Atmospheric Contributions to Global Ocean Tides for Satellite Gravimetry ...
To mitigate temporal aliasing effects in monthly mean global gravity fields from the GRACE and GRACE‐FO satellite tandem missions, both tidal and non‐tidal background models describing high‐frequency mass variability in atmosphere and oceans are needed. To quantify tides in the atmosphere, we exploi...
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ftdatacite:10.17169/refubium-38769 2023-06-11T04:07:07+02:00 Atmospheric Contributions to Global Ocean Tides for Satellite Gravimetry ... Balidakis, Kyriakos Sulzbach, Roman Shihora, Linus Dahle, Christoph Dill, Robert Dobslaw, Henryk 2022 https://dx.doi.org/10.17169/refubium-38769 https://refubium.fu-berlin.de/handle/fub188/39053 unknown Freie Universität Berlin https://doi.org/10.1029/2022MS003193 https://dx.doi.org/10.1029/2022ms003193 https://doi.org/10.1029/2022MS003193 Creative Commons Attribution 4.0 International This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 atmospheric tides ocean tides de‐aliasing GRACE‐FO ERA5 atmospheric forcing 500 Naturwissenschaften und Mathematik550 Geowissenschaften, Geologie550 Geowissenschaften Wissenschaftlicher Artikel article-journal Text ScholarlyArticle 2022 ftdatacite https://doi.org/10.17169/refubium-3876910.1029/2022ms003193 2023-05-02T10:36:13Z To mitigate temporal aliasing effects in monthly mean global gravity fields from the GRACE and GRACE‐FO satellite tandem missions, both tidal and non‐tidal background models describing high‐frequency mass variability in atmosphere and oceans are needed. To quantify tides in the atmosphere, we exploit the higher spatial (31 km) and temporal (1 hr) resolution provided by the latest atmospheric ECMWF reanalysis, ERA5. The oceanic response to atmospheric tides is subsequently modeled with the general ocean circulation model MPIOM (in a recently revised TP10L40 configuration that includes the feedback of self‐attraction and loading to the momentum equations and has an improved bathymetry around Antarctica) as well as the shallow water model TiME (employing a much higher spatial resolution and more elaborate tidal dissipation than MPIOM). Both ocean models consider jointly the effects of atmospheric pressure variations and surface wind stress. We present the characteristics of 16 waves beating at frequencies in ... Text Antarc* Antarctica DataCite Metadata Store (German National Library of Science and Technology) |
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atmospheric tides ocean tides de‐aliasing GRACE‐FO ERA5 atmospheric forcing 500 Naturwissenschaften und Mathematik550 Geowissenschaften, Geologie550 Geowissenschaften |
spellingShingle |
atmospheric tides ocean tides de‐aliasing GRACE‐FO ERA5 atmospheric forcing 500 Naturwissenschaften und Mathematik550 Geowissenschaften, Geologie550 Geowissenschaften Balidakis, Kyriakos Sulzbach, Roman Shihora, Linus Dahle, Christoph Dill, Robert Dobslaw, Henryk Atmospheric Contributions to Global Ocean Tides for Satellite Gravimetry ... |
topic_facet |
atmospheric tides ocean tides de‐aliasing GRACE‐FO ERA5 atmospheric forcing 500 Naturwissenschaften und Mathematik550 Geowissenschaften, Geologie550 Geowissenschaften |
description |
To mitigate temporal aliasing effects in monthly mean global gravity fields from the GRACE and GRACE‐FO satellite tandem missions, both tidal and non‐tidal background models describing high‐frequency mass variability in atmosphere and oceans are needed. To quantify tides in the atmosphere, we exploit the higher spatial (31 km) and temporal (1 hr) resolution provided by the latest atmospheric ECMWF reanalysis, ERA5. The oceanic response to atmospheric tides is subsequently modeled with the general ocean circulation model MPIOM (in a recently revised TP10L40 configuration that includes the feedback of self‐attraction and loading to the momentum equations and has an improved bathymetry around Antarctica) as well as the shallow water model TiME (employing a much higher spatial resolution and more elaborate tidal dissipation than MPIOM). Both ocean models consider jointly the effects of atmospheric pressure variations and surface wind stress. We present the characteristics of 16 waves beating at frequencies in ... |
format |
Text |
author |
Balidakis, Kyriakos Sulzbach, Roman Shihora, Linus Dahle, Christoph Dill, Robert Dobslaw, Henryk |
author_facet |
Balidakis, Kyriakos Sulzbach, Roman Shihora, Linus Dahle, Christoph Dill, Robert Dobslaw, Henryk |
author_sort |
Balidakis, Kyriakos |
title |
Atmospheric Contributions to Global Ocean Tides for Satellite Gravimetry ... |
title_short |
Atmospheric Contributions to Global Ocean Tides for Satellite Gravimetry ... |
title_full |
Atmospheric Contributions to Global Ocean Tides for Satellite Gravimetry ... |
title_fullStr |
Atmospheric Contributions to Global Ocean Tides for Satellite Gravimetry ... |
title_full_unstemmed |
Atmospheric Contributions to Global Ocean Tides for Satellite Gravimetry ... |
title_sort |
atmospheric contributions to global ocean tides for satellite gravimetry ... |
publisher |
Freie Universität Berlin |
publishDate |
2022 |
url |
https://dx.doi.org/10.17169/refubium-38769 https://refubium.fu-berlin.de/handle/fub188/39053 |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_relation |
https://doi.org/10.1029/2022MS003193 https://dx.doi.org/10.1029/2022ms003193 https://doi.org/10.1029/2022MS003193 |
op_rights |
Creative Commons Attribution 4.0 International This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.17169/refubium-3876910.1029/2022ms003193 |
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1768379798745251840 |