Geophysical Research Letters |
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Online Access: | http://plymsea.ac.uk/id/eprint/9484/ http://plymsea.ac.uk/id/eprint/9484/1/2021GL095266.pdf https://doi.org/10.1029/2021GL095266 |
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ftplymouthml:oai:plymsea.ac.uk:9484 2023-05-15T14:26:10+02:00 Near‐Surface Stratification Due to Ice Melt Biases Arctic Air‐Sea CO 2 Flux Estimates Dong, Y Yang, M Bakker, DCE Liss, PS Kitidis, V Brown, IJ Chierici, M Fransson, A Bell, TG 2021-11-23 text http://plymsea.ac.uk/id/eprint/9484/ http://plymsea.ac.uk/id/eprint/9484/1/2021GL095266.pdf https://doi.org/10.1029/2021GL095266 en eng AGU http://plymsea.ac.uk/id/eprint/9484/1/2021GL095266.pdf Dong, Y; Yang, M; Bakker, DCE; Liss, PS; Kitidis, V; Brown, IJ; Chierici, M; Fransson, A; Bell, TG. 2021 Near‐Surface Stratification Due to Ice Melt Biases Arctic Air‐Sea CO 2 Flux Estimates. Geophysical Research Letters, 48 (22). https://doi.org/10.1029/2021GL095266 <https://doi.org/10.1029/2021GL095266> cc_by_4 CC-BY Publication - Article PeerReviewed 2021 ftplymouthml https://doi.org/10.1029/2021GL095266 2022-09-13T05:49:58Z Air-sea carbon dioxide (CO2) flux is generally estimated by the bulk method using upper ocean CO2 fugacity measurements. In the summertime Arctic, sea-ice melt results in stratification within the upper ocean (top ∼10 m), which can bias bulk CO2 flux estimates when the seawater CO2 fugacity is taken from a ship's seawater inlet at ∼6 m depth (fCO2w_bulk). Direct flux measurements by eddy covariance are unaffected by near-surface stratification. We use eddy covariance CO2 flux measurements to infer sea surface CO2 fugacity (fCO2w_surface) in the Arctic Ocean. In sea-ice melt regions, fCO2w_surface values are consistently lower than fCO2w_bulk by an average of 39 μatm. Lower fCO2w_surface can be partially accounted for by fresher (≥27%) and colder (17%) melt waters. A back-of-the-envelope calculation shows that neglecting the summertime sea-ice melt could lead to a 6%–17% underestimate of the annual Arctic Ocean CO2 uptake. Article in Journal/Newspaper Arctic Arctic Arctic Ocean Sea ice Plymouth Marine Science Electronic Archive (PlyMSEA - Plymouth Marine Laboratory, PML) Arctic Arctic Ocean Geophysical Research Letters 48 22 |
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Open Polar |
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Plymouth Marine Science Electronic Archive (PlyMSEA - Plymouth Marine Laboratory, PML) |
op_collection_id |
ftplymouthml |
language |
English |
description |
Air-sea carbon dioxide (CO2) flux is generally estimated by the bulk method using upper ocean CO2 fugacity measurements. In the summertime Arctic, sea-ice melt results in stratification within the upper ocean (top ∼10 m), which can bias bulk CO2 flux estimates when the seawater CO2 fugacity is taken from a ship's seawater inlet at ∼6 m depth (fCO2w_bulk). Direct flux measurements by eddy covariance are unaffected by near-surface stratification. We use eddy covariance CO2 flux measurements to infer sea surface CO2 fugacity (fCO2w_surface) in the Arctic Ocean. In sea-ice melt regions, fCO2w_surface values are consistently lower than fCO2w_bulk by an average of 39 μatm. Lower fCO2w_surface can be partially accounted for by fresher (≥27%) and colder (17%) melt waters. A back-of-the-envelope calculation shows that neglecting the summertime sea-ice melt could lead to a 6%–17% underestimate of the annual Arctic Ocean CO2 uptake. |
format |
Article in Journal/Newspaper |
author |
Dong, Y Yang, M Bakker, DCE Liss, PS Kitidis, V Brown, IJ Chierici, M Fransson, A Bell, TG |
spellingShingle |
Dong, Y Yang, M Bakker, DCE Liss, PS Kitidis, V Brown, IJ Chierici, M Fransson, A Bell, TG Near‐Surface Stratification Due to Ice Melt Biases Arctic Air‐Sea CO 2 Flux Estimates |
author_facet |
Dong, Y Yang, M Bakker, DCE Liss, PS Kitidis, V Brown, IJ Chierici, M Fransson, A Bell, TG |
author_sort |
Dong, Y |
title |
Near‐Surface Stratification Due to Ice Melt Biases Arctic Air‐Sea CO 2 Flux Estimates |
title_short |
Near‐Surface Stratification Due to Ice Melt Biases Arctic Air‐Sea CO 2 Flux Estimates |
title_full |
Near‐Surface Stratification Due to Ice Melt Biases Arctic Air‐Sea CO 2 Flux Estimates |
title_fullStr |
Near‐Surface Stratification Due to Ice Melt Biases Arctic Air‐Sea CO 2 Flux Estimates |
title_full_unstemmed |
Near‐Surface Stratification Due to Ice Melt Biases Arctic Air‐Sea CO 2 Flux Estimates |
title_sort |
near‐surface stratification due to ice melt biases arctic air‐sea co 2 flux estimates |
publisher |
AGU |
publishDate |
2021 |
url |
http://plymsea.ac.uk/id/eprint/9484/ http://plymsea.ac.uk/id/eprint/9484/1/2021GL095266.pdf https://doi.org/10.1029/2021GL095266 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Arctic Ocean Sea ice |
genre_facet |
Arctic Arctic Arctic Ocean Sea ice |
op_relation |
http://plymsea.ac.uk/id/eprint/9484/1/2021GL095266.pdf Dong, Y; Yang, M; Bakker, DCE; Liss, PS; Kitidis, V; Brown, IJ; Chierici, M; Fransson, A; Bell, TG. 2021 Near‐Surface Stratification Due to Ice Melt Biases Arctic Air‐Sea CO 2 Flux Estimates. Geophysical Research Letters, 48 (22). https://doi.org/10.1029/2021GL095266 <https://doi.org/10.1029/2021GL095266> |
op_rights |
cc_by_4 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1029/2021GL095266 |
container_title |
Geophysical Research Letters |
container_volume |
48 |
container_issue |
22 |
_version_ |
1766298642324389888 |