experimental
Entry: coda wave
URI: https://registry.epos-eu.org/ncl/FAIR-Incubator/tcs-SEISMO/33
The seismograms of an earthquake usually show some vibrations long after the passage of relevant body wave and surface wave onsets in the considered distance range. This portion of the seismogram to its end is called the coda. Coda waves are believed to be back-scattering waves due to inhomogeneities in the Earth. They have been extensively used to obtain source spectra, as well as to measure seismic attenuation and site amplification factors by the coda normalization method
Core metadata
is a | Concept |
submitted by | Tendry R |
accepted on | 10 Feb 2022 10:24:49.687 |
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All metadata properties
date accepted |
10 Feb 2022 10:24:49.687
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date submitted |
10 Feb 2022 10:16:37.418
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definition |
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description |
The seismograms of an earthquake usually show some vibrations long after the passage of relevant body wave and surface wave onsets in the considered distance range. This portion of the seismogram to its end is called the coda. Coda waves are believed to be back-scattering waves due to inhomogeneities in the Earth. They have been extensively used to obtain source spectra, as well as to measure seismic attenuation and site amplification factors by the coda normalization method
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item class |
Concept
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label |
coda wave
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notation |
33
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register |
tcs sEISMO
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status |
status experimental
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submitter |
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type |
register item
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version info |
2
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Definition
broader |
seismic wave
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description |
The seismograms of an earthquake usually show some vibrations long after the passage of relevant body wave and surface wave onsets in the considered distance range. This portion of the seismogram to its end is called the coda. Coda waves are believed to be back-scattering waves due to inhomogeneities in the Earth. They have been extensively used to obtain source spectra, as well as to measure seismic attenuation and site amplification factors by the coda normalization method
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label |
coda wave
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notation |
33
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pref label |
coda wave
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type |
Concept
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