EGU24-14905, updated on 09 Mar 2024
https://doi.org/10.5194/egusphere-egu24-14905
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Removing low frequency ocean bottom seismometer tilt noise using simple sensor reorientation

Wayne Crawford1, Gabi Laske2, Nicholas Harmon3, and Catherine Rychert3
Wayne Crawford et al.
  • 1IPGP Université Paris Cité, CNRS UMR 7154, Paris, France (crawford@ipgp.fr)
  • 2Scripps Institution of Oceanography, UC San Diego, San Diego, USA
  • 3Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, USA

Ocean bottom seismometer data are strongly affected by noise from seafloor currents.  Techniques based on the transfer function between noise on the horizontal and vertical channels are commonly used to “clean” this noise from low-frequency (< 0.1 Hz) vertical channel data, but questions remain about the efficiency of this technique and its effect on seismological signals.  We present a method to “pre-clean” the vertical data through simple rotation of the seismometer to minimize the noise on the vertical channel.  The rotation is nearly identical to that indicated by the transfer function method, but has the advantage of losing no information.  Once this pre-cleaning is performed, transfer-function based cleaning can still be performed, generally resulting in lower noise levels than those obtained using the transfer function method alone and the remaining transfer function may provide information beyond that of the instrument’s mis-alignment with the gravitational field.  We will present examples from datasets around the world and discuss new information revealed.

How to cite: Crawford, W., Laske, G., Harmon, N., and Rychert, C.: Removing low frequency ocean bottom seismometer tilt noise using simple sensor reorientation, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-14905, https://doi.org/10.5194/egusphere-egu24-14905, 2024.

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