Deglacial Carbon Escape From the Northern Rim of the Southern Ocean
Abstract The Southern Ocean regulates atmospheric CO2 and Earth's climate as a critical region for air‐sea gas exchange, delicately poised between being a CO2 source and sink. Here, we estimate how long a water mass has remained isolated from the atmosphere and utilize 14C/12C ratios (Δ14C) to...
Published in: | Geophysical Research Letters |
---|---|
Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2024
|
Subjects: | |
Online Access: | https://doi.org/10.1029/2023GL106413 https://doaj.org/article/69d96e5042954ed6b5ca7ceb1bdd7c95 |
id |
ftdoajarticles:oai:doaj.org/article:69d96e5042954ed6b5ca7ceb1bdd7c95 |
---|---|
record_format |
openpolar |
spelling |
ftdoajarticles:oai:doaj.org/article:69d96e5042954ed6b5ca7ceb1bdd7c95 2024-09-15T17:48:19+00:00 Deglacial Carbon Escape From the Northern Rim of the Southern Ocean N. E. Umling E. Sikes P. Rafter N. F. Goodkin J. R. Southon 2024-04-01T00:00:00Z https://doi.org/10.1029/2023GL106413 https://doaj.org/article/69d96e5042954ed6b5ca7ceb1bdd7c95 EN eng Wiley https://doi.org/10.1029/2023GL106413 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL106413 https://doaj.org/article/69d96e5042954ed6b5ca7ceb1bdd7c95 Geophysical Research Letters, Vol 51, Iss 8, Pp n/a-n/a (2024) Antarctic intermediate water radiocarbon ventilation glacial foraminifera Geophysics. Cosmic physics QC801-809 article 2024 ftdoajarticles https://doi.org/10.1029/2023GL106413 2024-08-05T17:49:22Z Abstract The Southern Ocean regulates atmospheric CO2 and Earth's climate as a critical region for air‐sea gas exchange, delicately poised between being a CO2 source and sink. Here, we estimate how long a water mass has remained isolated from the atmosphere and utilize 14C/12C ratios (Δ14C) to trace the pathway and escape route of carbon sequestered in the deep ocean through the mixed layer to the atmosphere. The position of our core at the northern margin of the Southern Indian Ocean, tracks latitudinal shifts of the Southern Ocean frontal zones across the deglaciation. Our results suggest an expanded glacial Antarctic region trapped CO2, whereas deglacial expansion of the subantarctic permitted ventilation of the trapped CO2, contributing to a rapid atmospheric CO2 rise. We identify frontal positions as a key factor balancing CO2 outgassing versus sequestration in a region currently responsible for nearly half of global ocean CO2 uptake. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 51 8 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Antarctic intermediate water radiocarbon ventilation glacial foraminifera Geophysics. Cosmic physics QC801-809 |
spellingShingle |
Antarctic intermediate water radiocarbon ventilation glacial foraminifera Geophysics. Cosmic physics QC801-809 N. E. Umling E. Sikes P. Rafter N. F. Goodkin J. R. Southon Deglacial Carbon Escape From the Northern Rim of the Southern Ocean |
topic_facet |
Antarctic intermediate water radiocarbon ventilation glacial foraminifera Geophysics. Cosmic physics QC801-809 |
description |
Abstract The Southern Ocean regulates atmospheric CO2 and Earth's climate as a critical region for air‐sea gas exchange, delicately poised between being a CO2 source and sink. Here, we estimate how long a water mass has remained isolated from the atmosphere and utilize 14C/12C ratios (Δ14C) to trace the pathway and escape route of carbon sequestered in the deep ocean through the mixed layer to the atmosphere. The position of our core at the northern margin of the Southern Indian Ocean, tracks latitudinal shifts of the Southern Ocean frontal zones across the deglaciation. Our results suggest an expanded glacial Antarctic region trapped CO2, whereas deglacial expansion of the subantarctic permitted ventilation of the trapped CO2, contributing to a rapid atmospheric CO2 rise. We identify frontal positions as a key factor balancing CO2 outgassing versus sequestration in a region currently responsible for nearly half of global ocean CO2 uptake. |
format |
Article in Journal/Newspaper |
author |
N. E. Umling E. Sikes P. Rafter N. F. Goodkin J. R. Southon |
author_facet |
N. E. Umling E. Sikes P. Rafter N. F. Goodkin J. R. Southon |
author_sort |
N. E. Umling |
title |
Deglacial Carbon Escape From the Northern Rim of the Southern Ocean |
title_short |
Deglacial Carbon Escape From the Northern Rim of the Southern Ocean |
title_full |
Deglacial Carbon Escape From the Northern Rim of the Southern Ocean |
title_fullStr |
Deglacial Carbon Escape From the Northern Rim of the Southern Ocean |
title_full_unstemmed |
Deglacial Carbon Escape From the Northern Rim of the Southern Ocean |
title_sort |
deglacial carbon escape from the northern rim of the southern ocean |
publisher |
Wiley |
publishDate |
2024 |
url |
https://doi.org/10.1029/2023GL106413 https://doaj.org/article/69d96e5042954ed6b5ca7ceb1bdd7c95 |
genre |
Antarc* Antarctic Southern Ocean |
genre_facet |
Antarc* Antarctic Southern Ocean |
op_source |
Geophysical Research Letters, Vol 51, Iss 8, Pp n/a-n/a (2024) |
op_relation |
https://doi.org/10.1029/2023GL106413 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL106413 https://doaj.org/article/69d96e5042954ed6b5ca7ceb1bdd7c95 |
op_doi |
https://doi.org/10.1029/2023GL106413 |
container_title |
Geophysical Research Letters |
container_volume |
51 |
container_issue |
8 |
_version_ |
1810289464437637120 |