Broadband Ground Acceleration (GRNDACC)
Broadband Ground Acceleration is the time-series seismic signal sensed by a strong motion accelerometer within the Broadband Ocean Bottom Seismometer. These seismic signals provide a characterization of seismicity/earthquake activity along tectonic plate boundaries where two key phenomena can occur: large-magnitude subduction zone earthquakes and seismicity associated with migration of melt (magma) beneath the seafloor at underwater volcanoes.
Instrument Classes
The following instrument classes include this data product:
Typical Units
m/s^2
Sampling Regime
Seafloor/Crust