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A Liang-Kleeman Causality Analysis based on Linear Inverse Modeling

Justin Lien

TL;DR

The paper addresses causal inference in complex stochastic systems by integrating Liang-Kleeman information flow with Linear Inverse Modeling. It formulates a dynamical surrogate $\frac{d}{dt} \mathbf{x} = \mathbf{A} \mathbf{x} + \sqrt{2\mathbf{Q}} \cdot \text{noise}$ and develops White-LIM and Colored-LIM to estimate the linear dynamics $\mathbf{A}$ from data, with the colored-noise extension incorporating memory via an Ornstein-Uhlenbeck process and a tunable correlation time $\boldsymbol{\tau}$. Causality is quantified through $T_{j\to i}$, with $T_{j\to i} = \mathbf{A}_{ij} \frac{\mathbf{C}_{ij}}{\mathbf{C}_{ii}}$ for white noise, and the LIM-based approach enables separating the contributions of dynamics and correlation to causality. Applied to ENSO and IOD using historical climate data, the framework reveals mutual but asymmetric causality, and in the colored-noise case uncovers a Niño 3 region with significant noise memory that enhances information flow, offering deeper insights into global climate interactions and a more realistic causal inference tool for complex systems.

Abstract

Causality analysis is a powerful tool for determining cause-and-effect relationships between variables in a system by quantifying the influence of one variable on another. Despite significant advancements in the field, many existing studies are constrained by their focus on unidirectional causality or Gaussian external forcing, limiting their applicability to complex real-world problems. This study proposes a novel data-driven approach to causality analysis for complex stochastic differential systems, integrating the concepts of Liang-Kleeman information flow and linear inverse modeling. Our method models environmental noise as either memoryless Gaussian white noise or memory-retaining Ornstein-Uhlenbeck colored noise, and allows for self and mutual causality, providing a more realistic representation and interpretation of the underlying system. Moreover, this LIM-based approach can identify the individual contribution of dynamics and correlation to causality. We apply this approach to re-examine the causal relationships between the El Niño-Southern Oscillation (ENSO) and the Indian Ocean Dipole (IOD), two major climate phenomena that significantly influence global climate patterns. In general, regardless of the type of noise used, the causality between ENSO and IOD is mutual but asymmetric, with the causality map reflecting an ENSO-like pattern consistent with previous studies. Notably, in the case of colored noise, the noise memory map reveals a hotspot in the Niño 3 region, which is further related to the information flow. This suggests that our approach offers a more comprehensive framework and provides deeper insights into the causal inference of global climate systems.

A Liang-Kleeman Causality Analysis based on Linear Inverse Modeling

TL;DR

The paper addresses causal inference in complex stochastic systems by integrating Liang-Kleeman information flow with Linear Inverse Modeling. It formulates a dynamical surrogate and develops White-LIM and Colored-LIM to estimate the linear dynamics from data, with the colored-noise extension incorporating memory via an Ornstein-Uhlenbeck process and a tunable correlation time . Causality is quantified through , with for white noise, and the LIM-based approach enables separating the contributions of dynamics and correlation to causality. Applied to ENSO and IOD using historical climate data, the framework reveals mutual but asymmetric causality, and in the colored-noise case uncovers a Niño 3 region with significant noise memory that enhances information flow, offering deeper insights into global climate interactions and a more realistic causal inference tool for complex systems.

Abstract

Causality analysis is a powerful tool for determining cause-and-effect relationships between variables in a system by quantifying the influence of one variable on another. Despite significant advancements in the field, many existing studies are constrained by their focus on unidirectional causality or Gaussian external forcing, limiting their applicability to complex real-world problems. This study proposes a novel data-driven approach to causality analysis for complex stochastic differential systems, integrating the concepts of Liang-Kleeman information flow and linear inverse modeling. Our method models environmental noise as either memoryless Gaussian white noise or memory-retaining Ornstein-Uhlenbeck colored noise, and allows for self and mutual causality, providing a more realistic representation and interpretation of the underlying system. Moreover, this LIM-based approach can identify the individual contribution of dynamics and correlation to causality. We apply this approach to re-examine the causal relationships between the El Niño-Southern Oscillation (ENSO) and the Indian Ocean Dipole (IOD), two major climate phenomena that significantly influence global climate patterns. In general, regardless of the type of noise used, the causality between ENSO and IOD is mutual but asymmetric, with the causality map reflecting an ENSO-like pattern consistent with previous studies. Notably, in the case of colored noise, the noise memory map reveals a hotspot in the Niño 3 region, which is further related to the information flow. This suggests that our approach offers a more comprehensive framework and provides deeper insights into the causal inference of global climate systems.
Paper Structure (9 sections, 9 equations, 2 figures)

This paper contains 9 sections, 9 equations, 2 figures.

Figures (2)

  • Figure 1: The distribution of information flows (unit: nats/months) between DMI and Pacific SSTs computed by LIM-based methods, and Liang's method. The information flows larger than $0.02$ (smaller than $-0.02$) are masked out to $0.02$ (-0.02). The block box specifies the Niño 3 region.
  • Figure 2: The distribution of ${\bm{\tau}}$ (upper panel, unit in months), and $(i,j)$-entry of the observed and theoretical correlation functions (lower panels). The white circles in the upper panel specify the locations from which data is used to compute the correlation functions in the lower panels. The DMI and Pacific SSTs are symbolized by scripts 1, and 2, respectively. The dashed line represents the window over which the minimization is applied. The theoretical correlation function of Liang's method is computed by using Eqs. (\ref{['Eq:IF0']}), (\ref{['Eq:IF1']}), and (\ref{['Eq:bKw']}). The scale of the $y$-axis for SST auto-correlation (${\bf K}_{22}$) in Loc. 2 is significantly larger than others.