Deliverable 6.20 Observing systems for sea level in the Arctic

The Arctic Ocean is at the frontier of the fast-changing climate in the northern latitudes and sea level trends is a bulk measure of ongoing processes related climate change. Observations of sea level in the Arctic Ocean are nonetheless difficult to validate with independent measurements and is glob...

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Main Authors: Ludwigsen, Carsten Bjerre, Andersen, Ole Baltazar
Format: Report
Language:English
Published: 2021
Subjects:
Online Access:https://zenodo.org/record/7180352
https://doi.org/10.5281/zenodo.7180352
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record_format openpolar
spelling ftzenodo:oai:zenodo.org:7180352 2023-05-15T14:33:14+02:00 Deliverable 6.20 Observing systems for sea level in the Arctic Ludwigsen, Carsten Bjerre Andersen, Ole Baltazar 2021-11-15 https://zenodo.org/record/7180352 https://doi.org/10.5281/zenodo.7180352 eng eng info:eu-repo/grantAgreement/EC/H2020/727890/ doi:10.5281/zenodo.7180351 https://zenodo.org/communities/intaros-h2020 https://zenodo.org/record/7180352 https://doi.org/10.5281/zenodo.7180352 oai:zenodo.org:7180352 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode Arctic INTAROS Ocean Observing Systems Sea Level Satellite Altimetry In Situ Data info:eu-repo/semantics/report publication-deliverable 2021 ftzenodo https://doi.org/10.5281/zenodo.718035210.5281/zenodo.7180351 2023-03-10T22:10:27Z The Arctic Ocean is at the frontier of the fast-changing climate in the northern latitudes and sea level trends is a bulk measure of ongoing processes related climate change. Observations of sea level in the Arctic Ocean are nonetheless difficult to validate with independent measurements and is globally the region where the sea level change is most uncertain. By using specialized methods for observing sea level with satellite altimetry over sea ice regions in the Arctic, we are able to construct an altimetric sea level record that is in good agreement with the sea level observed by tide gauges. However, long-term changes of tide-gauges are influenced by vertical land motion (VLM) caused by past and present changes of ice. A novel model of the elastic rebound from present changes of Arctic ice has been applied to create a VLM-model that agrees well with GNSS. Sea level change from altimetry and VLM-corrected tide gauges are compared to a reconstructed sea level estimate, derived from the sea level fingerprints of present-day mass changes and steric sea level change derived from available arctic T/S-profiles. The comparison shows that the freshwater change is dominating the Arctic sea level change. Several recommendations have been outlined, to improve future analysis and observations of Arctic Ocean sea level. The most important is the lack of in-situ data in several regions of the Arctic Ocean that are necessary to validate the observations from remote sensing. Report Arctic Arctic Ocean Climate change Sea ice Zenodo Arctic Arctic Ocean
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic Arctic
INTAROS
Ocean Observing Systems
Sea Level
Satellite Altimetry
In Situ Data
spellingShingle Arctic
INTAROS
Ocean Observing Systems
Sea Level
Satellite Altimetry
In Situ Data
Ludwigsen, Carsten Bjerre
Andersen, Ole Baltazar
Deliverable 6.20 Observing systems for sea level in the Arctic
topic_facet Arctic
INTAROS
Ocean Observing Systems
Sea Level
Satellite Altimetry
In Situ Data
description The Arctic Ocean is at the frontier of the fast-changing climate in the northern latitudes and sea level trends is a bulk measure of ongoing processes related climate change. Observations of sea level in the Arctic Ocean are nonetheless difficult to validate with independent measurements and is globally the region where the sea level change is most uncertain. By using specialized methods for observing sea level with satellite altimetry over sea ice regions in the Arctic, we are able to construct an altimetric sea level record that is in good agreement with the sea level observed by tide gauges. However, long-term changes of tide-gauges are influenced by vertical land motion (VLM) caused by past and present changes of ice. A novel model of the elastic rebound from present changes of Arctic ice has been applied to create a VLM-model that agrees well with GNSS. Sea level change from altimetry and VLM-corrected tide gauges are compared to a reconstructed sea level estimate, derived from the sea level fingerprints of present-day mass changes and steric sea level change derived from available arctic T/S-profiles. The comparison shows that the freshwater change is dominating the Arctic sea level change. Several recommendations have been outlined, to improve future analysis and observations of Arctic Ocean sea level. The most important is the lack of in-situ data in several regions of the Arctic Ocean that are necessary to validate the observations from remote sensing.
format Report
author Ludwigsen, Carsten Bjerre
Andersen, Ole Baltazar
author_facet Ludwigsen, Carsten Bjerre
Andersen, Ole Baltazar
author_sort Ludwigsen, Carsten Bjerre
title Deliverable 6.20 Observing systems for sea level in the Arctic
title_short Deliverable 6.20 Observing systems for sea level in the Arctic
title_full Deliverable 6.20 Observing systems for sea level in the Arctic
title_fullStr Deliverable 6.20 Observing systems for sea level in the Arctic
title_full_unstemmed Deliverable 6.20 Observing systems for sea level in the Arctic
title_sort deliverable 6.20 observing systems for sea level in the arctic
publishDate 2021
url https://zenodo.org/record/7180352
https://doi.org/10.5281/zenodo.7180352
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Climate change
Sea ice
genre_facet Arctic
Arctic Ocean
Climate change
Sea ice
op_relation info:eu-repo/grantAgreement/EC/H2020/727890/
doi:10.5281/zenodo.7180351
https://zenodo.org/communities/intaros-h2020
https://zenodo.org/record/7180352
https://doi.org/10.5281/zenodo.7180352
oai:zenodo.org:7180352
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.718035210.5281/zenodo.7180351
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