Implications of the Regional Earthquake Likelihood Models test of earthquake forecasts in California


Published: 13 September 2012
Abstract Views: 2970
PDF: 529
Publisher's note
All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.

Authors

  • Michael Karl Sachs Physics Department, University of California, Davis, CA, United States.
  • Ya-Ting Lee Graduate Institute of Geophysics, National Central University, Jhongli, Taiwan, China.
  • Donald Turcotte Geology Department, University of California, Davis, CA, United States.
  • James R. Holliday Physics Department, University of California, Davis, CA, United States.
  • John B. Rundle Physics Department, University of California, Davis, CA; Geology Department, University of California, Davis, CA; Santa Fe Institute, Santa Fe, NM, United States.
The Regional Earthquake Likelihood Models (RELM) test was the first competitive comparison of prospective earthquake forecasts. The test was carried out over 5 years from 1 January 2006 to 31 December 2010 over a region that included all of California. The test area was divided into 7682 0.1°x0.1° spatial cells. Each submitted forecast gave the predicted numbers of earthquakes Nemi larger than M=4.95 in 0.1 magnitude bins for each cell. In this paper we present a method that separates the forecast of the number of test earthquakes from the forecast of their locations. We first obtain the number Nem of forecast earthquakes in magnitude bin m. We then determine the conditional probability λemi=Nemi/Nem that an earthquake in magnitude bin m will occur in cell i. The summation of λemi over all 7682 cells is unity. A random (no skill) forecast gives equal values of λemi for all spatial cells and magnitude bins. The skill of a forecast, in terms of the location of the earthquakes, is measured by the success in assigning large values of λemi to the cells in which earthquakes occur and low values of λemi to the cells where earthquakes do not occur. Thirty-one test earthquakes occurred in 27 different combinations of spatial cells i and magnitude bins m, we had the highest value of λemi for that mi cell. We evaluate the performance of eleven submitted forecasts in two ways. First, we determine the number of mi cells for which the forecast λemi was the largest, the best forecast is the one with the highest number. Second, we determine the mean value of λemi for the 27 mi cells for each forecast. The best forecast has the highest mean value of λemi. The success of a forecast during the test period is dependent on the allocation of the probabilities λemi between the mi cells, since the sum over the mi cells is unity. We illustrate the forecast distributions of λemi and discuss their differences. We conclude that the RELM test was successful in illustrating the choices required when a forecast of the location of a future earthquake is made.

Supporting Agencies

National Science Council (ROC), Institute of Geophysics (NCU, ROC), NASA

Sachs, M. K., Lee, Y.-T., Turcotte, D., Holliday, J. R., & Rundle, J. B. (2012). Implications of the Regional Earthquake Likelihood Models test of earthquake forecasts in California. Research in Geophysics, 2(2), e10. https://doi.org/10.4081/rg.2012.e10

Downloads

Download data is not yet available.

Citations