Polar Ocean Tides—Revisited Using Cryosat-2

With the availability of more than 9 years of Cryosat-2, it is possible to revisit polar ocean tides, which have traditionally been difficult to determine from satellite altimetry. The SAMOSA+ physical retracker is a stable retracker developed particularly for Cryosat-2. Being a physical retracker,...

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Published in:Remote Sensing
Main Authors: Andersen, Ole Baltazar, Rose, Stine Kildegaard, Hart-Davis, Michael G.
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:https://orbit.dtu.dk/en/publications/885f7d64-c3ab-4b97-bdc6-2161f0b44cac
https://doi.org/10.3390/rs15184479
https://backend.orbit.dtu.dk/ws/files/338179903/remotesensing-15-04479-v2.pdf
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spelling ftdtupubl:oai:pure.atira.dk:publications/885f7d64-c3ab-4b97-bdc6-2161f0b44cac 2024-09-15T17:44:39+00:00 Polar Ocean Tides—Revisited Using Cryosat-2 Andersen, Ole Baltazar Rose, Stine Kildegaard Hart-Davis, Michael G. 2023 application/pdf https://orbit.dtu.dk/en/publications/885f7d64-c3ab-4b97-bdc6-2161f0b44cac https://doi.org/10.3390/rs15184479 https://backend.orbit.dtu.dk/ws/files/338179903/remotesensing-15-04479-v2.pdf eng eng https://orbit.dtu.dk/en/publications/885f7d64-c3ab-4b97-bdc6-2161f0b44cac info:eu-repo/semantics/openAccess Andersen , O B , Rose , S K & Hart-Davis , M G 2023 , ' Polar Ocean Tides—Revisited Using Cryosat-2 ' , Remote Sensing , vol. 15 , no. 18 , 4479 . https://doi.org/10.3390/rs15184479 Ocean tides Polar oceans Satellite altimetry article 2023 ftdtupubl https://doi.org/10.3390/rs15184479 2024-08-13T00:03:07Z With the availability of more than 9 years of Cryosat-2, it is possible to revisit polar ocean tides, which have traditionally been difficult to determine from satellite altimetry. The SAMOSA+ physical retracker is a stable retracker developed particularly for Cryosat-2. Being a physical retracker, it enables the determination of the sea state bias. Correcting for the sea state bias enables more reliable sea level estimates compared with traditional empirical retrackers used before. 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 formalism. We utilize data from the sub-cycle of Cryosat-2, which follows a repeating pattern of approximately 28.33 days. This sub-repeat period makes it an advantageous alias period for the majority of significant constituents. This allowed for the estimation and mapping of the major tidal constituents in the open ocean and also in floating ice shelves from data extracted from leads in the sea ice. A novel empirical ocean tide model designed specifically for the polar region, DTU22, is introduced. Our findings reveal substantial enhancements in semi-diurnal tides within the Arctic Ocean and improvement in diurnal constituents within the Southern Ocean. In the Southern Ocean, the diurnal constituents are particularly improved using the empirical model by more than a factor of two to around 3 cm for both constituents compared with FES2014b. These outcomes underscore the significance of incorporating the reprocessed and retracted Cryosat-2 data into tidal modeling, highlighting its pivotal role in advancing the field. Article in Journal/Newspaper Antarc* Antarctic Antarctic Ocean Arctic Ocean Ice Shelves Sea ice Southern Ocean Technical University of Denmark: DTU Orbit Remote Sensing 15 18 4479
institution Open Polar
collection Technical University of Denmark: DTU Orbit
op_collection_id ftdtupubl
language English
topic Ocean tides
Polar oceans
Satellite altimetry
spellingShingle Ocean tides
Polar oceans
Satellite altimetry
Andersen, Ole Baltazar
Rose, Stine Kildegaard
Hart-Davis, Michael G.
Polar Ocean Tides—Revisited Using Cryosat-2
topic_facet Ocean tides
Polar oceans
Satellite altimetry
description With the availability of more than 9 years of Cryosat-2, it is possible to revisit polar ocean tides, which have traditionally been difficult to determine from satellite altimetry. The SAMOSA+ physical retracker is a stable retracker developed particularly for Cryosat-2. Being a physical retracker, it enables the determination of the sea state bias. Correcting for the sea state bias enables more reliable sea level estimates compared with traditional empirical retrackers used before. 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 formalism. We utilize data from the sub-cycle of Cryosat-2, which follows a repeating pattern of approximately 28.33 days. This sub-repeat period makes it an advantageous alias period for the majority of significant constituents. This allowed for the estimation and mapping of the major tidal constituents in the open ocean and also in floating ice shelves from data extracted from leads in the sea ice. A novel empirical ocean tide model designed specifically for the polar region, DTU22, is introduced. Our findings reveal substantial enhancements in semi-diurnal tides within the Arctic Ocean and improvement in diurnal constituents within the Southern Ocean. In the Southern Ocean, the diurnal constituents are particularly improved using the empirical model by more than a factor of two to around 3 cm for both constituents compared with FES2014b. These outcomes underscore the significance of incorporating the reprocessed and retracted Cryosat-2 data into tidal modeling, highlighting its pivotal role in advancing the field.
format Article in Journal/Newspaper
author Andersen, Ole Baltazar
Rose, Stine Kildegaard
Hart-Davis, Michael G.
author_facet Andersen, Ole Baltazar
Rose, Stine Kildegaard
Hart-Davis, Michael G.
author_sort Andersen, Ole Baltazar
title Polar Ocean Tides—Revisited Using Cryosat-2
title_short Polar Ocean Tides—Revisited Using Cryosat-2
title_full Polar Ocean Tides—Revisited Using Cryosat-2
title_fullStr Polar Ocean Tides—Revisited Using Cryosat-2
title_full_unstemmed Polar Ocean Tides—Revisited Using Cryosat-2
title_sort polar ocean tides—revisited using cryosat-2
publishDate 2023
url https://orbit.dtu.dk/en/publications/885f7d64-c3ab-4b97-bdc6-2161f0b44cac
https://doi.org/10.3390/rs15184479
https://backend.orbit.dtu.dk/ws/files/338179903/remotesensing-15-04479-v2.pdf
genre Antarc*
Antarctic
Antarctic Ocean
Arctic Ocean
Ice Shelves
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Antarctic Ocean
Arctic Ocean
Ice Shelves
Sea ice
Southern Ocean
op_source Andersen , O B , Rose , S K & Hart-Davis , M G 2023 , ' Polar Ocean Tides—Revisited Using Cryosat-2 ' , Remote Sensing , vol. 15 , no. 18 , 4479 . https://doi.org/10.3390/rs15184479
op_relation https://orbit.dtu.dk/en/publications/885f7d64-c3ab-4b97-bdc6-2161f0b44cac
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.3390/rs15184479
container_title Remote Sensing
container_volume 15
container_issue 18
container_start_page 4479
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