Demons in the North Atlantic: Variability of deep ocean ventilation
Translation of atmospheric forcing variability into the ocean interior via ocean ventilation is an important aspect of transient climate change. On a seasonal timescale in the subtropics, this translation is mediated by a so‐called “Demon” that prevents access to all except late‐winter mixed‐layer w...
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ftarchimer:oai:archimer.ifremer.fr:80055 2023-05-15T17:06:13+02:00 Demons in the North Atlantic: Variability of deep ocean ventilation Macgilchrist, G. A. Johnson, H. L. Lique, Camille Marshall, D. P. 2021-05 application/pdf https://archimer.ifremer.fr/doc/00688/80055/83058.pdf https://doi.org/10.1029/2020GL092340 https://archimer.ifremer.fr/doc/00688/80055/ eng eng American Geophysical Union (AGU) https://archimer.ifremer.fr/doc/00688/80055/83058.pdf doi:10.1029/2020GL092340 https://archimer.ifremer.fr/doc/00688/80055/ info:eu-repo/semantics/openAccess restricted use Geophysical Research Letters (0094-8276) (American Geophysical Union (AGU)), 2021-05 , Vol. 48 , N. 9 , P. e2020GL092340 (9p.) dense water formation Labrador Sea Lagrangian North Atlantic ocean mixed layer ocean ventilation text Publication info:eu-repo/semantics/article 2021 ftarchimer https://doi.org/10.1029/2020GL092340 2021-10-12T22:48:44Z Translation of atmospheric forcing variability into the ocean interior via ocean ventilation is an important aspect of transient climate change. On a seasonal timescale in the subtropics, this translation is mediated by a so‐called “Demon” that prevents access to all except late‐winter mixed‐layer water. Here, we use an eddy‐permitting numerical circulation model to investigate a similar process operating on longer (interannual) timescales in the subpolar North Atlantic. We find that variations in atmospheric forcing are mediated in their translation to the ocean interior, with year‐to‐year changes in the late‐winter mixed layer depth being the critical factor. The signature of persistent strong atmospheric forcing driving deep mixed layers is preferentially ventilated to the interior when the forcing is ceased. Susceptibility to this effect depends on the location and density of subduction — with the rate at which newly ventilated water escapes its region of subduction being the crucial factor. Plain Language Summary Water that leaves the ocean's surface boundary layer — where water is in direct contact with the overlying atmosphere — to be transported into the subsurface, is said to be “ventilated” (the name arising from the abundance of oxygen in newly ventilated water). The ventilation process, which carries implications for the ocean storage of climate‐relevant substances such as carbon dioxide, occurs only at certain times and under certain conditions. In describing a mechanism for the selective nature of ventilation over the seasonal cycle, Henry Stommel imagined a Demon sitting at the base of the surface boundary layer, granting access only to parcels of water that meet certain characteristics (namely their speed of “escape”). Thus, “Stommel's Demon” was born. Here, we investigate this same process as it operates in more northerly regions and on longer timescales. In so doing we give birth to a new “interannual Demon”, and describe its characteristics. Article in Journal/Newspaper Labrador Sea North Atlantic Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Geophysical Research Letters 48 9 |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
topic |
dense water formation Labrador Sea Lagrangian North Atlantic ocean mixed layer ocean ventilation |
spellingShingle |
dense water formation Labrador Sea Lagrangian North Atlantic ocean mixed layer ocean ventilation Macgilchrist, G. A. Johnson, H. L. Lique, Camille Marshall, D. P. Demons in the North Atlantic: Variability of deep ocean ventilation |
topic_facet |
dense water formation Labrador Sea Lagrangian North Atlantic ocean mixed layer ocean ventilation |
description |
Translation of atmospheric forcing variability into the ocean interior via ocean ventilation is an important aspect of transient climate change. On a seasonal timescale in the subtropics, this translation is mediated by a so‐called “Demon” that prevents access to all except late‐winter mixed‐layer water. Here, we use an eddy‐permitting numerical circulation model to investigate a similar process operating on longer (interannual) timescales in the subpolar North Atlantic. We find that variations in atmospheric forcing are mediated in their translation to the ocean interior, with year‐to‐year changes in the late‐winter mixed layer depth being the critical factor. The signature of persistent strong atmospheric forcing driving deep mixed layers is preferentially ventilated to the interior when the forcing is ceased. Susceptibility to this effect depends on the location and density of subduction — with the rate at which newly ventilated water escapes its region of subduction being the crucial factor. Plain Language Summary Water that leaves the ocean's surface boundary layer — where water is in direct contact with the overlying atmosphere — to be transported into the subsurface, is said to be “ventilated” (the name arising from the abundance of oxygen in newly ventilated water). The ventilation process, which carries implications for the ocean storage of climate‐relevant substances such as carbon dioxide, occurs only at certain times and under certain conditions. In describing a mechanism for the selective nature of ventilation over the seasonal cycle, Henry Stommel imagined a Demon sitting at the base of the surface boundary layer, granting access only to parcels of water that meet certain characteristics (namely their speed of “escape”). Thus, “Stommel's Demon” was born. Here, we investigate this same process as it operates in more northerly regions and on longer timescales. In so doing we give birth to a new “interannual Demon”, and describe its characteristics. |
format |
Article in Journal/Newspaper |
author |
Macgilchrist, G. A. Johnson, H. L. Lique, Camille Marshall, D. P. |
author_facet |
Macgilchrist, G. A. Johnson, H. L. Lique, Camille Marshall, D. P. |
author_sort |
Macgilchrist, G. A. |
title |
Demons in the North Atlantic: Variability of deep ocean ventilation |
title_short |
Demons in the North Atlantic: Variability of deep ocean ventilation |
title_full |
Demons in the North Atlantic: Variability of deep ocean ventilation |
title_fullStr |
Demons in the North Atlantic: Variability of deep ocean ventilation |
title_full_unstemmed |
Demons in the North Atlantic: Variability of deep ocean ventilation |
title_sort |
demons in the north atlantic: variability of deep ocean ventilation |
publisher |
American Geophysical Union (AGU) |
publishDate |
2021 |
url |
https://archimer.ifremer.fr/doc/00688/80055/83058.pdf https://doi.org/10.1029/2020GL092340 https://archimer.ifremer.fr/doc/00688/80055/ |
genre |
Labrador Sea North Atlantic |
genre_facet |
Labrador Sea North Atlantic |
op_source |
Geophysical Research Letters (0094-8276) (American Geophysical Union (AGU)), 2021-05 , Vol. 48 , N. 9 , P. e2020GL092340 (9p.) |
op_relation |
https://archimer.ifremer.fr/doc/00688/80055/83058.pdf doi:10.1029/2020GL092340 https://archimer.ifremer.fr/doc/00688/80055/ |
op_rights |
info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.1029/2020GL092340 |
container_title |
Geophysical Research Letters |
container_volume |
48 |
container_issue |
9 |
_version_ |
1766061256964308992 |