Changing Probabilities: The M7.7 Canada- M7.5 Alaska Earthquakes

The figure below shows the time-dependent changes in spatial forecast contours associated with the M7.7 Prince Rupert, Canada (10/27/2012) - M7.5 Craig, Alaska (1/5/2013) earthquake sequence. The Prince Rupert earthquake was an oblique-thrust (compressional) event, whereas the Craig earthquake was a right lateral strike (horizontal) slip event. Of concern, the forecast contours representing chance of an earthquake correspond to a higher probability down towards the southeast, nearer to Vancouver and Seattle. Those areas are the locations where the seismic phenomenon of Episodic Tremor and Slip (ETS) was first observed [1].
The latest forecast contours do not as yet include the influence of the Craig, Alaska earthquake and its aftershocks. The reason is that the real-time feed from the USGS is not incorporated into the ANSS catalog (from which we compute the forecast contours) until a day or two later. So while we presently compute near real-time forecast changes, true real-time forecasts are not currently displayed. We are currently working on a method to incorporate the real-time feed into the forecasts so that real-time forecasts will be displayed as the events occur.
[1] http://en.wikipedia.org/wiki/Episodic_tremor_and_slip
Keywords:
Earthquake Forecasting, Earthquakes, Faults, Plate Tectonics
About OpenHazards Bloggers
Steven Ward is a Research Geophysicist at
the Institute of Geophysics and Planetary Physics, UC Santa Cruz. He specializes in the quantification and simulation of
natural hazards. Read Steve's blog.
John Rundle is a Distinguished Professor of Physics
and Geology at UC Davis and
the Executive Director of the APEC Collaboration for Earthquake Simulations. He
chaired the Board of Advisors for the Southern California Earthquake Center from 1994 to 1996. Read John's blog.