Eddy heat flux across the Antarctic Circumpolar Current estimated from sea surface height standard deviation

Eddy heat flux (EHF) is a predominant mechanism for heat transport across the zonally unbounded mean flow of the Antarctic Circumpolar Current (ACC). Observations of dynamically relevant, divergent, 4 year mean EHF in Drake Passage from the cDrake project, as well as previous studies of atmospheric...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Foppert, A, Donohue, KA, Watts, DR, Tracey, KL
Format: Article in Journal/Newspaper
Language:English
Published: Wiley-Blackwell Publishing Inc. 2017
Subjects:
Online Access:https://doi.org/10.1002/2017JC012837
http://ecite.utas.edu.au/140516
id ftunivtasecite:oai:ecite.utas.edu.au:140516
record_format openpolar
spelling ftunivtasecite:oai:ecite.utas.edu.au:140516 2023-05-15T13:42:40+02:00 Eddy heat flux across the Antarctic Circumpolar Current estimated from sea surface height standard deviation Foppert, A Donohue, KA Watts, DR Tracey, KL 2017 application/pdf https://doi.org/10.1002/2017JC012837 http://ecite.utas.edu.au/140516 en eng Wiley-Blackwell Publishing Inc. http://ecite.utas.edu.au/140516/1/140516 - Eddy heat flux across the Antarctic Circumpolar Current estimated from sea.pdf http://dx.doi.org/10.1002/2017JC012837 Foppert, A and Donohue, KA and Watts, DR and Tracey, KL, Eddy heat flux across the Antarctic Circumpolar Current estimated from sea surface height standard deviation, Journal of Geophysical Research: Oceans, 122, (8) pp. 6947-6964. ISSN 2169-9275 (2017) [Refereed Article] http://ecite.utas.edu.au/140516 Earth Sciences Oceanography Physical oceanography Refereed Article PeerReviewed 2017 ftunivtasecite https://doi.org/10.1002/2017JC012837 2022-08-29T22:18:01Z Eddy heat flux (EHF) is a predominant mechanism for heat transport across the zonally unbounded mean flow of the Antarctic Circumpolar Current (ACC). Observations of dynamically relevant, divergent, 4 year mean EHF in Drake Passage from the cDrake project, as well as previous studies of atmospheric and oceanic storm tracks, motivates the use of sea surface height (SSH) standard deviation, H*, as a proxy for depth‐integrated, downgradient, time‐mean EHF in the ACC. Statistics from the Southern Ocean State Estimate corroborate this choice and validate throughout the ACC the spatial agreement between H* and EHF seen locally in Drake Passage. Eight regions of elevated EHF are identified from nearly 23.5 years of satellite altimetry data. Elevated cross‐front exchange usually does not span the full latitudinal width of the ACC in each region, implying a hand‐off of heat between ACC fronts and frontal zones as they encounter the different EHF hot spots along their circumpolar path. Integrated along circumpolar streamlines, defined by mean SSH contours, there is a convergence of EHF in the ACC: 1.06 PW enters from the north and 0.02 PW exits to the south. Temporal trends in low‐frequency [EHF] are calculated in a running‐mean sense using H* from overlapping 4 year subsets of SSH. Significant increases in downgradient [EHF] magnitude have occurred since 1993 at Kerguelen Plateau, Southeast Indian Ridge, and the Brazil‐Malvinas Confluence, whereas the other five EHF hot spots have insignificant trends of varying sign. Article in Journal/Newspaper Antarc* Antarctic Drake Passage Southern Ocean eCite UTAS (University of Tasmania) Antarctic Southern Ocean The Antarctic Kerguelen Drake Passage Indian Southeast Indian Ridge ENVELOPE(110.000,110.000,-50.000,-50.000) Journal of Geophysical Research: Oceans 122 8 6947 6964
institution Open Polar
collection eCite UTAS (University of Tasmania)
op_collection_id ftunivtasecite
language English
topic Earth Sciences
Oceanography
Physical oceanography
spellingShingle Earth Sciences
Oceanography
Physical oceanography
Foppert, A
Donohue, KA
Watts, DR
Tracey, KL
Eddy heat flux across the Antarctic Circumpolar Current estimated from sea surface height standard deviation
topic_facet Earth Sciences
Oceanography
Physical oceanography
description Eddy heat flux (EHF) is a predominant mechanism for heat transport across the zonally unbounded mean flow of the Antarctic Circumpolar Current (ACC). Observations of dynamically relevant, divergent, 4 year mean EHF in Drake Passage from the cDrake project, as well as previous studies of atmospheric and oceanic storm tracks, motivates the use of sea surface height (SSH) standard deviation, H*, as a proxy for depth‐integrated, downgradient, time‐mean EHF in the ACC. Statistics from the Southern Ocean State Estimate corroborate this choice and validate throughout the ACC the spatial agreement between H* and EHF seen locally in Drake Passage. Eight regions of elevated EHF are identified from nearly 23.5 years of satellite altimetry data. Elevated cross‐front exchange usually does not span the full latitudinal width of the ACC in each region, implying a hand‐off of heat between ACC fronts and frontal zones as they encounter the different EHF hot spots along their circumpolar path. Integrated along circumpolar streamlines, defined by mean SSH contours, there is a convergence of EHF in the ACC: 1.06 PW enters from the north and 0.02 PW exits to the south. Temporal trends in low‐frequency [EHF] are calculated in a running‐mean sense using H* from overlapping 4 year subsets of SSH. Significant increases in downgradient [EHF] magnitude have occurred since 1993 at Kerguelen Plateau, Southeast Indian Ridge, and the Brazil‐Malvinas Confluence, whereas the other five EHF hot spots have insignificant trends of varying sign.
format Article in Journal/Newspaper
author Foppert, A
Donohue, KA
Watts, DR
Tracey, KL
author_facet Foppert, A
Donohue, KA
Watts, DR
Tracey, KL
author_sort Foppert, A
title Eddy heat flux across the Antarctic Circumpolar Current estimated from sea surface height standard deviation
title_short Eddy heat flux across the Antarctic Circumpolar Current estimated from sea surface height standard deviation
title_full Eddy heat flux across the Antarctic Circumpolar Current estimated from sea surface height standard deviation
title_fullStr Eddy heat flux across the Antarctic Circumpolar Current estimated from sea surface height standard deviation
title_full_unstemmed Eddy heat flux across the Antarctic Circumpolar Current estimated from sea surface height standard deviation
title_sort eddy heat flux across the antarctic circumpolar current estimated from sea surface height standard deviation
publisher Wiley-Blackwell Publishing Inc.
publishDate 2017
url https://doi.org/10.1002/2017JC012837
http://ecite.utas.edu.au/140516
long_lat ENVELOPE(110.000,110.000,-50.000,-50.000)
geographic Antarctic
Southern Ocean
The Antarctic
Kerguelen
Drake Passage
Indian
Southeast Indian Ridge
geographic_facet Antarctic
Southern Ocean
The Antarctic
Kerguelen
Drake Passage
Indian
Southeast Indian Ridge
genre Antarc*
Antarctic
Drake Passage
Southern Ocean
genre_facet Antarc*
Antarctic
Drake Passage
Southern Ocean
op_relation http://ecite.utas.edu.au/140516/1/140516 - Eddy heat flux across the Antarctic Circumpolar Current estimated from sea.pdf
http://dx.doi.org/10.1002/2017JC012837
Foppert, A and Donohue, KA and Watts, DR and Tracey, KL, Eddy heat flux across the Antarctic Circumpolar Current estimated from sea surface height standard deviation, Journal of Geophysical Research: Oceans, 122, (8) pp. 6947-6964. ISSN 2169-9275 (2017) [Refereed Article]
http://ecite.utas.edu.au/140516
op_doi https://doi.org/10.1002/2017JC012837
container_title Journal of Geophysical Research: Oceans
container_volume 122
container_issue 8
container_start_page 6947
op_container_end_page 6964
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