Temporal Variations of the Marine Geoid
The effects of temporal changes in the marine geoid on estimates of the ocean dynamic topography are being investigated. Influences from mass redistribution due to changes of land hydrology, ice sheets, glacial isostatic adjustment (GIA), and ocean and atmospheric dynamics are considered, and the as...
Published in: | Journal of Geophysical Research: Oceans |
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ftsubggeo:oai:e-docs.geo-leo.de:11858/8375 2024-06-09T07:39:26+00:00 Temporal Variations of the Marine Geoid Siegismund, F. Köhl, A. Rummel, R. Stammer, D. 1 Institute of Oceanography, Center for Earth System Research and Sustainability University of Hamburg Hamburg Germany 2 Institute for Astronomical and Physical Geodesy Technical University of Munich Munich Germany 2020-11-08 https://doi.org/10.23689/fidgeo-4035 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/8375 eng eng doi:10.23689/fidgeo-4035 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/8375 This is an open access article under the terms of the Creative Commons Attribution‐NonCommercial‐NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made. ddc:550.312 ddc:551.46 geoid height altimetry ocean dynamic topography temporal variability trend doc-type:article 2020 ftsubggeo https://doi.org/10.23689/fidgeo-4035 2024-05-10T04:58:51Z The effects of temporal changes in the marine geoid on estimates of the ocean dynamic topography are being investigated. Influences from mass redistribution due to changes of land hydrology, ice sheets, glacial isostatic adjustment (GIA), and ocean and atmospheric dynamics are considered, and the associated crustal deformation is included. The strongest signals are associated with the seasonal cycle caused by changes in terrestrial water storage and ice sheets as well as the redistribution of atmospheric mass. Second to this is the importance of an overall trend caused by GIA and decreasing ice sheets over Greenland and Antarctica. On long spatial scales, the amplitude of regional trends estimated for the geoid height has a sizable fraction of those from sea level anomaly (SLA) for the period 1993–2016, also after subtraction of steric height of the upper 1,000 m to analyze trends in deep ocean geostrophic currents. The estimated strong negative geoid height trend south of Greenland for the period 1993–2016 opposes changes in dynamic sea level for the same period thereby affecting past studies on changes of both the strength of the subpolar gyre based on SLA and the meridional overturning circulation on a section between Cape Farewell and Portugal applying ocean dynamic topography and hydrography. We conclude that temporal geoid height trends should be considered in studies of (multi)decadal trends in sea level and circulation on large spatial scales based on altimetry data referenced to a geoid field. Plain Language Summary: Changes in ocean surface currents are routinely obtained from satellite altimetry data. A correction for changes in the geoid, the equipotential surface of gravity closest to sea level, is considered small and thus usually neglected. We investigate temporal geoid height changes and potential implications on ocean circulation studies using space‐borne gravity data and results from ocean and atmosphere models to discover the individual processes of mass redistribution in the climate system ... Article in Journal/Newspaper Antarc* Antarctica Cape Farewell Greenland GEO-LEOe-docs (FID GEO) Greenland Journal of Geophysical Research: Oceans 125 11 |
institution |
Open Polar |
collection |
GEO-LEOe-docs (FID GEO) |
op_collection_id |
ftsubggeo |
language |
English |
topic |
ddc:550.312 ddc:551.46 geoid height altimetry ocean dynamic topography temporal variability trend |
spellingShingle |
ddc:550.312 ddc:551.46 geoid height altimetry ocean dynamic topography temporal variability trend Siegismund, F. Köhl, A. Rummel, R. Stammer, D. 1 Institute of Oceanography, Center for Earth System Research and Sustainability University of Hamburg Hamburg Germany 2 Institute for Astronomical and Physical Geodesy Technical University of Munich Munich Germany Temporal Variations of the Marine Geoid |
topic_facet |
ddc:550.312 ddc:551.46 geoid height altimetry ocean dynamic topography temporal variability trend |
description |
The effects of temporal changes in the marine geoid on estimates of the ocean dynamic topography are being investigated. Influences from mass redistribution due to changes of land hydrology, ice sheets, glacial isostatic adjustment (GIA), and ocean and atmospheric dynamics are considered, and the associated crustal deformation is included. The strongest signals are associated with the seasonal cycle caused by changes in terrestrial water storage and ice sheets as well as the redistribution of atmospheric mass. Second to this is the importance of an overall trend caused by GIA and decreasing ice sheets over Greenland and Antarctica. On long spatial scales, the amplitude of regional trends estimated for the geoid height has a sizable fraction of those from sea level anomaly (SLA) for the period 1993–2016, also after subtraction of steric height of the upper 1,000 m to analyze trends in deep ocean geostrophic currents. The estimated strong negative geoid height trend south of Greenland for the period 1993–2016 opposes changes in dynamic sea level for the same period thereby affecting past studies on changes of both the strength of the subpolar gyre based on SLA and the meridional overturning circulation on a section between Cape Farewell and Portugal applying ocean dynamic topography and hydrography. We conclude that temporal geoid height trends should be considered in studies of (multi)decadal trends in sea level and circulation on large spatial scales based on altimetry data referenced to a geoid field. Plain Language Summary: Changes in ocean surface currents are routinely obtained from satellite altimetry data. A correction for changes in the geoid, the equipotential surface of gravity closest to sea level, is considered small and thus usually neglected. We investigate temporal geoid height changes and potential implications on ocean circulation studies using space‐borne gravity data and results from ocean and atmosphere models to discover the individual processes of mass redistribution in the climate system ... |
format |
Article in Journal/Newspaper |
author |
Siegismund, F. Köhl, A. Rummel, R. Stammer, D. 1 Institute of Oceanography, Center for Earth System Research and Sustainability University of Hamburg Hamburg Germany 2 Institute for Astronomical and Physical Geodesy Technical University of Munich Munich Germany |
author_facet |
Siegismund, F. Köhl, A. Rummel, R. Stammer, D. 1 Institute of Oceanography, Center for Earth System Research and Sustainability University of Hamburg Hamburg Germany 2 Institute for Astronomical and Physical Geodesy Technical University of Munich Munich Germany |
author_sort |
Siegismund, F. |
title |
Temporal Variations of the Marine Geoid |
title_short |
Temporal Variations of the Marine Geoid |
title_full |
Temporal Variations of the Marine Geoid |
title_fullStr |
Temporal Variations of the Marine Geoid |
title_full_unstemmed |
Temporal Variations of the Marine Geoid |
title_sort |
temporal variations of the marine geoid |
publishDate |
2020 |
url |
https://doi.org/10.23689/fidgeo-4035 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/8375 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Antarc* Antarctica Cape Farewell Greenland |
genre_facet |
Antarc* Antarctica Cape Farewell Greenland |
op_relation |
doi:10.23689/fidgeo-4035 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/8375 |
op_rights |
This is an open access article under the terms of the Creative Commons Attribution‐NonCommercial‐NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made. |
op_doi |
https://doi.org/10.23689/fidgeo-4035 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
125 |
container_issue |
11 |
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1801379488616939520 |