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Field of coherence of GPS-measured earth tremors

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Abstract

A new method for investigating the coherence field of the noise component of high-frequency GPS time series is proposed. The method is applied to the main territory of the USA, which is characterized by a dense network of GPS stations. The data are presented in steps of 5 min from February 28, 2013, until June 29, 2019, on the Nevada Geodetic Laboratory Web site. The proposed method estimates the spatial distribution of the mean values of multiple coherence, calculated within nodes of a regular grid, between GPS coordinates of a given number of nearest operable stations and the periods at which the maximum values of coherence are reached. The two-dimensional probability density of the positions of places where the coherence maximum is most often realized is estimated. These estimates can be obtained for the entire history of observations and also in a sliding time window of a given length, which makes it possible to trace the dynamics of changes in time in the coherence field of the earth’s tremor. The entropy of the two-dimensional probability density of places of concentration of maximum values of coherence allows us to distinguish seasonal changes in the structure of the coherence field of GPS noise. To study the temporal dynamics, we use the auxiliary time series of changes in the maximum multiple coherence at 50 reference points located throughout the study area. The study of the coherence properties of this auxiliary 50-dimensional time series (“secondary coherence”) in a 180-day sliding time window highlighted a series of synchronization bursts of earth’s surface tremors.

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Acknowledgements

The author is grateful to the Nevada Geodetic Laboratory, University of Nevada, Reno, for providing free access to three-component GPS time series with sampling time step 5 min from the global network all over the world. This work was supported by the Russian Foundation for Basic Research, Project No. 18-05-00133 “Estimation of fluctuations of seismic hazard on the basis of complex analysis of the Earth’s ambient noise.”

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Correspondence to Alexey Lyubushin.

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Lyubushin, A. Field of coherence of GPS-measured earth tremors. GPS Solut 23, 120 (2019). https://doi.org/10.1007/s10291-019-0909-0

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  • DOI: https://doi.org/10.1007/s10291-019-0909-0

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