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首页> 外文期刊>Physica, A. Statistical mechanics and its applications >Universal approach to overcoming nonstationarity, unsteadiness and non-Markovity of stochastic processes in complex systems
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Universal approach to overcoming nonstationarity, unsteadiness and non-Markovity of stochastic processes in complex systems

机译:克服复杂系统中随机过程的非平稳性,不稳定性和非马尔可夫性的通用方法

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In the present paper, we suggest a new universal approach to study complex systems by microscopic, mesoscopic, and macroscopic methods. We discuss new possibilities of extracting information on nonstationarity, unsteadiness and non-Markovity of discrete stochastic processes in complex systems. We consider statistical properties of the fast, intermediate and slow components of the investigated processes in complex systems within the framework of microscopic, mesoscopic and macroscopic approaches separately. Among them theoretical analysis is carried out by means of local noisy time-dependent parameters and the conception of a quasi-Brownian particle (QBP) (mesoscopic approach) as well as the use of wavelet transformation of the initial row time series. As a concrete example we examine the seismic time series data for strong and weak earthquakes in Turkey (1998, 1999) in detail, as well as technogenic explosions. We propose a new possible solution to the problem of forecasting strong earthquakes. Besides we have found out that an unexpected restoration of the first two local noisy parameters in weak earthquakes and technogenic explosions is determined by exponential law. In this paper we have also carried out the comparison and have discussed the received time dependence of the local parameters for various seismic phenomena. (C) 2004 Elsevier B.V. All rights reserved.
机译:在本文中,我们提出了一种通过微观,介观和宏观方法研究复杂系统的通用方法。我们讨论了提取有关复杂系统中离散随机过程的非平稳性,不稳定性和非马尔可夫性信息的新可能性。我们分别在微观,介观和宏观方法的框架内考虑复杂系统中所研究过程的快速,中间和慢速组件的统计特性。其中,理论分析是通过与局部噪声相关的时间相关参数以及准布朗粒子(QBP)(介观方法)的概念以及初始行时间序列的小波变换来进行的。作为一个具体的例子,我们详细研究了土耳其(1998年,1999年)的强地震和弱地震的地震时间序列数据,以及技术爆炸。我们提出了一种解决强地震预报问题的新方法。此外,我们还发现,在弱地震和技术爆炸中,前两个局部噪声参数的意外恢复是由指数定律确定的。在本文中,我们还进行了比较,并讨论了各种地震现象的局部参数的接收时间依赖性。 (C)2004 Elsevier B.V.保留所有权利。

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