Arctic Sea Level Budget Assessment during the GRACE/Argo Time Period
Sea level change is an important indicator of climate change. Our study focuses on the sea level budget assessment of the Arctic Ocean using: (1) the newly reprocessed satellite altimeter data with major changes in the processing techniques; (2) ocean mass change data derived from GRACE satellite gr...
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ftmdpi:oai:mdpi.com:/2072-4292/12/17/2837/ 2023-08-20T04:03:28+02:00 Arctic Sea Level Budget Assessment during the GRACE/Argo Time Period Roshin Raj Ole Andersen Johnny Johannessen Benjamin Gutknecht Sourav Chatterjee Stine Rose Antonio Bonaduce Martin Horwath Heidi Ranndal Kristin Richter Hindumathi Palanisamy Carsten Ludwigsen Laurent Bertino J. Ø. Nilsen Per Knudsen Anna Hogg Anny Cazenave Jérôme Benveniste agris 2020-09-01 application/pdf https://doi.org/10.3390/rs12172837 EN eng Multidisciplinary Digital Publishing Institute Environmental Remote Sensing https://dx.doi.org/10.3390/rs12172837 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 12; Issue 17; Pages: 2837 sea level satellite altimetry GRACE ocean mass change steric height Arctic Oscillation Arctic dipole Cryosat-2 Nordic Seas Beaufort Gyre Text 2020 ftmdpi https://doi.org/10.3390/rs12172837 2023-08-01T00:01:26Z Sea level change is an important indicator of climate change. Our study focuses on the sea level budget assessment of the Arctic Ocean using: (1) the newly reprocessed satellite altimeter data with major changes in the processing techniques; (2) ocean mass change data derived from GRACE satellite gravimetry; (3) and steric height estimated from gridded hydrographic data for the GRACE/Argo time period (2003–2016). The Beaufort Gyre (BG) and the Nordic Seas (NS) regions exhibit the largest positive trend in sea level during the study period. Halosteric sea level change is found to dominate the area averaged sea level trend of BG, while the trend in NS is found to be influenced by halosteric and ocean mass change effects. Temporal variability of sea level in these two regions reveals a significant shift in the trend pattern centered around 2009–2011. Analysis suggests that this shift can be explained by a change in large-scale atmospheric circulation patterns over the Arctic. The sea level budget assessment of the Arctic found a residual trend of more than 1.0 mm/yr. This nonclosure of the sea level budget is further attributed to the limitations of the three above mentioned datasets in the Arctic region. Text Arctic Arctic Ocean Climate change Nordic Seas MDPI Open Access Publishing Arctic Arctic Ocean Remote Sensing 12 17 2837 |
institution |
Open Polar |
collection |
MDPI Open Access Publishing |
op_collection_id |
ftmdpi |
language |
English |
topic |
sea level satellite altimetry GRACE ocean mass change steric height Arctic Oscillation Arctic dipole Cryosat-2 Nordic Seas Beaufort Gyre |
spellingShingle |
sea level satellite altimetry GRACE ocean mass change steric height Arctic Oscillation Arctic dipole Cryosat-2 Nordic Seas Beaufort Gyre Roshin Raj Ole Andersen Johnny Johannessen Benjamin Gutknecht Sourav Chatterjee Stine Rose Antonio Bonaduce Martin Horwath Heidi Ranndal Kristin Richter Hindumathi Palanisamy Carsten Ludwigsen Laurent Bertino J. Ø. Nilsen Per Knudsen Anna Hogg Anny Cazenave Jérôme Benveniste Arctic Sea Level Budget Assessment during the GRACE/Argo Time Period |
topic_facet |
sea level satellite altimetry GRACE ocean mass change steric height Arctic Oscillation Arctic dipole Cryosat-2 Nordic Seas Beaufort Gyre |
description |
Sea level change is an important indicator of climate change. Our study focuses on the sea level budget assessment of the Arctic Ocean using: (1) the newly reprocessed satellite altimeter data with major changes in the processing techniques; (2) ocean mass change data derived from GRACE satellite gravimetry; (3) and steric height estimated from gridded hydrographic data for the GRACE/Argo time period (2003–2016). The Beaufort Gyre (BG) and the Nordic Seas (NS) regions exhibit the largest positive trend in sea level during the study period. Halosteric sea level change is found to dominate the area averaged sea level trend of BG, while the trend in NS is found to be influenced by halosteric and ocean mass change effects. Temporal variability of sea level in these two regions reveals a significant shift in the trend pattern centered around 2009–2011. Analysis suggests that this shift can be explained by a change in large-scale atmospheric circulation patterns over the Arctic. The sea level budget assessment of the Arctic found a residual trend of more than 1.0 mm/yr. This nonclosure of the sea level budget is further attributed to the limitations of the three above mentioned datasets in the Arctic region. |
format |
Text |
author |
Roshin Raj Ole Andersen Johnny Johannessen Benjamin Gutknecht Sourav Chatterjee Stine Rose Antonio Bonaduce Martin Horwath Heidi Ranndal Kristin Richter Hindumathi Palanisamy Carsten Ludwigsen Laurent Bertino J. Ø. Nilsen Per Knudsen Anna Hogg Anny Cazenave Jérôme Benveniste |
author_facet |
Roshin Raj Ole Andersen Johnny Johannessen Benjamin Gutknecht Sourav Chatterjee Stine Rose Antonio Bonaduce Martin Horwath Heidi Ranndal Kristin Richter Hindumathi Palanisamy Carsten Ludwigsen Laurent Bertino J. Ø. Nilsen Per Knudsen Anna Hogg Anny Cazenave Jérôme Benveniste |
author_sort |
Roshin Raj |
title |
Arctic Sea Level Budget Assessment during the GRACE/Argo Time Period |
title_short |
Arctic Sea Level Budget Assessment during the GRACE/Argo Time Period |
title_full |
Arctic Sea Level Budget Assessment during the GRACE/Argo Time Period |
title_fullStr |
Arctic Sea Level Budget Assessment during the GRACE/Argo Time Period |
title_full_unstemmed |
Arctic Sea Level Budget Assessment during the GRACE/Argo Time Period |
title_sort |
arctic sea level budget assessment during the grace/argo time period |
publisher |
Multidisciplinary Digital Publishing Institute |
publishDate |
2020 |
url |
https://doi.org/10.3390/rs12172837 |
op_coverage |
agris |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Climate change Nordic Seas |
genre_facet |
Arctic Arctic Ocean Climate change Nordic Seas |
op_source |
Remote Sensing; Volume 12; Issue 17; Pages: 2837 |
op_relation |
Environmental Remote Sensing https://dx.doi.org/10.3390/rs12172837 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.3390/rs12172837 |
container_title |
Remote Sensing |
container_volume |
12 |
container_issue |
17 |
container_start_page |
2837 |
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1774713827343990784 |