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Stochastically‐induced dynamics of earthquakes. / Makoveeva, Eugenya v.; Tsvetkov, Ivan n.; Ryashko, Lev b.
In: Mathematical Methods in the Applied Sciences, Vol. 47, No. 8, 30.05.2024, p. 6762-6769.

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Harvard

Makoveeva, EV, Tsvetkov, IN & Ryashko, LB 2024, 'Stochastically‐induced dynamics of earthquakes', Mathematical Methods in the Applied Sciences, vol. 47, no. 8, pp. 6762-6769. https://doi.org/10.1002/mma.8892

APA

Vancouver

Makoveeva EV, Tsvetkov IN, Ryashko LB. Stochastically‐induced dynamics of earthquakes. Mathematical Methods in the Applied Sciences. 2024 May 30;47(8):6762-6769. doi: 10.1002/mma.8892

Author

Makoveeva, Eugenya v. ; Tsvetkov, Ivan n. ; Ryashko, Lev b. / Stochastically‐induced dynamics of earthquakes. In: Mathematical Methods in the Applied Sciences. 2024 ; Vol. 47, No. 8. pp. 6762-6769.

BibTeX

@article{5af5409964df4c45b7b308d6e44833dd,
title = "Stochastically‐induced dynamics of earthquakes",
abstract = "Motivated by an important geophysical application, we analyze the nonlinear dynamics of the number of earthquakes per unit time in a given Earth's surface area. At first, we consider a dynamical model of earthquakes describing their rhythmic behavior with time delays. This model comprises different earthquake scenarios divided into three types (A, B, and C) accordingly to various system dynamics. We show that the deterministic system contains stable equilibria and a limit cycle whose size drastically depends on the production rate (Formula presented.) of earthquakes and their time delay effect. As this takes place, the frequency of earthquakes possesses an oscillatory behavior dependent on (Formula presented.). To study the role of (Formula presented.) in more detail, we have introduced a white Gaussian noise in the governing equation. First of all, we have shown that the dynamical system is stochastically excitable, that is, it excites larger-amplitude noise-induced fluctuations in the frequency of earthquakes. In addition, these large-amplitude stochastic fluctuations can alternate with small-amplitude fluctuations over time. In other words, the frequency of earthquakes can change its amplitude in an irregular manner under the influence of white noise. Another important effect is how close the current value of (Formula presented.) is to its bifurcation point. The closer this value is, the less noise generates large-amplitude fluctuations in the earthquake frequency. ",
author = "Makoveeva, {Eugenya v.} and Tsvetkov, {Ivan n.} and Ryashko, {Lev b.}",
note = "This work was supported by the Ministry of Science and Higher Education of the Russian Federation (project no. FEUZ‐2021‐0014).",
year = "2024",
month = may,
day = "30",
doi = "10.1002/mma.8892",
language = "English",
volume = "47",
pages = "6762--6769",
journal = "Mathematical Methods in the Applied Sciences",
issn = "0170-4214",
publisher = "John Wiley & Sons Inc.",
number = "8",

}

RIS

TY - JOUR

T1 - Stochastically‐induced dynamics of earthquakes

AU - Makoveeva, Eugenya v.

AU - Tsvetkov, Ivan n.

AU - Ryashko, Lev b.

N1 - This work was supported by the Ministry of Science and Higher Education of the Russian Federation (project no. FEUZ‐2021‐0014).

PY - 2024/5/30

Y1 - 2024/5/30

N2 - Motivated by an important geophysical application, we analyze the nonlinear dynamics of the number of earthquakes per unit time in a given Earth's surface area. At first, we consider a dynamical model of earthquakes describing their rhythmic behavior with time delays. This model comprises different earthquake scenarios divided into three types (A, B, and C) accordingly to various system dynamics. We show that the deterministic system contains stable equilibria and a limit cycle whose size drastically depends on the production rate (Formula presented.) of earthquakes and their time delay effect. As this takes place, the frequency of earthquakes possesses an oscillatory behavior dependent on (Formula presented.). To study the role of (Formula presented.) in more detail, we have introduced a white Gaussian noise in the governing equation. First of all, we have shown that the dynamical system is stochastically excitable, that is, it excites larger-amplitude noise-induced fluctuations in the frequency of earthquakes. In addition, these large-amplitude stochastic fluctuations can alternate with small-amplitude fluctuations over time. In other words, the frequency of earthquakes can change its amplitude in an irregular manner under the influence of white noise. Another important effect is how close the current value of (Formula presented.) is to its bifurcation point. The closer this value is, the less noise generates large-amplitude fluctuations in the earthquake frequency.

AB - Motivated by an important geophysical application, we analyze the nonlinear dynamics of the number of earthquakes per unit time in a given Earth's surface area. At first, we consider a dynamical model of earthquakes describing their rhythmic behavior with time delays. This model comprises different earthquake scenarios divided into three types (A, B, and C) accordingly to various system dynamics. We show that the deterministic system contains stable equilibria and a limit cycle whose size drastically depends on the production rate (Formula presented.) of earthquakes and their time delay effect. As this takes place, the frequency of earthquakes possesses an oscillatory behavior dependent on (Formula presented.). To study the role of (Formula presented.) in more detail, we have introduced a white Gaussian noise in the governing equation. First of all, we have shown that the dynamical system is stochastically excitable, that is, it excites larger-amplitude noise-induced fluctuations in the frequency of earthquakes. In addition, these large-amplitude stochastic fluctuations can alternate with small-amplitude fluctuations over time. In other words, the frequency of earthquakes can change its amplitude in an irregular manner under the influence of white noise. Another important effect is how close the current value of (Formula presented.) is to its bifurcation point. The closer this value is, the less noise generates large-amplitude fluctuations in the earthquake frequency.

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U2 - 10.1002/mma.8892

DO - 10.1002/mma.8892

M3 - Conference article

VL - 47

SP - 6762

EP - 6769

JO - Mathematical Methods in the Applied Sciences

JF - Mathematical Methods in the Applied Sciences

SN - 0170-4214

IS - 8

ER -

ID: 56640164