Polar ocean tides revisited ...

<!--!introduction!--> Polar oceans have generally been harder to determine from satellite altimetry because the regions outside the 66 parallel has traditionally only been surveyed satellites in sun-sun-synchronous orbits. With Cryosat-2 this has changed. However, the satellite poses a number...

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Main Authors: Andersen, Ole, Rose, Stine Kildegaard
Format: Conference Object
Language:unknown
Published: GFZ German Research Centre for Geosciences 2023
Subjects:
Online Access:https://dx.doi.org/10.57757/iugg23-2136
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018651
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spelling ftdatacite:10.57757/iugg23-2136 2023-07-23T04:15:43+02:00 Polar ocean tides revisited ... Andersen, Ole Rose, Stine Kildegaard 2023 https://dx.doi.org/10.57757/iugg23-2136 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018651 unknown GFZ German Research Centre for Geosciences Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Article ConferencePaper Oral 2023 ftdatacite https://doi.org/10.57757/iugg23-2136 2023-07-03T18:35:08Z <!--!introduction!--> Polar oceans have generally been harder to determine from satellite altimetry because the regions outside the 66 parallel has traditionally only been surveyed satellites in sun-sun-synchronous orbits. With Cryosat-2 this has changed. However, the satellite poses a number of challenges to tidal analysis because of its long ground-track repeat period (368 days) and its diverse measurement modes, low-rate mode (LRM) over the ocean and synthetic aperture radar interferometric mode (SARin) over ice surfaces and parts of the ocean. The SAMOSA+ physical retracker was developed to process the Cryosat-2 data across measurement modes and hereby enables the determination of the sea state bias. This way it provides more stable sea level estimates compared with traditional empirical retrackers used in the Polar Ocean. Nearly 10 years of Cryosat-2 data have been analyzed for residual ocean tides to the FES2014 ocean tide model in the Arctic Ocean and Antarctic Ocean using the response ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... Conference Object Antarc* Antarctic Antarctic Ocean Arctic Arctic Ocean DataCite Metadata Store (German National Library of Science and Technology) Arctic Antarctic Arctic Ocean Antarctic Ocean
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description <!--!introduction!--> Polar oceans have generally been harder to determine from satellite altimetry because the regions outside the 66 parallel has traditionally only been surveyed satellites in sun-sun-synchronous orbits. With Cryosat-2 this has changed. However, the satellite poses a number of challenges to tidal analysis because of its long ground-track repeat period (368 days) and its diverse measurement modes, low-rate mode (LRM) over the ocean and synthetic aperture radar interferometric mode (SARin) over ice surfaces and parts of the ocean. The SAMOSA+ physical retracker was developed to process the Cryosat-2 data across measurement modes and hereby enables the determination of the sea state bias. This way it provides more stable sea level estimates compared with traditional empirical retrackers used in the Polar Ocean. Nearly 10 years of Cryosat-2 data have been analyzed for residual ocean tides to the FES2014 ocean tide model in the Arctic Ocean and Antarctic Ocean using the response ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ...
format Conference Object
author Andersen, Ole
Rose, Stine Kildegaard
spellingShingle Andersen, Ole
Rose, Stine Kildegaard
Polar ocean tides revisited ...
author_facet Andersen, Ole
Rose, Stine Kildegaard
author_sort Andersen, Ole
title Polar ocean tides revisited ...
title_short Polar ocean tides revisited ...
title_full Polar ocean tides revisited ...
title_fullStr Polar ocean tides revisited ...
title_full_unstemmed Polar ocean tides revisited ...
title_sort polar ocean tides revisited ...
publisher GFZ German Research Centre for Geosciences
publishDate 2023
url https://dx.doi.org/10.57757/iugg23-2136
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018651
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Arctic Ocean
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Antarctic Ocean
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Arctic Ocean
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op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.57757/iugg23-2136
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