Earth and Space Science (Nov 2020)
Detection, Analysis, and Removal of Glitches From InSight's Seismic Data From Mars
- John‐Robert Scholz,
- Rudolf Widmer‐Schnidrig,
- Paul Davis,
- Philippe Lognonné,
- Baptiste Pinot,
- Raphaël F. Garcia,
- Kenneth Hurst,
- Laurent Pou,
- Francis Nimmo,
- Salma Barkaoui,
- Sébastien de Raucourt,
- Brigitte Knapmeyer‐Endrun,
- Martin Knapmeyer,
- Guénolé Orhand‐Mainsant,
- Nicolas Compaire,
- Arthur Cuvier,
- Éric Beucler,
- Mickaël Bonnin,
- Rakshit Joshi,
- Grégory Sainton,
- Eléonore Stutzmann,
- Martin Schimmel,
- Anna Horleston,
- Maren Böse,
- Savas Ceylan,
- John Clinton,
- Martin van Driel,
- Taichi Kawamura,
- Amir Khan,
- Simon C. Stähler,
- Domenico Giardini,
- Constantinos Charalambous,
- Alexander E. Stott,
- William T. Pike,
- Ulrich R. Christensen,
- W. Bruce Banerdt
Affiliations
- John‐Robert Scholz
- Max Planck Institute for Solar System Research Göttingen Germany
- Rudolf Widmer‐Schnidrig
- Black Forest Observatory, Institute of Geodesy Stuttgart University Stuttgart Germany
- Paul Davis
- Department of Earth, Planetary, and Space Sciences University of California Los Angeles Los Angeles CA USA
- Philippe Lognonné
- Université de Paris, Institut de physique du globe de Paris, CNRS Paris France
- Baptiste Pinot
- Institut Supérieur de l'Aéronautique et de l'Espace SUPAERO Toulouse France
- Raphaël F. Garcia
- Institut Supérieur de l'Aéronautique et de l'Espace SUPAERO Toulouse France
- Kenneth Hurst
- Jet Propulsion Laboratory California Institute of Technology Pasadena USA
- Laurent Pou
- Department of Earth and Planetary Sciences University of California Santa Cruz Santa Cruz CA USA
- Francis Nimmo
- Department of Earth and Planetary Sciences University of California Santa Cruz Santa Cruz CA USA
- Salma Barkaoui
- Université de Paris, Institut de physique du globe de Paris, CNRS Paris France
- Sébastien de Raucourt
- Université de Paris, Institut de physique du globe de Paris, CNRS Paris France
- Brigitte Knapmeyer‐Endrun
- Bensberg Observatory University of Cologne Bergisch Gladbach Germany
- Martin Knapmeyer
- DLR Institute of Planetary Research Berlin Germany
- Guénolé Orhand‐Mainsant
- Institut Supérieur de l'Aéronautique et de l'Espace SUPAERO Toulouse France
- Nicolas Compaire
- Institut Supérieur de l'Aéronautique et de l'Espace SUPAERO Toulouse France
- Arthur Cuvier
- Laboratoire de Planétologie et Géodynamique, Université de Nantes, Université d'Angers Nantes France
- Éric Beucler
- Laboratoire de Planétologie et Géodynamique, Université de Nantes, Université d'Angers Nantes France
- Mickaël Bonnin
- Laboratoire de Planétologie et Géodynamique, Université de Nantes, Université d'Angers Nantes France
- Rakshit Joshi
- Max Planck Institute for Solar System Research Göttingen Germany
- Grégory Sainton
- Université de Paris, Institut de physique du globe de Paris, CNRS Paris France
- Eléonore Stutzmann
- Université de Paris, Institut de physique du globe de Paris, CNRS Paris France
- Martin Schimmel
- Institute of Earth Sciences Jaume Almera ‐ CSIC Barcelona Spain
- Anna Horleston
- School of Earth Sciences University of Bristol Bristol UK
- Maren Böse
- Swiss Seismological Service (SED) ETH Zurich Zurich, Switzerland
- Savas Ceylan
- Institute of Geophysics ETH Zürich Zurich Switzerland
- John Clinton
- Swiss Seismological Service (SED) ETH Zurich Zurich, Switzerland
- Martin van Driel
- Institute of Geophysics ETH Zürich Zurich Switzerland
- Taichi Kawamura
- Université de Paris, Institut de physique du globe de Paris, CNRS Paris France
- Amir Khan
- Institute of Geophysics ETH Zürich Zurich Switzerland
- Simon C. Stähler
- Institute of Geophysics ETH Zürich Zurich Switzerland
- Domenico Giardini
- Institute of Geophysics ETH Zürich Zurich Switzerland
- Constantinos Charalambous
- Department of Electrical and Electronic Engineering Imperial College London London UK
- Alexander E. Stott
- Department of Electrical and Electronic Engineering Imperial College London London UK
- William T. Pike
- Department of Electrical and Electronic Engineering Imperial College London London UK
- Ulrich R. Christensen
- Max Planck Institute for Solar System Research Göttingen Germany
- W. Bruce Banerdt
- Jet Propulsion Laboratory California Institute of Technology Pasadena USA
- DOI
- https://doi.org/10.1029/2020EA001317
- Journal volume & issue
-
Vol. 7,
no. 11
pp. n/a – n/a
Abstract
Abstract The instrument package SEIS (Seismic Experiment for Internal Structure) with the three very broadband and three short‐period seismic sensors is installed on the surface on Mars as part of NASA's InSight Discovery mission. When compared to terrestrial installations, SEIS is deployed in a very harsh wind and temperature environment that leads to inevitable degradation of the quality of the recorded data. One ubiquitous artifact in the raw data is an abundance of transient one‐sided pulses often accompanied by high‐frequency spikes. These pulses, which we term “glitches”, can be modeled as the response of the instrument to a step in acceleration, while the spikes can be modeled as the response to a simultaneous step in displacement. We attribute the glitches primarily to SEIS‐internal stress relaxations caused by the large temperature variations to which the instrument is exposed during a Martian day. Only a small fraction of glitches correspond to a motion of the SEIS package as a whole caused by minuscule tilts of either the instrument or the ground. In this study, we focus on the analysis of the glitch+spike phenomenon and present how these signals can be automatically detected and removed from SEIS's raw data. As glitches affect many standard seismological analysis methods such as receiver functions, spectral decomposition and source inversions, we anticipate that studies of the Martian seismicity as well as studies of Mars' internal structure should benefit from deglitched seismic data.
Keywords