Rossby Waves in the Southern Ocean: A comparison of TOPEX/POSEIDON altimetry with model predictions

Results are presented from an eddy-resolving model of the Southern Ocean which suggest that regions of moderate eddy activity are occupied by wavelike eddies with wavelengths of about 300 km and periods of 4 to 12 months. These waves travel eastward where the current (and wave amplitude)is strongest...

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Published in:Journal of Geophysical Research
Main Author: Hughes, Christopher
Format: Article in Journal/Newspaper
Language:English
Published: 1995
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/19364/
https://nora.nerc.ac.uk/id/eprint/19364/1/1995-Hughes_JGR_Rossby_TP.pdf
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spelling ftnerc:oai:nora.nerc.ac.uk:19364 2023-05-15T18:24:41+02:00 Rossby Waves in the Southern Ocean: A comparison of TOPEX/POSEIDON altimetry with model predictions Hughes, Christopher 1995-08-15 text http://nora.nerc.ac.uk/id/eprint/19364/ https://nora.nerc.ac.uk/id/eprint/19364/1/1995-Hughes_JGR_Rossby_TP.pdf en eng https://nora.nerc.ac.uk/id/eprint/19364/1/1995-Hughes_JGR_Rossby_TP.pdf Hughes, Christopher orcid:0000-0002-9355-0233 . 1995 Rossby Waves in the Southern Ocean: A comparison of TOPEX/POSEIDON altimetry with model predictions. Journal of Geophysical Research, 100 (C8). 15933-15950. https://doi.org/10.1029/95JC01380 <https://doi.org/10.1029/95JC01380> Marine Sciences Publication - Article PeerReviewed 1995 ftnerc https://doi.org/10.1029/95JC01380 2023-02-04T19:32:17Z Results are presented from an eddy-resolving model of the Southern Ocean which suggest that regions of moderate eddy activity are occupied by wavelike eddies with wavelengths of about 300 km and periods of 4 to 12 months. These waves travel eastward where the current (and wave amplitude)is strongest, and westward elsewhere, and it is argued that they are Rossby waves advected by the mean flow. It is shown that TOPEX/POSEIDON altimetry data should be able to resolve these waves in the Pacific sector of the Southern Ocean. A technique for wave detection is then presented which is capable of extracting useful information about the waves in this as well as other regions. Altimeter data are then presented which confirm the existence of waves in the Pacific sector and are consistent with wave presence elsewhere. An analysis of tide model errors shows that such errors are incapable of producing a signal which could mimic the modeled waves, although tide model errors may explain the difference between altimetry and model results in shallow regions of the ocean and in regions of low eddy activity. Article in Journal/Newspaper Southern Ocean Natural Environment Research Council: NERC Open Research Archive Southern Ocean Pacific Journal of Geophysical Research 100 C8 15933
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language English
topic Marine Sciences
spellingShingle Marine Sciences
Hughes, Christopher
Rossby Waves in the Southern Ocean: A comparison of TOPEX/POSEIDON altimetry with model predictions
topic_facet Marine Sciences
description Results are presented from an eddy-resolving model of the Southern Ocean which suggest that regions of moderate eddy activity are occupied by wavelike eddies with wavelengths of about 300 km and periods of 4 to 12 months. These waves travel eastward where the current (and wave amplitude)is strongest, and westward elsewhere, and it is argued that they are Rossby waves advected by the mean flow. It is shown that TOPEX/POSEIDON altimetry data should be able to resolve these waves in the Pacific sector of the Southern Ocean. A technique for wave detection is then presented which is capable of extracting useful information about the waves in this as well as other regions. Altimeter data are then presented which confirm the existence of waves in the Pacific sector and are consistent with wave presence elsewhere. An analysis of tide model errors shows that such errors are incapable of producing a signal which could mimic the modeled waves, although tide model errors may explain the difference between altimetry and model results in shallow regions of the ocean and in regions of low eddy activity.
format Article in Journal/Newspaper
author Hughes, Christopher
author_facet Hughes, Christopher
author_sort Hughes, Christopher
title Rossby Waves in the Southern Ocean: A comparison of TOPEX/POSEIDON altimetry with model predictions
title_short Rossby Waves in the Southern Ocean: A comparison of TOPEX/POSEIDON altimetry with model predictions
title_full Rossby Waves in the Southern Ocean: A comparison of TOPEX/POSEIDON altimetry with model predictions
title_fullStr Rossby Waves in the Southern Ocean: A comparison of TOPEX/POSEIDON altimetry with model predictions
title_full_unstemmed Rossby Waves in the Southern Ocean: A comparison of TOPEX/POSEIDON altimetry with model predictions
title_sort rossby waves in the southern ocean: a comparison of topex/poseidon altimetry with model predictions
publishDate 1995
url http://nora.nerc.ac.uk/id/eprint/19364/
https://nora.nerc.ac.uk/id/eprint/19364/1/1995-Hughes_JGR_Rossby_TP.pdf
geographic Southern Ocean
Pacific
geographic_facet Southern Ocean
Pacific
genre Southern Ocean
genre_facet Southern Ocean
op_relation https://nora.nerc.ac.uk/id/eprint/19364/1/1995-Hughes_JGR_Rossby_TP.pdf
Hughes, Christopher orcid:0000-0002-9355-0233 . 1995 Rossby Waves in the Southern Ocean: A comparison of TOPEX/POSEIDON altimetry with model predictions. Journal of Geophysical Research, 100 (C8). 15933-15950. https://doi.org/10.1029/95JC01380 <https://doi.org/10.1029/95JC01380>
op_doi https://doi.org/10.1029/95JC01380
container_title Journal of Geophysical Research
container_volume 100
container_issue C8
container_start_page 15933
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