Contribution of topographically-generated submesoscale turbulence to Southern Ocean overturning

The ocean's global overturning circulation regulates the transport and storage of heat, carbon and nutrients. Upwelling across the Southern Ocean's Antarctic Circumpolar Current and into the mixed layer, coupled to water mass modification by surface buoyancy forcing, has been highlighted a...

Full description

Bibliographic Details
Published in:Nature Geoscience
Main Authors: Ruan, Xiaozhou, Thompson, Andrew F., Flexas, Mar M., Sprintall, Janet
Format: Article in Journal/Newspaper
Language:unknown
Published: Nature Publishing Group 2017
Subjects:
Online Access:https://doi.org/10.1038/NGEO3053
id ftcaltechauth:oai:authors.library.caltech.edu:eh7hr-00n40
record_format openpolar
spelling ftcaltechauth:oai:authors.library.caltech.edu:eh7hr-00n40 2024-06-23T07:47:50+00:00 Contribution of topographically-generated submesoscale turbulence to Southern Ocean overturning Ruan, Xiaozhou Thompson, Andrew F. Flexas, Mar M. Sprintall, Janet 2017-11 https://doi.org/10.1038/NGEO3053 unknown Nature Publishing Group https://doi.org/10.1038/NGEO3053 oai:authors.library.caltech.edu:eh7hr-00n40 eprintid:80899 resolverid:CaltechAUTHORS:20170829-110203986 info:eu-repo/semantics/openAccess Other Nature Geoscience, 10(11), 840-845, (2017-11) info:eu-repo/semantics/article 2017 ftcaltechauth https://doi.org/10.1038/NGEO3053 2024-06-12T03:19:13Z The ocean's global overturning circulation regulates the transport and storage of heat, carbon and nutrients. Upwelling across the Southern Ocean's Antarctic Circumpolar Current and into the mixed layer, coupled to water mass modification by surface buoyancy forcing, has been highlighted as a key process in the closure of the overturning circulation. Here, using twelve high-resolution hydrographic sections in southern Drake Passage, collected with autonomous ocean gliders, we show that Circumpolar Deep Water originating from the North Atlantic, known as Lower Circumpolar Deep Water, intersects sloping topography in narrow and strong boundary currents. Observations of strong lateral buoyancy gradients, enhanced bottom turbulence, thick bottom mixed layers and modified water masses are consistent with growing evidence that topographically generated submesoscale flows over continental slopes enhance near-bottom mixing, and that cross-density upwelling occurs preferentially over sloping topography. Interactions between narrow frontal currents and topography occur elsewhere along the path of the Antarctic Circumpolar Current, which leads us to propose that such interactions contribute significantly to the closure of the overturning in the Southern Ocean. © 2017 Macmillan Publishers Limited, part of Springer Nature. Received: 11 May 2017; Accepted: 20 September 2017; Published online: 30 October 2017. X.R., A.F.T. and M.M.F. received support from NSF grant OPP-1246460. J.S. received support from NSF grant OPP-1246160. A.F.T. also received support from the David and Lucille Packard Foundation. Author Contributions: A.F.T. and J.S. conceived and designed the field programme; X.R., A.F.T. and J.S. collected the data; X.R., A.F.T. and M.M.F. analysed the data; X.R., A.F.T., M.M.F. and J.S. co-wrote the paper. The authors declare no competing financial interests. Supplemental Material - ngeo3053-s1.pdf Article in Journal/Newspaper Antarc* Antarctic Drake Passage North Atlantic Southern Ocean Caltech Authors (California Institute of Technology) Antarctic Drake Passage Southern Ocean The Antarctic Nature Geoscience 10 11 840 845
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
description The ocean's global overturning circulation regulates the transport and storage of heat, carbon and nutrients. Upwelling across the Southern Ocean's Antarctic Circumpolar Current and into the mixed layer, coupled to water mass modification by surface buoyancy forcing, has been highlighted as a key process in the closure of the overturning circulation. Here, using twelve high-resolution hydrographic sections in southern Drake Passage, collected with autonomous ocean gliders, we show that Circumpolar Deep Water originating from the North Atlantic, known as Lower Circumpolar Deep Water, intersects sloping topography in narrow and strong boundary currents. Observations of strong lateral buoyancy gradients, enhanced bottom turbulence, thick bottom mixed layers and modified water masses are consistent with growing evidence that topographically generated submesoscale flows over continental slopes enhance near-bottom mixing, and that cross-density upwelling occurs preferentially over sloping topography. Interactions between narrow frontal currents and topography occur elsewhere along the path of the Antarctic Circumpolar Current, which leads us to propose that such interactions contribute significantly to the closure of the overturning in the Southern Ocean. © 2017 Macmillan Publishers Limited, part of Springer Nature. Received: 11 May 2017; Accepted: 20 September 2017; Published online: 30 October 2017. X.R., A.F.T. and M.M.F. received support from NSF grant OPP-1246460. J.S. received support from NSF grant OPP-1246160. A.F.T. also received support from the David and Lucille Packard Foundation. Author Contributions: A.F.T. and J.S. conceived and designed the field programme; X.R., A.F.T. and J.S. collected the data; X.R., A.F.T. and M.M.F. analysed the data; X.R., A.F.T., M.M.F. and J.S. co-wrote the paper. The authors declare no competing financial interests. Supplemental Material - ngeo3053-s1.pdf
format Article in Journal/Newspaper
author Ruan, Xiaozhou
Thompson, Andrew F.
Flexas, Mar M.
Sprintall, Janet
spellingShingle Ruan, Xiaozhou
Thompson, Andrew F.
Flexas, Mar M.
Sprintall, Janet
Contribution of topographically-generated submesoscale turbulence to Southern Ocean overturning
author_facet Ruan, Xiaozhou
Thompson, Andrew F.
Flexas, Mar M.
Sprintall, Janet
author_sort Ruan, Xiaozhou
title Contribution of topographically-generated submesoscale turbulence to Southern Ocean overturning
title_short Contribution of topographically-generated submesoscale turbulence to Southern Ocean overturning
title_full Contribution of topographically-generated submesoscale turbulence to Southern Ocean overturning
title_fullStr Contribution of topographically-generated submesoscale turbulence to Southern Ocean overturning
title_full_unstemmed Contribution of topographically-generated submesoscale turbulence to Southern Ocean overturning
title_sort contribution of topographically-generated submesoscale turbulence to southern ocean overturning
publisher Nature Publishing Group
publishDate 2017
url https://doi.org/10.1038/NGEO3053
geographic Antarctic
Drake Passage
Southern Ocean
The Antarctic
geographic_facet Antarctic
Drake Passage
Southern Ocean
The Antarctic
genre Antarc*
Antarctic
Drake Passage
North Atlantic
Southern Ocean
genre_facet Antarc*
Antarctic
Drake Passage
North Atlantic
Southern Ocean
op_source Nature Geoscience, 10(11), 840-845, (2017-11)
op_relation https://doi.org/10.1038/NGEO3053
oai:authors.library.caltech.edu:eh7hr-00n40
eprintid:80899
resolverid:CaltechAUTHORS:20170829-110203986
op_rights info:eu-repo/semantics/openAccess
Other
op_doi https://doi.org/10.1038/NGEO3053
container_title Nature Geoscience
container_volume 10
container_issue 11
container_start_page 840
op_container_end_page 845
_version_ 1802638027030265856