Event Response to the July 2019 Ridgecrest Earthquake Sequence

Dynamic displacement signals from these earthquakes were recorded by NOTA GNSS stations streaming high-rate (1-sps / 1 Hz) data in real time. These data allowed peak ground displacements (PGDs) to be calculated automatically from the displacement traces within seconds of the earthquake, as the surface waves propagated away from the epicenter.

For the M6.4 2019-07-04 event, the nearest station (P595) recorded a PGD of 113 mm. Using inversions from stations out to 100 km of the epicenter, a “geodetic” magnitude of M6.3 was estimated within 30 seconds of the earthquake occurring. This GNSS-only magnitude only slightly underestimated the final known magnitude.

For the M7.1 2019-07-06 event, the nearest station (P595) recorded a PGD of 697 mm, much larger than the projected value of ~410 mm. The next closest site (CCCC) recorded a PGD of 354 mm, similar to the projected value of 360mm. Using inversions from stations out to 200 km of the epicenter, a “geodetic” magnitude of M 6.9 was estimated within 30 seconds of the earthquake occurring. This GNSS data-only magnitude underestimated the final known magnitude, but was more accurate than the preliminary seismic data-only estimate of M6.2 at 30 seconds after origin time.

Note: Figures and findings are preliminary and subject to revision.

For the M6.4 2019-07-04 event, high-rate 5-sps (5 Hz) data are being downloaded from 200+ NOTA stations within ~250 km of the epicenter for a 3-hour time window around the event (± 1.5 hours), as well as 1-sps (1 Hz) data for a 3-day time window (± 1.5 days).

For the M7.1 2019-07-06 event, high-rate 5-sps (5 Hz) data are being downloaded from 700+ NOTA stations within 1,000 km of the epiecenter for a 3-hour time window around the event (± 1.5 hours), as well as 1-sps (1 Hz) data for a 1-day time window (continuing from the 3-day window from the M6.4 download). A map of downloaded stations is provided in Figure 4.

These data will soon be available in RINEX format from the UNAVCO high rate data ftp site.

Coseismic offsets from this event have been estimated by the GAGE GNSS Analysis Centers (Figure 20). Preliminary “rapid” offsets have been tabulated and published in an event (*.EVT) file available from the UNAVCO event data products ftp site. As more data and final orbits become available, the ACC will also produce a “final” offset solution, as well as offsets estimated from Kalman filter time series analyses. The final event file will be added to the event data products ftp site. The Kalman filter offset solution will be included in the master offset file.

Fully processed 1-sps borehole strainmeter (BSM) datasets for both of these events have been produced. These datasets can be downloaded from the UNAVCO borehole strainmeter event response page. See figures for examples of signals recorded by the BSM network.