MODELING EXTREME-EVENT PRECURSORS WITH THE FRACTIONAL DIFFUSION EQUATION

被引:18
作者
Caputo, Michele [1 ]
Carcione, Jose M. [2 ]
Botelho, Marco A. B. [3 ]
机构
[1] Univ Roma La Sapienza, Dept Phys, I-00185 Rome, Italy
[2] Ist Nazl Oceanog & Geofis Sperimentale OGS, I-34010 Trieste, Italy
[3] Univ Fed Bahia, Inst Geociencias, Salvador, BA, Brazil
关键词
extreme events; precursors; forecast; earthquakes; Omori's law; memory; fractional derivatives; AFTERSHOCKS; CALCULUS; PATTERNS;
D O I
10.1515/fca-2015-0014
中图分类号
O29 [应用数学];
学科分类号
070104 ;
摘要
Extreme catastrophic events such as earthquakes, terrorism and economic collapses are difficult to predict. We propose a tentative mathematical model for the precursors of these events based on a memory formalism and apply it to earthquakes suggesting a physical interpretation. In this case, a precursor can be the anomalous increasing rate of events (aftershocks) following a moderate earthquake, contrary to Omori's law. This trend constitute foreshocks of the main event and can be modelled with fractional time derivatives. A fractional derivative of order 0 < nu < 2 replaces the first-order time derivative in the classical diffusion equation. We obtain the frequency-domain Green's function and the corresponding time-domain solution by performing an inverse Fourier transform. Alternatively, we propose a numerical algorithm, where the time derivative is computed with the Grunwald-Letnikov expansion, which is a finite-difference generalization of the standard finite-difference operator to derivatives of fractional order. The results match the analytical solution obtained from the Green function. The calculation requires to store the whole field in the computer memory since anomalous diffusion "remembers the past".
引用
收藏
页码:208 / 222
页数:15
相关论文
共 43 条
[1]   Solution for a fractional diffusion-wave equation defined in a bounded domain [J].
Agrawal, OP .
NONLINEAR DYNAMICS, 2002, 29 (1-4) :145-155
[2]  
[Anonymous], CRITICAL PHENOMENA N
[3]  
[Anonymous], 2004, LECT NOTES MATH
[4]  
[Anonymous], ACCADEMIA SCI FERRAR
[5]  
[Anonymous], 1996, Journal of Business, Finance & Accounting
[6]  
[Anonymous], STUDIES NONLINEAR DY
[7]  
[Anonymous], P DETC03 CHIC
[8]  
Caputo M., 1977, Annali di Geofisica, V30, P269
[9]   LINEAR MODELS OF DISSIPATION WHOSE Q IS ALMOST FREQUENCY INDEPENDENT-2 [J].
CAPUTO, M .
GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1967, 13 (05) :529-&
[10]   ON THE CURRENT STATE OF LAKE SEDIMENT PALEOMAGNETIC RESEARCH [J].
CREER, KM ;
TUCHOLKA, P .
GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1983, 74 (01) :223-238