Accuracy assessment of ocean tide models around Antarctica

Accurate ocean fide models for the circum-Antarctic seas are required to remove unwanted signals from floating ice elevation and space-borne, time-variable gravity measurements (e.g., GRACE). We present accuracy assessments for several global (CSR4, FES2004, FES99, GOT00.2, NAO.99b, TPXO6.2) and Ant...

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Published in:Geophysical Research Letters
Main Authors: King, MA, Padman, L
Format: Article in Journal/Newspaper
Language:English
Published: x 2005
Subjects:
Online Access:https://doi.org/10.1029/2005GL023901
http://ecite.utas.edu.au/81815
id ftunivtasecite:oai:ecite.utas.edu.au:81815
record_format openpolar
spelling ftunivtasecite:oai:ecite.utas.edu.au:81815 2023-05-15T14:02:31+02:00 Accuracy assessment of ocean tide models around Antarctica King, MA Padman, L 2005 https://doi.org/10.1029/2005GL023901 http://ecite.utas.edu.au/81815 en eng x http://dx.doi.org/10.1029/2005GL023901 King, MA and Padman, L, Accuracy assessment of ocean tide models around Antarctica, Geophysical Research Letters, 32, (23) pp. 1-4. ISSN 0094-8276 (2005) [Refereed Article] http://ecite.utas.edu.au/81815 Earth Sciences Physical Geography and Environmental Geoscience Physical Geography and Environmental Geoscience not elsewhere classified Refereed Article PeerReviewed 2005 ftunivtasecite https://doi.org/10.1029/2005GL023901 2019-12-13T21:46:50Z Accurate ocean fide models for the circum-Antarctic seas are required to remove unwanted signals from floating ice elevation and space-borne, time-variable gravity measurements (e.g., GRACE). We present accuracy assessments for several global (CSR4, FES2004, FES99, GOT00.2, NAO.99b, TPXO6.2) and Antarctic (CADA00.10 and CATS02.01) ocean tide models using coastal and pelagic tide gauges, gravimetric data and GPS records of ice shelf surface elevation. The accuracies of CSR4 and NAO.99b are poor in the ice shelf regions. The optimum model for the entire circum-Antarctic seas is TPXO6.2, with a root-mean-square deviation of 5-7 cm, 40% lower than the next best model, FES2004. The main exception is the Filchner-Ronne Ice Shelf where CADA00.10 and CATS02.01 most accurately represent observations from two sites near the Rutford Ice Stream grounding line. Copyright 2005 by the American Geophysical Union. Article in Journal/Newspaper Antarc* Antarctic Antarctica Filchner Ronne Ice Shelf Filchner-Ronne Ice Shelf Ice Shelf Ronne Ice Shelf Rutford Ice Stream eCite UTAS (University of Tasmania) Antarctic Ronne Ice Shelf ENVELOPE(-61.000,-61.000,-78.500,-78.500) Rutford ENVELOPE(-85.300,-85.300,-78.600,-78.600) Rutford Ice Stream ENVELOPE(-80.000,-80.000,-79.167,-79.167) Geophysical Research Letters 32 23
institution Open Polar
collection eCite UTAS (University of Tasmania)
op_collection_id ftunivtasecite
language English
topic Earth Sciences
Physical Geography and Environmental Geoscience
Physical Geography and Environmental Geoscience not elsewhere classified
spellingShingle Earth Sciences
Physical Geography and Environmental Geoscience
Physical Geography and Environmental Geoscience not elsewhere classified
King, MA
Padman, L
Accuracy assessment of ocean tide models around Antarctica
topic_facet Earth Sciences
Physical Geography and Environmental Geoscience
Physical Geography and Environmental Geoscience not elsewhere classified
description Accurate ocean fide models for the circum-Antarctic seas are required to remove unwanted signals from floating ice elevation and space-borne, time-variable gravity measurements (e.g., GRACE). We present accuracy assessments for several global (CSR4, FES2004, FES99, GOT00.2, NAO.99b, TPXO6.2) and Antarctic (CADA00.10 and CATS02.01) ocean tide models using coastal and pelagic tide gauges, gravimetric data and GPS records of ice shelf surface elevation. The accuracies of CSR4 and NAO.99b are poor in the ice shelf regions. The optimum model for the entire circum-Antarctic seas is TPXO6.2, with a root-mean-square deviation of 5-7 cm, 40% lower than the next best model, FES2004. The main exception is the Filchner-Ronne Ice Shelf where CADA00.10 and CATS02.01 most accurately represent observations from two sites near the Rutford Ice Stream grounding line. Copyright 2005 by the American Geophysical Union.
format Article in Journal/Newspaper
author King, MA
Padman, L
author_facet King, MA
Padman, L
author_sort King, MA
title Accuracy assessment of ocean tide models around Antarctica
title_short Accuracy assessment of ocean tide models around Antarctica
title_full Accuracy assessment of ocean tide models around Antarctica
title_fullStr Accuracy assessment of ocean tide models around Antarctica
title_full_unstemmed Accuracy assessment of ocean tide models around Antarctica
title_sort accuracy assessment of ocean tide models around antarctica
publisher x
publishDate 2005
url https://doi.org/10.1029/2005GL023901
http://ecite.utas.edu.au/81815
long_lat ENVELOPE(-61.000,-61.000,-78.500,-78.500)
ENVELOPE(-85.300,-85.300,-78.600,-78.600)
ENVELOPE(-80.000,-80.000,-79.167,-79.167)
geographic Antarctic
Ronne Ice Shelf
Rutford
Rutford Ice Stream
geographic_facet Antarctic
Ronne Ice Shelf
Rutford
Rutford Ice Stream
genre Antarc*
Antarctic
Antarctica
Filchner Ronne Ice Shelf
Filchner-Ronne Ice Shelf
Ice Shelf
Ronne Ice Shelf
Rutford Ice Stream
genre_facet Antarc*
Antarctic
Antarctica
Filchner Ronne Ice Shelf
Filchner-Ronne Ice Shelf
Ice Shelf
Ronne Ice Shelf
Rutford Ice Stream
op_relation http://dx.doi.org/10.1029/2005GL023901
King, MA and Padman, L, Accuracy assessment of ocean tide models around Antarctica, Geophysical Research Letters, 32, (23) pp. 1-4. ISSN 0094-8276 (2005) [Refereed Article]
http://ecite.utas.edu.au/81815
op_doi https://doi.org/10.1029/2005GL023901
container_title Geophysical Research Letters
container_volume 32
container_issue 23
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