Seasonal variation of the M2 tide
The seasonal cycle of the main lunar tidal constituent M 2 is studied globally by an analysis of a high-resolution ocean circulation and tide model (STORMTIDE) simulation, of 19 years of satellite altimeter data, and of multiyear tide-gauge records. The barotropic seasonal tidal variability is domin...
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ftpubman:oai:pure.mpg.de:item_1909507 2023-10-09T21:49:18+02:00 Seasonal variation of the M2 tide Müller, M. Cherniawsky, J. Foreman, M. von Storch, J. 2014-02 application/pdf http://hdl.handle.net/11858/00-001M-0000-0015-0F60-A http://hdl.handle.net/11858/00-001M-0000-0018-0DC7-B eng eng info:eu-repo/semantics/altIdentifier/doi/10.1007/s10236-013-0679-0 http://hdl.handle.net/11858/00-001M-0000-0015-0F60-A http://hdl.handle.net/11858/00-001M-0000-0018-0DC7-B Ocean Dynamics info:eu-repo/semantics/article 2014 ftpubman https://doi.org/10.1007/s10236-013-0679-0 2023-09-17T23:46:40Z The seasonal cycle of the main lunar tidal constituent M 2 is studied globally by an analysis of a high-resolution ocean circulation and tide model (STORMTIDE) simulation, of 19 years of satellite altimeter data, and of multiyear tide-gauge records. The barotropic seasonal tidal variability is dominant in coastal and polar regions with relative changes of the tidal amplitude of 5–10 %. A comparison with the observations shows that the ocean circulation and tide model captures the seasonal pattern of the M 2 tide reasonably well. There are two main processes leading to the seasonal variability in the barotropic tide: First, seasonal changes in stratification on the continental shelf affect the vertical profile of eddy viscosity and, in turn, the vertical current profile. Second, the frictional effect between sea-ice and the surface ocean layer leads to seasonally varying tidal transport. We estimate from the model simulation that the M 2 tidal energy dissipation at the sea surface varies seasonally in the Arctic (ocean regions north of 60°N) between 2 and 34 GW, whereas in the Southern Ocean, it varies between 0.5 and 2 GW. The M 2 internal tide is mainly affected by stratification, and the induced modified phase speed of the internal waves leads to amplitude differences in the surface tide signal of 0.005–0.0150 m. The seasonal signals of the M 2 surface tide are large compared to the accuracy demands of satellite altimetry and gravity observations and emphasize the importance to consider seasonal tidal variability in the correction processes of satellite data. Article in Journal/Newspaper Arctic Arctic Ocean Sea ice Southern Ocean Max Planck Society: MPG.PuRe Arctic Southern Ocean Arctic Ocean Ocean Dynamics 64 2 159 177 |
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Open Polar |
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Max Planck Society: MPG.PuRe |
op_collection_id |
ftpubman |
language |
English |
description |
The seasonal cycle of the main lunar tidal constituent M 2 is studied globally by an analysis of a high-resolution ocean circulation and tide model (STORMTIDE) simulation, of 19 years of satellite altimeter data, and of multiyear tide-gauge records. The barotropic seasonal tidal variability is dominant in coastal and polar regions with relative changes of the tidal amplitude of 5–10 %. A comparison with the observations shows that the ocean circulation and tide model captures the seasonal pattern of the M 2 tide reasonably well. There are two main processes leading to the seasonal variability in the barotropic tide: First, seasonal changes in stratification on the continental shelf affect the vertical profile of eddy viscosity and, in turn, the vertical current profile. Second, the frictional effect between sea-ice and the surface ocean layer leads to seasonally varying tidal transport. We estimate from the model simulation that the M 2 tidal energy dissipation at the sea surface varies seasonally in the Arctic (ocean regions north of 60°N) between 2 and 34 GW, whereas in the Southern Ocean, it varies between 0.5 and 2 GW. The M 2 internal tide is mainly affected by stratification, and the induced modified phase speed of the internal waves leads to amplitude differences in the surface tide signal of 0.005–0.0150 m. The seasonal signals of the M 2 surface tide are large compared to the accuracy demands of satellite altimetry and gravity observations and emphasize the importance to consider seasonal tidal variability in the correction processes of satellite data. |
format |
Article in Journal/Newspaper |
author |
Müller, M. Cherniawsky, J. Foreman, M. von Storch, J. |
spellingShingle |
Müller, M. Cherniawsky, J. Foreman, M. von Storch, J. Seasonal variation of the M2 tide |
author_facet |
Müller, M. Cherniawsky, J. Foreman, M. von Storch, J. |
author_sort |
Müller, M. |
title |
Seasonal variation of the M2 tide |
title_short |
Seasonal variation of the M2 tide |
title_full |
Seasonal variation of the M2 tide |
title_fullStr |
Seasonal variation of the M2 tide |
title_full_unstemmed |
Seasonal variation of the M2 tide |
title_sort |
seasonal variation of the m2 tide |
publishDate |
2014 |
url |
http://hdl.handle.net/11858/00-001M-0000-0015-0F60-A http://hdl.handle.net/11858/00-001M-0000-0018-0DC7-B |
geographic |
Arctic Southern Ocean Arctic Ocean |
geographic_facet |
Arctic Southern Ocean Arctic Ocean |
genre |
Arctic Arctic Ocean Sea ice Southern Ocean |
genre_facet |
Arctic Arctic Ocean Sea ice Southern Ocean |
op_source |
Ocean Dynamics |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1007/s10236-013-0679-0 http://hdl.handle.net/11858/00-001M-0000-0015-0F60-A http://hdl.handle.net/11858/00-001M-0000-0018-0DC7-B |
op_doi |
https://doi.org/10.1007/s10236-013-0679-0 |
container_title |
Ocean Dynamics |
container_volume |
64 |
container_issue |
2 |
container_start_page |
159 |
op_container_end_page |
177 |
_version_ |
1779312321854701568 |