Earthquake activity varies spatially and temporally. Seismologists are trying to accurately describe the seismicity using statistical models, and based on these make forecasts of future seismicity. Two basic laws, the Gutenberg Richter law that describes the earthquake size distribution of earthquakes, and the Omori law that describes the decay of aftershock activity are helpful in characterizing the independent and dependent part of the seismicity, respectively. Prediction of earthquakes, however, is currently impossible
Following the 2009 L'Aquila earthquake, the Dipartimento della Protezione Civile Italiana (DPC), app...
Abstract—Our purpose is to analyze the causes of recent failures in earthquake forecasting, as well ...
[1] Assuming that earthquakes are the realization of a stochastic point process and that the magnitu...
While the deterministic prediction of individual earthquakes appears to be an unrealistic goal at pr...
Predicting earthquakes has been a goal of seismology for centuries. In spite of increasing understan...
The answer to the above question depends on the definition of earthquake prediction. We discuss seve...
Predictability of earthquakes has been vigorously debated in the last decades with the dominant -alb...
This chapter focuses on prediction of earthquakes. Because earthquakes occur suddenly, often with de...
International audienceAs part of an effort to develop a systematic methodology for earthquake foreca...
By nature, earthquake prediction is only possible with some statistical uncertainty. Methods are bei...
Frequency–size relation of earthquakes in a region can be approximated by the Gutenberg-Richter law ...
ETAS is currently the most widely accepted state-of-the-art when it comes to time-dependent earthqua...
International audienceWe provide an overview of the basic models of the aftershock processes and adv...
This report reviews two methods of earthquake prediction: statistical analysis and observation of ge...
Following the 2009 L'Aquila earthquake, the Dipartimento della Protezione Civile Italiana (DPC), app...
Following the 2009 L'Aquila earthquake, the Dipartimento della Protezione Civile Italiana (DPC), app...
Abstract—Our purpose is to analyze the causes of recent failures in earthquake forecasting, as well ...
[1] Assuming that earthquakes are the realization of a stochastic point process and that the magnitu...
While the deterministic prediction of individual earthquakes appears to be an unrealistic goal at pr...
Predicting earthquakes has been a goal of seismology for centuries. In spite of increasing understan...
The answer to the above question depends on the definition of earthquake prediction. We discuss seve...
Predictability of earthquakes has been vigorously debated in the last decades with the dominant -alb...
This chapter focuses on prediction of earthquakes. Because earthquakes occur suddenly, often with de...
International audienceAs part of an effort to develop a systematic methodology for earthquake foreca...
By nature, earthquake prediction is only possible with some statistical uncertainty. Methods are bei...
Frequency–size relation of earthquakes in a region can be approximated by the Gutenberg-Richter law ...
ETAS is currently the most widely accepted state-of-the-art when it comes to time-dependent earthqua...
International audienceWe provide an overview of the basic models of the aftershock processes and adv...
This report reviews two methods of earthquake prediction: statistical analysis and observation of ge...
Following the 2009 L'Aquila earthquake, the Dipartimento della Protezione Civile Italiana (DPC), app...
Following the 2009 L'Aquila earthquake, the Dipartimento della Protezione Civile Italiana (DPC), app...
Abstract—Our purpose is to analyze the causes of recent failures in earthquake forecasting, as well ...
[1] Assuming that earthquakes are the realization of a stochastic point process and that the magnitu...