The DTU21 global mean sea surface and first evaluation

A new mean sea surface (MSS) from the Technical University of Denmark (DTU) called DTU21MSS for referencing sea-level anomalies from satellite altimetry is introduced in this paper, and a suite of evaluations are performed. One of the reasons for updating the existing mean sea surface is the fact th...

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Published in:Earth System Science Data
Main Authors: Andersen, Ole Baltazar, Rose, Stine Kildegaard, Abulaitijiang, Adili, Zhang, Shengjun, Fleury, Sara
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/essd-15-4065-2023
https://essd.copernicus.org/articles/15/4065/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:essd111143 2023-10-09T21:49:15+02:00 The DTU21 global mean sea surface and first evaluation Andersen, Ole Baltazar Rose, Stine Kildegaard Abulaitijiang, Adili Zhang, Shengjun Fleury, Sara 2023-09-13 application/pdf https://doi.org/10.5194/essd-15-4065-2023 https://essd.copernicus.org/articles/15/4065/2023/ eng eng doi:10.5194/essd-15-4065-2023 https://essd.copernicus.org/articles/15/4065/2023/ eISSN: 1866-3516 Text 2023 ftcopernicus https://doi.org/10.5194/essd-15-4065-2023 2023-09-18T16:24:16Z A new mean sea surface (MSS) from the Technical University of Denmark (DTU) called DTU21MSS for referencing sea-level anomalies from satellite altimetry is introduced in this paper, and a suite of evaluations are performed. One of the reasons for updating the existing mean sea surface is the fact that during the last 6 years, nearly 3 times as many data have been made available by space agencies, resulting in more than 15 years of altimetry from long-repeat orbits (LROs) or geodetic missions. This includes the two interleaved long-repeat cycles of Jason-2 with a systematic cross-track distance as low as 4 km. A new processing chain with updated filtering and editing has been implemented for the DTU21MSS. This way, the DTU21MSS has been computed from 2 Hz altimetry in contrast to the former DTU15MSS and DTU18MSS which were computed from 1 Hz altimetry. The new DTU21MSS is computed over the same 20-year averaging time from 1 January 1993 to 31 December 2012 with a well-specified central time of 1 January 2003 and is available from https://doi.org/10.11583/DTU.19383221.v1 (Andersen, 2022). Cryosat-2 employs synthetic aperture radar (SAR) and SAR interferometric (SARin) modes in a large part of the Arctic Ocean due to the presence of sea ice. For SAR- and SARin-mode data we applied the SAMOSA + physical retracking to make it compatible with the physical retracker used for conventional low-resolution-mode data in other parts of the ocean. Text Arctic Arctic Ocean Sea ice Copernicus Publications: E-Journals Arctic Arctic Ocean Earth System Science Data 15 9 4065 4075
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description A new mean sea surface (MSS) from the Technical University of Denmark (DTU) called DTU21MSS for referencing sea-level anomalies from satellite altimetry is introduced in this paper, and a suite of evaluations are performed. One of the reasons for updating the existing mean sea surface is the fact that during the last 6 years, nearly 3 times as many data have been made available by space agencies, resulting in more than 15 years of altimetry from long-repeat orbits (LROs) or geodetic missions. This includes the two interleaved long-repeat cycles of Jason-2 with a systematic cross-track distance as low as 4 km. A new processing chain with updated filtering and editing has been implemented for the DTU21MSS. This way, the DTU21MSS has been computed from 2 Hz altimetry in contrast to the former DTU15MSS and DTU18MSS which were computed from 1 Hz altimetry. The new DTU21MSS is computed over the same 20-year averaging time from 1 January 1993 to 31 December 2012 with a well-specified central time of 1 January 2003 and is available from https://doi.org/10.11583/DTU.19383221.v1 (Andersen, 2022). Cryosat-2 employs synthetic aperture radar (SAR) and SAR interferometric (SARin) modes in a large part of the Arctic Ocean due to the presence of sea ice. For SAR- and SARin-mode data we applied the SAMOSA + physical retracking to make it compatible with the physical retracker used for conventional low-resolution-mode data in other parts of the ocean.
format Text
author Andersen, Ole Baltazar
Rose, Stine Kildegaard
Abulaitijiang, Adili
Zhang, Shengjun
Fleury, Sara
spellingShingle Andersen, Ole Baltazar
Rose, Stine Kildegaard
Abulaitijiang, Adili
Zhang, Shengjun
Fleury, Sara
The DTU21 global mean sea surface and first evaluation
author_facet Andersen, Ole Baltazar
Rose, Stine Kildegaard
Abulaitijiang, Adili
Zhang, Shengjun
Fleury, Sara
author_sort Andersen, Ole Baltazar
title The DTU21 global mean sea surface and first evaluation
title_short The DTU21 global mean sea surface and first evaluation
title_full The DTU21 global mean sea surface and first evaluation
title_fullStr The DTU21 global mean sea surface and first evaluation
title_full_unstemmed The DTU21 global mean sea surface and first evaluation
title_sort dtu21 global mean sea surface and first evaluation
publishDate 2023
url https://doi.org/10.5194/essd-15-4065-2023
https://essd.copernicus.org/articles/15/4065/2023/
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
op_source eISSN: 1866-3516
op_relation doi:10.5194/essd-15-4065-2023
https://essd.copernicus.org/articles/15/4065/2023/
op_doi https://doi.org/10.5194/essd-15-4065-2023
container_title Earth System Science Data
container_volume 15
container_issue 9
container_start_page 4065
op_container_end_page 4075
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