Clock errors in land and ocean bottom seismograms: High-accuracy estimates from multiple-component noise cross-correlations
Autor: | Karin Sigloch, Sarah Hable, Guilhem Barruol, Céline Hadziioannou, Simon Stähler |
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Přispěvatelé: | Ludwig-Maximilians-Universität München (LMU), Department of Earth Sciences [Oxford], University of Oxford [Oxford], Laboratoire GéoSciences Réunion (LGSR), Université de La Réunion (UR)-Institut de Physique du Globe de Paris, Institut de Physique du Globe de Paris (IPGP), Centre National de la Recherche Scientifique (CNRS)-Université de La Réunion (UR)-Université Paris Diderot - Paris 7 (UPD7)-IPG PARIS-Institut national des sciences de l'Univers (INSU - CNRS), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology in Zürich [Zürich] (ETH Zürich), Universität Hamburg (UHH), ANR-11-BS56-0013,RHUM-RUM,Imagerie mantellique du point chaud de La Réunion(2011), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich), Institut de Physique du Globe de Paris-Université de La Réunion (UR), Institut national des sciences de l'Univers (INSU - CNRS)-IPG PARIS-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Centre National de la Recherche Scientifique (CNRS) |
Rok vydání: | 2018 |
Předmět: |
Observational error
010504 meteorology & atmospheric sciences Seismic noise business.industry [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] Clock drift Skew Time signal Seismic interferometry 010502 geochemistry & geophysics Geodesy 01 natural sciences Synchronization Seismic instruments Geophysics Geochemistry and Petrology Assisted GPS Time-series analysis Global Positioning System 14. Life underwater business Geology 0105 earth and related environmental sciences |
Zdroj: | Geophysical Journal International Geophysical Journal International, Oxford University Press (OUP), 2018, 214 (3), pp.2014-2034. ⟨10.1093/gji/ggy236⟩ Geophysical Journal International (0956-540X) (Oxford Univ Press), 2018-09, Vol. 214, N. 3, P. 2014-2034 Geophysical Journal International, 214 (3) |
ISSN: | 0956-540X 1365-246X |
Popis: | Many applications in seismology rely on the accurate absolute timing of seismograms. However, both seismological land stations and ocean bottom seismometers (OBSs) can be affected by clock errors, which cause the absolute timing of seismograms to deviate from a highly accurate reference time signal, usually provided by GPS satellites. Timing problems can occur in land stations when synchronization with a GPS signal is temporarily or permanently lost. This can give rise to complicated, time-dependent clock drifts relative to GPS time, due to varying environmental conditions. Seismometers at the ocean bottom cannot receive GPS satellite signals, but operate in more stable ambient conditions than land stations. The standard protocol is to synchronize an OBS with a GPS signal immediately before deployment and after recovery. The measured timing deviation, called “skew”, is assumed to have accumulated linearly over the deployment interval, an assumption that is plausible but usually not verifiable. In recent years, cross-correlations of ambient microseismic noise have been put to use for correcting timing errors, but have been limited to interstation distances of at most a few tens of kilometres without reducing the temporal resolution. We apply noise cross-correlations to the evaluation of clock errors in four broadband land stations and 53 wideband and broadband OBSs, which were installed on and around the island of La Réunion in the western Indian Ocean during the RHUM-RUM (Réunion Hotspot and Upper Mantle - Réunions Unterer Mantel) experiment. We correlate all three seismic components, plus a hydrophone channel in OBS stations. Daily cross-correlation functions are derived for intermediate distances (∼20 km) for land-to-land station pairs; stable, 10-day stacks are obtained for very large interstation distances up to >300 km for land-to-OBS, and OBS-to-OBS configurations. Averaging over multiple station pairs, and up to 16 component pairs per station, improves the accuracy of the method by a factor of four compared to the single-channel approaches of prior studies. The timing accuracy of our method is estimated to be ∼20 ms standard deviation, or one sample at a sampling rate of 50 Hz. In land stations, non-linear clock drifts and clock jumps of up to six minutes are detected and successfully corrected. For 52 out of 53 OBSs, we successfully obtain drift functions over time, which validate the common assumption of linear clock drift. Skew values that were available for 29 of these OBSs are consistent with our independent estimates within their observational error bars. For 23 OBSs that lacked skew measurements, linear OBS clock drifts range between 0.2 ms/day and 8.8 ms/day. In addition to linear drift, three OBSs are affected by clock jumps of ∼1 s, probably indicating a missing sample problem that would otherwise have gone undetected. Thus we demonstrate the routine feasibility of high-accuracy clock corrections in land and ocean bottom seismometers over a wide range of interstation distances. |
Databáze: | OpenAIRE |
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