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Journal ArticleDOI

Removing Noise from the Vertical Component Records of Ocean‐Bottom Seismometers: Results from Year One of the Cascadia Initiative

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TLDR
In this paper, the authors developed a methodology for reducing the amplitude of vertical noise sources by 1-2 orders of magnitude, revealing many events that could not be distinguished before noise reduction, and correcting for any signal distortion caused by the noise removal.
Abstract
Through an array of ocean‐bottom seismometers, the Cascadia Initiative is investigating the structure of the Juan de Fuca and Gorda plates. Because the instruments are on the seafloor, they are subject to substantial noise from water waves and bottom currents, especially at long periods. If the seismometer is slightly tilted, some of the high bottom current noise on the horizontals leaks onto the vertical record. Another major type of noise, compliance noise, is created when pressure variations associated with infragravity waves physically deflect the seabed. Extending the work of Crawford and Webb (2000), we developed a methodology for reducing the amplitude of vertical noise sources by 1–2 orders of magnitude, revealing many events that could not be distinguished before noise reduction, and for correcting for any signal distortion caused by the noise removal. We use the horizontal records to predict and remove the tilt noise from the verticals, and we use the pressure records to predict and remove the compliance noise from the first year of Cascadia Initiative data. After determining the degree and direction of tilt for each day at each station, we assessed the success of different instrument designs at minimizing tilt noise; external shielding of the seismometer sensor package is effective at reducing bottom current noise. Tilt at individual instruments can vary continuously throughout a several month deployment and should be determined at least daily for optimal noise removal. By understanding and reducing these noise sources, we hope to open the Cascadia dataset to a wider range of applications.

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Citations
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Journal ArticleDOI

Water input into the Mariana subduction zone estimated from ocean-bottom seismic data

TL;DR: Seismic images of Earth's crust and uppermost mantle around the Mariana trench derived from Rayleigh-wave analysis of broadband ocean-bottom seismic data show widespread serpentinization, suggesting that much more water is subducted than previously thought.
Journal ArticleDOI

High-resolution seismic constraints on flow dynamics in the oceanic asthenosphere.

TL;DR: Rayleigh waves are used to provide unique localized constraints on seismic anisotropy within the oceanic lithosphere–asthenosphere system in the middle of a plate to suggest that the highest strain deformation in the shallow oceanic mantle occurs during corner flow at the ridge axis, and via pressure-driven or buoyancy-driven flow within the asthenosphere.
Journal ArticleDOI

Fluid pressure and shear zone development over the locked to slow slip region in Cascadia.

TL;DR: Thickening of the LVL down dip where viscous creep dominates suggests that it represents the development of an increasingly thick and fluid-rich shear zone, enabled by fluid production in subducting oceanic crust.
Journal ArticleDOI

Imaging the Plate Interface in the Cascadia Seismogenic Zone: New Constraints from Offshore Receiver Functions

TL;DR: Inversions of onshore Global Positioning System data also can be used to determine the locking behavior and place the locked zone offshore (e.g., McCaffrey et al. as discussed by the authors ).
Journal ArticleDOI

Mantle flow geometry from ridge to trench beneath the Gorda-Juan de Fuca plate system

TL;DR: In this paper, the authors show that shallow mantle flow could be induced by the motions of overriding tectonic plates or by deeper mantle convection, and that flow aligns with the motion of the largest oceanic plates.
References
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Book

RANDOM DATA Analysis and Measurement Procedures

TL;DR: A revised and expanded edition of this classic reference/text, covering the latest techniques for the analysis and measurement of stationary and nonstationary random data passing through physical systems, is presented in this article.
Journal ArticleDOI

A theory of the origin of microseisms

TL;DR: In this paper, it was shown that in an infinite wave train there is in general a second-order pressure variation at infinite depth which is applied equally over the whole fluid and is associated with no particle motion.
Journal ArticleDOI

Broadband seismology and noise under the ocean

TL;DR: In this paper, the authors use wind and wave climatology to predict the temporal and geographical variability of the seismic noise spectrum and assess likely sites for permanent seafloor observatories.
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Ocean-generated microseismic noise located with the Gräfenberg array

TL;DR: In this paper, the authors used frequency-wavenumber analysis to locate the generating areas of mid-period seismic ground distortions using broadband continuous recordings over four months in winter 1995/96.
Journal ArticleDOI

Phase velocities of Rayleigh waves in the MELT experiment on the East Pacific Rise

TL;DR: The phase velocities of Rayleigh waves increase more rapidly with distance from the East Pacific Rise (EPR) axis than is predicted by models of conductive cooling of the lithosphere.
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