Academic Journal
Comparison of Atmospheric and Non-tidal Ocean Loading Corrections for High-Precision Terrestrial Gravity Time Series.
| Τίτλος: | Comparison of Atmospheric and Non-tidal Ocean Loading Corrections for High-Precision Terrestrial Gravity Time Series. |
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| Συγγραφείς: | Antokoletz, Ezequiel D.1 (AUTHOR) Ezequiel.Antokoletz@bkg.bund.de, Boy, Jean-Paul2 (AUTHOR), Wziontek, Hartmut1 (AUTHOR), Balidakis, Kyriakos1,3 (AUTHOR), Klügel, Thomas1 (AUTHOR), Dobslaw, Henryk3 (AUTHOR), Tocho, Claudia N.4 (AUTHOR) |
| Πηγή: | Pure & Applied Geophysics. Jan2026, Vol. 183 Issue 1, p43-58. 16p. |
| Θεματικοί όροι: | *Atmospheric pressure, *Gravimeters (Geophysical instruments), *Sea level, *Numerical weather forecasting, *Gravitation, *Mass transfer, *Wind pressure |
| Περίληψη: | Besides Earth tides, the atmosphere causes the most significant contributions to time-variable gravity. State-of-the-art modelling approaches of atmospheric loading (Newtonian attraction and deformation) benefit from numerical weather models in order to account for global air mass variations. Atmospheric loading effects are often computed assuming that the oceans respond as an Inverse Barometer (IB) which is not completely valid for periods shorter than a few weeks. Therefore, a more precise modelling is only possible considering the ocean response to atmospheric pressure and winds based on simulations of an ocean dynamic model. Superconducting gravimeters (SGs) measure temporal gravity variations with high-resolution and exceptional stability and are capable to sense mass redistribution in the atmosphere, the oceans and in terrestrial water storage. In this sense, although SGs provide information for particular sites, they allow for a reliable validation of mass variations represented by models for atmosphere and oceans. In the present study, a comparison of atmospheric and non-tidal ocean loading corrections as calculated by the recently updated Atmospheric attraction computation service (Atmacs) and the EOST Loading Service is performed. For this comparison, a set of SG stations is selected, with focus on stations close to the oceans where non-tidal ocean loading effects are more significant. An emphasis is made on the reduction of gravity residuals by different corrections. [ABSTRACT FROM AUTHOR] |
| Βάση Δεδομένων: | Academic Search Index |
| FullText | Links: – Type: other Text: Availability: 0 CustomLinks: – Url: https://dx.doi.org/doi:10.1007/s00024-025-03804-0 Name: EDS - Springer Nature Journals (s7799221) Category: fullText Text: View record at Springer |
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| Header | DbId: asx DbLabel: Academic Search Index An: 191290700 RelevancyScore: 1393 AccessLevel: 6 PubType: Academic Journal PubTypeId: academicJournal PreciseRelevancyScore: 1393.34948730469 |
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| Items | – Name: Title Label: Title Group: Ti Data: Comparison of Atmospheric and Non-tidal Ocean Loading Corrections for High-Precision Terrestrial Gravity Time Series. – Name: Author Label: Authors Group: Au Data: <searchLink fieldCode="AR" term="%22Antokoletz%2C+Ezequiel+D%2E%22">Antokoletz, Ezequiel D.</searchLink><relatesTo>1</relatesTo> (AUTHOR)<i> Ezequiel.Antokoletz@bkg.bund.de</i><br /><searchLink fieldCode="AR" term="%22Boy%2C+Jean-Paul%22">Boy, Jean-Paul</searchLink><relatesTo>2</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Wziontek%2C+Hartmut%22">Wziontek, Hartmut</searchLink><relatesTo>1</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Balidakis%2C+Kyriakos%22">Balidakis, Kyriakos</searchLink><relatesTo>1,3</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Klügel%2C+Thomas%22">Klügel, Thomas</searchLink><relatesTo>1</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Dobslaw%2C+Henryk%22">Dobslaw, Henryk</searchLink><relatesTo>3</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Tocho%2C+Claudia+N%2E%22">Tocho, Claudia N.</searchLink><relatesTo>4</relatesTo> (AUTHOR) – Name: TitleSource Label: Source Group: Src Data: <searchLink fieldCode="JN" term="%22Pure+%26+Applied+Geophysics%22">Pure & Applied Geophysics</searchLink>. Jan2026, Vol. 183 Issue 1, p43-58. 16p. – Name: Subject Label: Subject Terms Group: Su Data: *<searchLink fieldCode="DE" term="%22Atmospheric+pressure%22">Atmospheric pressure</searchLink><br />*<searchLink fieldCode="DE" term="%22Gravimeters+%28Geophysical+instruments%29%22">Gravimeters (Geophysical instruments)</searchLink><br />*<searchLink fieldCode="DE" term="%22Sea+level%22">Sea level</searchLink><br />*<searchLink fieldCode="DE" term="%22Numerical+weather+forecasting%22">Numerical weather forecasting</searchLink><br />*<searchLink fieldCode="DE" term="%22Gravitation%22">Gravitation</searchLink><br />*<searchLink fieldCode="DE" term="%22Mass+transfer%22">Mass transfer</searchLink><br />*<searchLink fieldCode="DE" term="%22Wind+pressure%22">Wind pressure</searchLink> – Name: Abstract Label: Abstract Group: Ab Data: Besides Earth tides, the atmosphere causes the most significant contributions to time-variable gravity. State-of-the-art modelling approaches of atmospheric loading (Newtonian attraction and deformation) benefit from numerical weather models in order to account for global air mass variations. Atmospheric loading effects are often computed assuming that the oceans respond as an Inverse Barometer (IB) which is not completely valid for periods shorter than a few weeks. Therefore, a more precise modelling is only possible considering the ocean response to atmospheric pressure and winds based on simulations of an ocean dynamic model. Superconducting gravimeters (SGs) measure temporal gravity variations with high-resolution and exceptional stability and are capable to sense mass redistribution in the atmosphere, the oceans and in terrestrial water storage. In this sense, although SGs provide information for particular sites, they allow for a reliable validation of mass variations represented by models for atmosphere and oceans. In the present study, a comparison of atmospheric and non-tidal ocean loading corrections as calculated by the recently updated Atmospheric attraction computation service (Atmacs) and the EOST Loading Service is performed. For this comparison, a set of SG stations is selected, with focus on stations close to the oceans where non-tidal ocean loading effects are more significant. An emphasis is made on the reduction of gravity residuals by different corrections. [ABSTRACT FROM AUTHOR] |
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| RecordInfo | BibRecord: BibEntity: Identifiers: – Type: doi Value: 10.1007/s00024-025-03804-0 Languages: – Code: eng Text: English PhysicalDescription: Pagination: PageCount: 16 StartPage: 43 Subjects: – SubjectFull: Atmospheric pressure Type: general – SubjectFull: Gravimeters (Geophysical instruments) Type: general – SubjectFull: Sea level Type: general – SubjectFull: Numerical weather forecasting Type: general – SubjectFull: Gravitation Type: general – SubjectFull: Mass transfer Type: general – SubjectFull: Wind pressure Type: general Titles: – TitleFull: Comparison of Atmospheric and Non-tidal Ocean Loading Corrections for High-Precision Terrestrial Gravity Time Series. Type: main BibRelationships: HasContributorRelationships: – PersonEntity: Name: NameFull: Antokoletz, Ezequiel D. – PersonEntity: Name: NameFull: Boy, Jean-Paul – PersonEntity: Name: NameFull: Wziontek, Hartmut – PersonEntity: Name: NameFull: Balidakis, Kyriakos – PersonEntity: Name: NameFull: Klügel, Thomas – PersonEntity: Name: NameFull: Dobslaw, Henryk – PersonEntity: Name: NameFull: Tocho, Claudia N. IsPartOfRelationships: – BibEntity: Dates: – D: 01 M: 01 Text: Jan2026 Type: published Y: 2026 Identifiers: – Type: issn-print Value: 00334553 Numbering: – Type: volume Value: 183 – Type: issue Value: 1 Titles: – TitleFull: Pure & Applied Geophysics Type: main |
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