z-logo
open-access-imgOpen Access
Comparative performance of time‐invariant, long‐range and short‐range forecasting models on the earthquake catalogue of Greece
Author(s) -
Console R.,
Rhoades D. A.,
Murru M.,
Evison F. F.,
Papadimitriou E. E.,
Karakostas V. G.
Publication year - 2006
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2005jb004113
Subject(s) - range (aeronautics) , statistic , poisson distribution , induced seismicity , magnitude (astronomy) , scale (ratio) , geology , econometrics , meteorology , statistics , seismology , mathematics , geography , physics , cartography , materials science , composite material , astronomy
Time‐invariant, long‐range, and short‐range forecasting models were fitted to the earthquake catalogue of Greece for magnitudes 4.0 and greater to optimize their ability to forecast events of magnitude 6.0 and greater in the period 1966–1980. The models considered were stationary spatially uniform and spatially varying Poisson models, a long‐range forecasting model based on the precursory scale increase phenomenon with every earthquake regarded as a precursor according to scale, and epidemic type short‐range forecasting models with spatially uniform and spatially varying spontaneous seismicity. Each of the models was then applied to the catalogue for 1981–2002, and their forecasting performance was compared using the log likelihood statistic. The long‐range forecasting model performed substantially better than the time‐invariant models, and the short‐range forecasting models performed substantially better again. The results show that the information value to be gained from modeling temporal and spatial variation of earthquake occurrence rate, at both long and short range, is much greater than can be gained from modeling spatial variation alone.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here