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...
Published in: | Ocean Dynamics |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Springer
2003
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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 |
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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 |