S43D-2843
Predictability of Great Earthquakes: The 25 April 2015 M7.9 Gorkha (Nepal)

Thursday, 17 December 2015
Poster Hall (Moscone South)
Vladimir G Kossobokov, Institute of Earthquake Prediction Theory and Mathematical Geophysics, Russian Academy of Sciences, Moscow, Russia; International Seismic Safety Organization, Arsita, Italy
Abstract:
Understanding of seismic process in terms of non-linear dynamics of a hierarchical system of blocks-and-faults and deterministic chaos, has already led to reproducible intermediate-term middle-range prediction of the great and significant earthquakes. The technique based on monitoring charcteristics of seismic static in an area proportional to source size of incipient earthquake is confirmed at the confidence level above 99% by statistics of Global Testing in forward application from 1992 to the present. The semi-annual predictions determined for the next half-year by the algorithm M8 aimed (i) at magnitude 8+ earthquakes in 262 circles of investigation, CI’s, each of 667-km radius and (ii) at magnitude 7.5+ earthquakes in 180 CI’s, each of 427-km radius are communicated each January and July to the Global Test Observers (about 150 today). The pre-fixed location of CI’s cover all seismic regions where the M8 algorithm could run in its original version that requires annual rate of activity of 16 or more main shocks.

According to predictions released in January 2015 for the first half of 2015, the 25 April 2015 Nepal MwGCMT = 7.9 earthquake falls outside the Test area for M7.5+, while its epicenter is within the accuracy limits of the alarm area for M8.0+ that spread along 1300 km of Himalayas. We note that (i) the earthquake confirms identification of areas prone to strong earthquakes in Himalayas by pattern recognition (Bhatia et al. 1992) and (ii) it would have been predicted by the modified version of the M8 algorithm aimed at M7.5+. The modified version is adjusted to a low level of earthquake detection, about 10 main shocks per year, and is tested successfully by Mojarab et al. (2015) in application to the recent earthquakes in Eastern Anatolia (23 October 2011, M7.3 Van earthquake) and Iranian Plateau (16 April 2013, M7.7 Saravan and the 24 September 2013, M7.7 Awaran earthquakes).