Eddy response to Southern Ocean climate modes

Interannual variations in Southern Ocean eddy kinetic energy (EKE) are investigated using 16 years of altimetric data. Circumpolar averages show a peak in EKE from 2000 to 2002, 2-3 years after the peak in the Southern Annular Mode (SAM) index. Although the SAM forcing is in phase around the circump...

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Main Authors: Morrow, R., Ward, Marshall, Hogg, Andrew, Pasquet, S.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2015
Subjects:
Online Access:http://hdl.handle.net/1885/33526
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spelling ftanucanberra:oai:digitalcollections.anu.edu.au:1885/33526 2023-05-15T18:24:48+02:00 Eddy response to Southern Ocean climate modes Morrow, R. Ward, Marshall Hogg, Andrew Pasquet, S. 2015-12-08T22:25:39Z http://hdl.handle.net/1885/33526 unknown American Geophysical Union 0148-0227 http://hdl.handle.net/1885/33526 Journal of Geophysical Research Journal article 2015 ftanucanberra 2015-12-28T23:24:11Z Interannual variations in Southern Ocean eddy kinetic energy (EKE) are investigated using 16 years of altimetric data. Circumpolar averages show a peak in EKE from 2000 to 2002, 2-3 years after the peak in the Southern Annular Mode (SAM) index. Although the SAM forcing is in phase around the circumpolar band, we find the EKE response varies regionally. The strongest EKE is in the Pacific, with energy peaks occurring progressively later toward the east. We suggest that this is due to the presence of two climate modes: SAM and ENSO. When strong positive SAM events coincide with La Niña periods, as in 1999, anomalous meridional wind forcing is enhanced in the South Pacific Ocean, contributing to the observed increase in EKE 2-3 years later. When positive SAM events coincide with El Niño periods, as in 1993, the climate modes are in opposition in the South Pacific, leading to a weak EKE response during the mid-1990s. Numerical modeling supports these observations. By applying different combinations of SAM and ENSO, we can reproduce both the elevated Pacific EKE response to SAM as well as an additional amplification/suppression of EKE during La Niña/El Niño. In general, we find that the EKE response depends on the interplay between wind forcing, topography, and mean flow and produces a strongly heterogeneous distribution in the Southern Ocean. Article in Journal/Newspaper Southern Ocean Australian National University: ANU Digital Collections Pacific Southern Ocean
institution Open Polar
collection Australian National University: ANU Digital Collections
op_collection_id ftanucanberra
language unknown
description Interannual variations in Southern Ocean eddy kinetic energy (EKE) are investigated using 16 years of altimetric data. Circumpolar averages show a peak in EKE from 2000 to 2002, 2-3 years after the peak in the Southern Annular Mode (SAM) index. Although the SAM forcing is in phase around the circumpolar band, we find the EKE response varies regionally. The strongest EKE is in the Pacific, with energy peaks occurring progressively later toward the east. We suggest that this is due to the presence of two climate modes: SAM and ENSO. When strong positive SAM events coincide with La Niña periods, as in 1999, anomalous meridional wind forcing is enhanced in the South Pacific Ocean, contributing to the observed increase in EKE 2-3 years later. When positive SAM events coincide with El Niño periods, as in 1993, the climate modes are in opposition in the South Pacific, leading to a weak EKE response during the mid-1990s. Numerical modeling supports these observations. By applying different combinations of SAM and ENSO, we can reproduce both the elevated Pacific EKE response to SAM as well as an additional amplification/suppression of EKE during La Niña/El Niño. In general, we find that the EKE response depends on the interplay between wind forcing, topography, and mean flow and produces a strongly heterogeneous distribution in the Southern Ocean.
format Article in Journal/Newspaper
author Morrow, R.
Ward, Marshall
Hogg, Andrew
Pasquet, S.
spellingShingle Morrow, R.
Ward, Marshall
Hogg, Andrew
Pasquet, S.
Eddy response to Southern Ocean climate modes
author_facet Morrow, R.
Ward, Marshall
Hogg, Andrew
Pasquet, S.
author_sort Morrow, R.
title Eddy response to Southern Ocean climate modes
title_short Eddy response to Southern Ocean climate modes
title_full Eddy response to Southern Ocean climate modes
title_fullStr Eddy response to Southern Ocean climate modes
title_full_unstemmed Eddy response to Southern Ocean climate modes
title_sort eddy response to southern ocean climate modes
publisher American Geophysical Union
publishDate 2015
url http://hdl.handle.net/1885/33526
geographic Pacific
Southern Ocean
geographic_facet Pacific
Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_source Journal of Geophysical Research
op_relation 0148-0227
http://hdl.handle.net/1885/33526
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