Machine learning and marsquakes: a tool to predict atmospheric-seismic noise for the NASA InSight mission

Author:

Stott A E1ORCID,Garcia R F1,Chédozeau A1,Spiga A2,Murdoch N1,Pinot B1,Mimoun D1,Charalambous C3,Horleston A4,King S D5,Kawamura T6,Dahmen N7,Barkaoui S6,Lognonné P6,Banerdt W B8ORCID

Affiliation:

1. Institut Supérieur de l’Aéronautique et de l’Espace (ISAE-SUPAERO) , 31400 Toulouse, France

2. Laboratoire de Météorologie Dynamique/IPSL, Sorbonne Université, CNRS, Ecole Normale Supérieure, PSL Research University , Ecole Polytechnique, 75005 Paris, France

3. Department of Electrical and Electronic Engineering , Imperial College London, SW7 2AZ London, UK

4. School of Earth Sciences, University of Bristol , BS8 1RJ Bristol, UK

5. Department of Geosciences, Virginia Tech , Blacksburg, 24061 VA, USA

6. Institut de Physique du globe de Paris, Université de Paris, CNRS , 75005 Paris, France

7. Institute of Geophysics , ETH Zurich, 8092 Zurich, Switzerland

8. Jet Propulsion Laboratory, California Institute of Technology , Pasadena, 91109 CA, USA

Abstract

SUMMARY The SEIS (seismic experiment for the interior structure of Mars) experiment on the NASA InSight mission has catalogued hundreds of marsquakes so far. However, the detectability of these events is controlled by the weather which generates noise on the seismometer. This affects the catalogue on both diurnal and seasonal scales. We propose to use machine learning methods to fit the wind, pressure and temperature data to the seismic energy recorded in the 0.4–1 and 2.2–2.6 Hz bandwidths to examine low- (LF) and high-frequency (HF) seismic event categories respectively. We implement Gaussian process regression and neural network models for this task. This approach provides the relationship between the atmospheric state and seismic energy. The obtained seismic energy estimate is used to calculate signal-to-noise ratios (SNR) of marsquakes for multiple bandwidths. We can then demonstrate the presence of LF energy above the noise level during several events predominantly categorized as HF, suggesting a continuum in event spectra distribution across the marsquake types. We introduce an algorithm to detect marsquakes based on the subtraction of the predicted noise from the observed data. This algorithm finds 39 previously undetected marsquakes, with another 40 possible candidates. Furthermore, an analysis of the detection algorithm’s variable threshold provides an empirical estimate of marsquake detectivity. This suggests that events producing the largest signal on the seismometer would be seen almost all the time, the median size signal event 45–50 per cent of the time and smallest signal events 5−20 per cent of the time.

Funder

NASA

CNES

ANR

UK Space Agency

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Reference44 articles.

1. Insight auxiliary payload sensor suite (apss);Banfield;Space Sci. Rev.,2019

2. The atmosphere of mars as observed by insight;Banfield;Nat. Geosci.,2020

3. Anatomy of continuous mars seis and pressure data from unsupervised learning;Barkaoui;Bull. seism. Soc. Am.,2021

4. Obspy: a python toolbox for seismology;Beyreuther;Seismol. Res. Lett.,2010

5. Magnitude scales for marsquakes calibrated from insight data;Böse;Bull. seism. Soc. Am.,2021

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