Observation of Coriolis coupled modes below 1 mHz
We present observations of spectral energy at toroidal mode frequencies in vertical seismic recordings of the 1998 Balleny Islands earthquake. Since toroidal modes on a spherically symmetric, non-rotating Earth have horizontally polarized particle motion these observations call for an explanation. W...
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2000
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fthighwire:oai:open-archive.highwire.org:gji:143/1/113 2023-05-15T15:37:24+02:00 Observation of Coriolis coupled modes below 1 mHz Zürn, W. Laske, G. Widmer-Schnidrig, R. Gilbert, F. 2000-10-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/143/1/113 https://doi.org/10.1046/j.1365-246x.2000.00220.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/143/1/113 http://dx.doi.org/10.1046/j.1365-246x.2000.00220.x Copyright (C) 2000, Oxford University Press Articles TEXT 2000 fthighwire https://doi.org/10.1046/j.1365-246x.2000.00220.x 2013-05-27T17:21:55Z We present observations of spectral energy at toroidal mode frequencies in vertical seismic recordings of the 1998 Balleny Islands earthquake. Since toroidal modes on a spherically symmetric, non-rotating Earth have horizontally polarized particle motion these observations call for an explanation. We first rule out local and instrumental effects as being responsible for the vertical-component signal of the toroidal modes 0 T 3 (0.59mHz) and 0 T 4 (0.77mHz). The global effects that we consider are general heterogeneous mantle structure, ellipticity of figure and rotation. We find that rotation through Coriolis coupling of low-order spheroidal and toroidal oscillations is the dominant mechanism. Text Balleny Islands HighWire Press (Stanford University) Balleny Islands Geophysical Journal International 143 1 113 118 |
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HighWire Press (Stanford University) |
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English |
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Articles Zürn, W. Laske, G. Widmer-Schnidrig, R. Gilbert, F. Observation of Coriolis coupled modes below 1 mHz |
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Articles |
description |
We present observations of spectral energy at toroidal mode frequencies in vertical seismic recordings of the 1998 Balleny Islands earthquake. Since toroidal modes on a spherically symmetric, non-rotating Earth have horizontally polarized particle motion these observations call for an explanation. We first rule out local and instrumental effects as being responsible for the vertical-component signal of the toroidal modes 0 T 3 (0.59mHz) and 0 T 4 (0.77mHz). The global effects that we consider are general heterogeneous mantle structure, ellipticity of figure and rotation. We find that rotation through Coriolis coupling of low-order spheroidal and toroidal oscillations is the dominant mechanism. |
format |
Text |
author |
Zürn, W. Laske, G. Widmer-Schnidrig, R. Gilbert, F. |
author_facet |
Zürn, W. Laske, G. Widmer-Schnidrig, R. Gilbert, F. |
author_sort |
Zürn, W. |
title |
Observation of Coriolis coupled modes below 1 mHz |
title_short |
Observation of Coriolis coupled modes below 1 mHz |
title_full |
Observation of Coriolis coupled modes below 1 mHz |
title_fullStr |
Observation of Coriolis coupled modes below 1 mHz |
title_full_unstemmed |
Observation of Coriolis coupled modes below 1 mHz |
title_sort |
observation of coriolis coupled modes below 1 mhz |
publisher |
Oxford University Press |
publishDate |
2000 |
url |
http://gji.oxfordjournals.org/cgi/content/short/143/1/113 https://doi.org/10.1046/j.1365-246x.2000.00220.x |
geographic |
Balleny Islands |
geographic_facet |
Balleny Islands |
genre |
Balleny Islands |
genre_facet |
Balleny Islands |
op_relation |
http://gji.oxfordjournals.org/cgi/content/short/143/1/113 http://dx.doi.org/10.1046/j.1365-246x.2000.00220.x |
op_rights |
Copyright (C) 2000, Oxford University Press |
op_doi |
https://doi.org/10.1046/j.1365-246x.2000.00220.x |
container_title |
Geophysical Journal International |
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143 |
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1 |
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113 |
op_container_end_page |
118 |
_version_ |
1766367959482105856 |