Abstract

Seismic ambient noise with frequencies > 1 Hz includes noise related to human activities. A reduction in seismic noise during the COVID-19 pandemic has been observed worldwide, as restrictions were imposed to control outbreaks of the SARS-CoV-2 virus. In this context, we studied the effect of changes in anthropogenic activities during COVID-19 on the seismic noise levels in the Tokyo metropolitan area, Japan, considering time of day, day of the week, and seasonal changes. The results showed the largest reduction in noise levels during the first state of emergency under most conditions. After the first state of emergency was lifted, the daytime noise reverted to previous levels immediately on weekdays and gradually on Sundays. This was likely because economic activities instantly resumed, while non-essential outings on Sundays were still mostly avoided. Furthermore, the daytime noise level on Sundays was strongly reduced regardless of changes on weekdays after the second state of emergency, which restricted activities mainly at night. Sunday noise levels gradually increased from the middle of the second state of emergency, suggesting a gradual reduction in public concern about COVID-19 following a decrease in the number of infections. Our findings demonstrate that seismic noise can be used to monitor social activities.

Highlights

  • Seismic ambient noise with frequencies > 1 Hz includes noise related to human activities

  • Using continuous seismic data recorded by MeSO-net stations, we monitored the changes in the seismic noise levels around Tokyo from April 2017 to March 2021

  • To constrain the effect of human activities on anthropogenic seismic noise, we studied the temporal variations of power spectral density (PSD) depending on the time of day and day of the week (Figs. 4 and 5)

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Summary

Introduction

Seismic ambient noise with frequencies > 1 Hz includes noise related to human activities. After the outbreak of COVID-19, the difference in the temporal variations of PSD with time of day became larger in both frequency bands (Fig. 4b).

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Conclusion
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