在多尺度系统中检测时间不可逆转性:在Lorenz96模型中的相关性和响应函数
Niccolò Cocciaglia1,2, Dario Lucente3
1Department of Physics, University of Rome Sapienza, P.le Aldo Moro 2, 00185 Rome, Italy.
Chaos (Woodbury, N.Y.)
|April 8, 2025
概括
统计力学揭示了地质物理模型中的不平衡性质. 扰动对尺度的影响不同,显示方向能量传输和协议依赖的响应.
科学领域:
- 地质物理学 地质物理学
- 统计力学 统计力学
- 动态系统 动态系统
背景情况:
- 多尺度系统在地球物理研究中至关重要.
- 统计力学为分析复杂系统提供了强大的工具.
- 洛伦兹96模型是测试地球物理概念的标准.
研究的目的:
- 描述两个尺度的洛伦兹96模型的非平衡性质.
- 调查能源运输和规模相互作用.
- 评估扰动协议对系统动态的作用.
主要方法:
- 利用了更高阶的相关函数.
- 分析了对外部能量干扰的反应.
- 检查了平衡 (无粘性) 和不平衡 (粘性) 条件.
主要成果:
- 检测到时间逆转对称性破坏,并描述了运输特性.
- 综合变量扰动显著影响负面变量,反向影响微不足道.
- 对扰动的系统响应高度依赖于扰动协议.
结论:
- 统计力学工具对于分析地球物理模型是有效的.
- 洛伦兹96模型中的尺度相互作用表现出明显的不对称性.
- 了解系统动力学需要的不仅仅是观察放松过程.
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