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Fig. 3 Earthquake seismic waves detected in Berkeley.

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Presentation on theme: "Fig. 3 Earthquake seismic waves detected in Berkeley."— Presentation transcript:

1 Fig. 3 Earthquake seismic waves detected in Berkeley.
Earthquake seismic waves detected in Berkeley. The atomic gravimeter measures the vertical acceleration of the seismic waves with an update rate of 0.13 Hz. The seismic signal is the vertical channel of the seismometer located in Haviland Hall in the University of California (UC) Berkeley campus. It is in arbitrary unit and has an update rate of 0.1 Hz. Xuejian Wu et al. Sci Adv 2019;5:eaax0800 Copyright © 2019 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).

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