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In the new study, Grilli and colleagues worked back from details of the ocean surface motion recorded by gauges along the Japanese shore on the day of the earthquake.
Interseismic landward motion recorded by continuous GPS above subduction zones is interpreted as the accumulation of elastic stress that is subsequently released either by true seismic events or by slow earthquakes (Dragert et al. 2001).
Borja et al. [6] developed a fully nonlinear finite-element model to investigate the impact of hysteretic and viscous material behavior on the down-hole motion recorded by an array at a large-scale seismic test site in Lotung, Taiwan during an earthquake event.
The dynein motors were made to carry a smaller polystyrene bead as cargo, and the movement of this smaller bead was tracked using a computer algorithm to interpret the motion recorded by a microscope.
In the present work we have compared the rib cage motion recorded by surface sensors with the changes in diaphragm activity registered by sonomicrometry, transdiaphragmatic pressure and airflow recorded in dogs during spontaneous and inspiratory load breathing.
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The quake-generated ground motions recorded by seismometers contain large amounts of information about how earthquakes unfold.
The stations employed and the epicenters of the events studied are plotted in Figure 2. Figure 3 shows examples of three-component seismograms of transverse (T), radial (R), and vertical (Z) component ground motions recorded by the Hi-net stations.
Fig. 2. Waveforms and particle motions recorded by the KR07 station (location in Fig. 1) filtered in the 2 3 Hz band for the beginning part of the explosive event at 23:19 JST on 1 February, 2011.
This result may be due to the reduced precision of the Swaymeter (1 mm), the dampening of body motion through the Swaymeter and pen-paper interface friction, and the higher frequency motions recorded by the forceplate system.
The analysis employs strong motion data recorded by the Japanese Digital Strong-Motion Seismograph Network KiK-Net operated by National Research Institute for Earth Science and Disaster Prevention (Aoi et al., 2000).
Here we conduct a follow-up study of Wu and Peng (2011) utilizing the newly available strong motion data recorded by the Japanese Digital Strong-Motion Seismograph Network KiK-Net from 15 months before to 5 months after the Tohoku main shock.
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