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Networks as Renormalized Models for Emergent Behavior in Physical Systems

机译:网络作为物理系统中突发事件的重新规范化模型

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摘要

Networks are paradigms for describing complex biological, social and technological systems. Here I argue that networks provide a coherent framework to construct coarse-grained models for many different physical systems. To elucidate these ideas, I discuss two long-standing problems. The first concerns the structure and dynamics of magnetic fields in the solar corona, as exemplified by sunspots that startled Galileo almost 400 years ago. We discovered that the magnetic structure of the corona embodies a scale free network, with spots at all scales. A network model representing the three-dimensional geometry of magnetic fields, where links rewire and nodes merge when they collide in space, gives quantitative agreement with available data, and suggests new measurements. Seismicity is addressed in terms of relations between events without imposing space-time windows. A metric estimates the correlation between any two earthquakes. Linking strongly correlated pairs, and ignoring pairs with weak correlation organizes the spatio-temporal process into a sparse, directed, weighted network. New scaling laws for seismicity are found. For instance, the aftershock decay rate decreases as 1/t in time up to a correlation time, t[omori]. An estimate from the data gives t[omori] to be about one year for small magnitude 3 earthquakes, about 1400 years for the Landers event, and roughly 26,000 years for the earthquake causing the 2004 Asian tsunami. Our results confirm Kagan's conjecture that aftershocks can rumble on for centuries.
机译:网络是描述复杂的生物,社会和技术系统的范例。在这里,我认为网络提供了一个一致的框架,可以为许多不同的物理系统构建粗粒度模型。为了阐明这些想法,我讨论了两个长期存在的问题。首先是太阳日冕中磁场的结构和动力学,这是近400年前震惊伽利略的黑子所例证的。我们发现电晕的磁性结构体现了无标度网络,在所有标度上都有斑点。代表磁场三维几何形状的网络模型,其中链接重布线和节点在空间碰撞时会合并,并与可用数据达成定量一致性,并提出新的测量方法。地震是通过事件之间的关系来解决的,而没有施加时空窗口。度量标准可估计任意两次地震之间的相关性。链接强相关的对,而忽略弱相关的对,将时空过程组织成一个稀疏,有向,加权的网络。发现了新的地震活动缩放定律。例如,余震衰减率直到相关时间t omo随时间降低1 / t。根据数据估算,小三级地震的tomo约为1年,兰德斯地震的tomo约为1400年,而2004年亚洲海啸的地震的tto约为26,000年。我们的结果证实了卡根的推测,即余震可能持续数百年。

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    Paczuski, M;

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  • 年度 2005
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  • 原文格式 PDF
  • 正文语种 eng
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