马尔科夫分析和兰杰文方程的地球表面温度数据
Maedeh Lak1, Sakineh Hosseinabadi2, Amir Ali Masoudi3
1Department of Condensed Matter Physics, Faculty of Physics, Alzahra University, Tehran, Iran.
Scientific reports
|August 11, 2025
概括
马尔科夫分析显示,地球是地球.
科学领域:
- 气候科学 气候科学
- 非线性动力学是一种非线性动力学.
- 统计物理 统计物理
背景情况:
- 气候变化是由非线性温度波动驱动的.
- 传统方法难以处理复杂的,非线性气候数据.
- 需要新的方法来理解地球的温度动态.
研究的目的:
- 为了研究地球表面温度的非线性动态.
- 将马尔科夫分析应用于NASA GISS温度数据.
- 为了推导出捕捉温度波动动态的方程.
主要方法:
- 在 NASA GISS 的温度数据中应用马尔科夫分析.
- 通过查普曼-科尔莫戈罗夫 (CK) 验证验证了马科维亚的性质.
- 导出福克-普朗克和朗格文等式来计算温度波动.
主要成果:
- 温度波动在 > 2 个月的间隔内表现出马科维行为.
- 导出福克-普朗克方程与线性漂移和二次扩散系数.
- 在更高的温度下发现了不断增加的随机波动,这表明了多相关性.
结论:
- 马尔科夫分析为了解气候温度动态提供了一个强大的框架.
- 导出方程提供了对非线性温度波动的理论见解.
- 这些发现促进了气候研究的发展,并带来了潜在的实际应用.
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