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 so-called Antarctic Circumpolar Wave (ACW). It is found...

Full description

Bibliographic Details
Published in:Ocean Dynamics
Main Authors: Marsland, S., Latif, Mojib, Legutke, S.
Format: Article in Journal/Newspaper
Language:English
Published: Springer 2003
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/2075/
https://oceanrep.geomar.de/id/eprint/2075/1/fulltext.pdf
https://doi.org/10.1007/s10236-003-0041-z
_version_ 1821683385934807040
author Marsland, S.
Latif, Mojib
Legutke, S.
author_facet Marsland, S.
Latif, Mojib
Legutke, S.
author_sort Marsland, S.
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
container_issue 4
container_start_page 323
container_title Ocean Dynamics
container_volume 53
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 so-called 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 low-frequency 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.
format Article in Journal/Newspaper
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
geographic Antarctic
Southern Ocean
geographic_facet Antarctic
Southern Ocean
id ftoceanrep:oai:oceanrep.geomar.de:2075
institution Open Polar
language English
op_collection_id ftoceanrep
op_container_end_page 331
op_doi https://doi.org/10.1007/s10236-003-0041-z
op_relation https://oceanrep.geomar.de/id/eprint/2075/1/fulltext.pdf
Marsland, S., Latif, M. and Legutke, S. (2003) Antarctic Circumpolar Modes in a Coupled Ocean-Atmosphere Model. Ocean Dynamics, 53 (4). pp. 323-333. DOI 10.1007/s10236-003-0041-z <https://doi.org/10.1007/s10236-003-0041-z>.
doi:10.1007/s10236-003-0041-z
op_rights info:eu-repo/semantics/restrictedAccess
publishDate 2003
publisher Springer
record_format openpolar
spelling ftoceanrep:oai:oceanrep.geomar.de:2075 2025-01-16T19:14:22+00:00 Antarctic Circumpolar Modes in a Coupled Ocean-Atmosphere Model Marsland, S. Latif, Mojib Legutke, S. 2003 text https://oceanrep.geomar.de/id/eprint/2075/ https://oceanrep.geomar.de/id/eprint/2075/1/fulltext.pdf https://doi.org/10.1007/s10236-003-0041-z en eng Springer https://oceanrep.geomar.de/id/eprint/2075/1/fulltext.pdf Marsland, S., Latif, M. and Legutke, S. (2003) Antarctic Circumpolar Modes in a Coupled Ocean-Atmosphere Model. Ocean Dynamics, 53 (4). pp. 323-333. DOI 10.1007/s10236-003-0041-z <https://doi.org/10.1007/s10236-003-0041-z>. doi:10.1007/s10236-003-0041-z info:eu-repo/semantics/restrictedAccess Article PeerReviewed 2003 ftoceanrep https://doi.org/10.1007/s10236-003-0041-z 2024-09-04T05:04:40Z 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 so-called 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 low-frequency 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. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Antarctic Southern Ocean Ocean Dynamics 53 4 323 331
spellingShingle Marsland, S.
Latif, Mojib
Legutke, S.
Antarctic Circumpolar Modes in a Coupled Ocean-Atmosphere Model
title 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_short Antarctic Circumpolar Modes in a Coupled Ocean-Atmosphere Model
title_sort antarctic circumpolar modes in a coupled ocean-atmosphere model
url https://oceanrep.geomar.de/id/eprint/2075/
https://oceanrep.geomar.de/id/eprint/2075/1/fulltext.pdf
https://doi.org/10.1007/s10236-003-0041-z