Articles | Volume 11, issue 1
Research article
29 Jan 2020
Research article |  | 29 Jan 2020

The relative contributions of scattering and viscoelasticity to the attenuation of S waves in Earth's mantle

Susini deSilva and Vernon F. Cormier


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Vernon Cormier on behalf of the Authors (13 Nov 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (25 Nov 2019) by Caroline Beghein
RR by Ian Jackson (14 Dec 2019)
ED: Publish as is (17 Dec 2019) by Caroline Beghein
ED: Publish as is (20 Dec 2019) by CharLotte Krawczyk(Executive Editor)
Short summary
Seismic waves attenuate with distance due to two effects: (1) removal of energy by internal friction and (2) redistribution of energy into different distances and time windows by scattering from heterogeneous Earth structure. The relative contribution of these two effects is estimated by synthesizing seismograms having varying amounts of internal friction and heterogeneities. The attenuation of observed S waveforms requires contributions from both internal friction and scattering.