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dc.date.accessioned2018-08-14T16:23:59Z
dc.date.available2018-08-14T16:23:59Z
dc.date.created2012-02-01T10:43:12Z
dc.date.issued2012
dc.identifier.citationKöhler, Andreas Weidle, Christian Maupin, Valerie . On the effect of topography on surface wave propagation in the ambient noise frequency range. Journal of Seismology. 2012, 16(2), 221-231
dc.identifier.urihttp://hdl.handle.net/10852/62963
dc.description.abstractDue to the increasing popularity of analyzing empirical Green’s functions obtained from ambient seismic noise, more and more regional tomographical studies based on short-period surface waves are published. Results could potentially be biased in mountainous regions where topography is not small compared to the wavelength and penetration depth of the considered waves. We investigate the effect of topography on the propagation of short-period Rayleigh waves empirically by means of synthetic data using a spectral element code and a 3-D model with real topography. We show that topography along a profile through the studied area can result in an underestimation of phase velocities of up to about 0.7% at the shortest investigated period (3 s). Contrary to the expectation that this bias results from the increased surface distance along topography, we find that this error can be estimated by local topographic contrasts in the vicinity of the receiver alone. We discuss and generalize our results by considering topographic profiles through other mountain ranges and find that southern Norway is a good proxy to assess the topography effect. Nevertheless, topographic bias on phase velocity measurements is in general not large enough to significantly affect recovered velocity variations in the ambient noise frequency range. © 2012 Springer Verlagen_US
dc.languageEN
dc.titleOn the effect of topography on surface wave propagation in the ambient noise frequency rangeen_US
dc.typeJournal articleen_US
dc.creator.authorKöhler, Andreas
dc.creator.authorWeidle, Christian
dc.creator.authorMaupin, Valerie
cristin.unitcode185,15,22,0
cristin.unitnameInstitutt for geofag
cristin.ispublishedtrue
cristin.fulltextpostprint
cristin.qualitycode1
dc.identifier.cristin902738
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Journal of Seismology&rft.volume=16&rft.spage=221&rft.date=2012
dc.identifier.jtitleJournal of Seismology
dc.identifier.volume16
dc.identifier.issue2
dc.identifier.startpage221
dc.identifier.endpage231
dc.identifier.doihttp://dx.doi.org/10.1007/s10950-011-9264-5
dc.identifier.urnURN:NBN:no-65528
dc.type.documentTidsskriftartikkelen_US
dc.type.peerreviewedPeer reviewed
dc.source.issn1383-4649
dc.identifier.fulltextFulltext https://www.duo.uio.no/bitstream/handle/10852/62963/3/KoehlerEtal.pdf
dc.type.versionAcceptedVersion


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