Antarctic circumpolar modes in a coupled ocean-atmosphere model

Eastward-propagating patterns in anomalous potential temperature and salinity of the Southern Ocean are analyzed in the output of a 1000-year simulation of the global coupled atmosphere-ocean GCM ECHO-G. Such features can be associated with the socalled Antarctic Circumpolar Wave (ACW). It is found...

Full description

Bibliographic Details
Published in:Ocean Dynamics
Main Authors: Marsland, SJ, Latif, M, Legutke, S
Format: Article in Journal/Newspaper
Language:English
Published: Springer Heidelberg 2003
Subjects:
Online Access:https://doi.org/10.1007/s10236-003-0041-z
http://ecite.utas.edu.au/35567
id ftunivtasecite:oai:ecite.utas.edu.au:35567
record_format openpolar
spelling ftunivtasecite:oai:ecite.utas.edu.au:35567 2023-05-15T14:03:55+02:00 Antarctic circumpolar modes in a coupled ocean-atmosphere model Marsland, SJ Latif, M Legutke, S 2003 https://doi.org/10.1007/s10236-003-0041-z http://ecite.utas.edu.au/35567 en eng Springer Heidelberg http://dx.doi.org/10.1007/s10236-003-0041-z Marsland, SJ and Latif, M and Legutke, S, Antarctic circumpolar modes in a coupled ocean-atmosphere model, Ocean Dynamics, 53, (4) pp. 323-331. ISSN 1616-7341 (2003) [Refereed Article] http://ecite.utas.edu.au/35567 Earth Sciences Oceanography Physical Oceanography Refereed Article PeerReviewed 2003 ftunivtasecite https://doi.org/10.1007/s10236-003-0041-z 2019-12-13T21:14:03Z Eastward-propagating patterns in anomalous potential temperature and salinity of the Southern Ocean are analyzed in the output of a 1000-year simulation of the global coupled atmosphere-ocean GCM ECHO-G. Such features can be associated with the socalled Antarctic Circumpolar Wave (ACW). It is found that time-longitude diagrams that have traditionally been used to aid the visualization of the ACW are strongly influenced by the width of the bandpass time filtering. This is due to the masking of considerable lowfrequency variability that occurs over a broad range of time scales. Frequency-wavenumber analysis of the ACW shows that the eastward-propagating waves do have preferred spectral peaks, but that both the period and wavenumber change erratically when comparing different centuries throughout the simulation. The variability of the ACW on a variety of time scales from interannual to centennial suggests that the waiting time for a sufficient observational record to determine the time scale of variability of the real world ACW (and the associated decadal time scale predictability of climate for southern landmasses) will be a very long one. Springer-Verlag 2003. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean eCite UTAS (University of Tasmania) Antarctic Southern Ocean Ocean Dynamics 53 4 323 331
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
Marsland, SJ
Latif, M
Legutke, S
Antarctic circumpolar modes in a coupled ocean-atmosphere model
topic_facet Earth Sciences
Oceanography
Physical Oceanography
description Eastward-propagating patterns in anomalous potential temperature and salinity of the Southern Ocean are analyzed in the output of a 1000-year simulation of the global coupled atmosphere-ocean GCM ECHO-G. Such features can be associated with the socalled Antarctic Circumpolar Wave (ACW). It is found that time-longitude diagrams that have traditionally been used to aid the visualization of the ACW are strongly influenced by the width of the bandpass time filtering. This is due to the masking of considerable lowfrequency variability that occurs over a broad range of time scales. Frequency-wavenumber analysis of the ACW shows that the eastward-propagating waves do have preferred spectral peaks, but that both the period and wavenumber change erratically when comparing different centuries throughout the simulation. The variability of the ACW on a variety of time scales from interannual to centennial suggests that the waiting time for a sufficient observational record to determine the time scale of variability of the real world ACW (and the associated decadal time scale predictability of climate for southern landmasses) will be a very long one. Springer-Verlag 2003.
format Article in Journal/Newspaper
author Marsland, SJ
Latif, M
Legutke, S
author_facet Marsland, SJ
Latif, M
Legutke, S
author_sort Marsland, SJ
title Antarctic circumpolar modes in a coupled ocean-atmosphere model
title_short Antarctic circumpolar modes in a coupled ocean-atmosphere model
title_full Antarctic circumpolar modes in a coupled ocean-atmosphere model
title_fullStr Antarctic circumpolar modes in a coupled ocean-atmosphere model
title_full_unstemmed Antarctic circumpolar modes in a coupled ocean-atmosphere model
title_sort antarctic circumpolar modes in a coupled ocean-atmosphere model
publisher Springer Heidelberg
publishDate 2003
url https://doi.org/10.1007/s10236-003-0041-z
http://ecite.utas.edu.au/35567
geographic Antarctic
Southern Ocean
geographic_facet Antarctic
Southern Ocean
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
op_relation http://dx.doi.org/10.1007/s10236-003-0041-z
Marsland, SJ and Latif, M and Legutke, S, Antarctic circumpolar modes in a coupled ocean-atmosphere model, Ocean Dynamics, 53, (4) pp. 323-331. ISSN 1616-7341 (2003) [Refereed Article]
http://ecite.utas.edu.au/35567
op_doi https://doi.org/10.1007/s10236-003-0041-z
container_title Ocean Dynamics
container_volume 53
container_issue 4
container_start_page 323
op_container_end_page 331
_version_ 1766274788559421440