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Causal inference from cross-sectional earth system data with geographical convergent cross mapping
Bingbo Gao1,2, Jianyu Yang1,2, Ziyue Chen3
1College of Land Science and Technology, China Agricultural University, Beijing, China.
Nature Communications
|September 22, 2023
Summary
This study introduces a Geographical Convergent Cross Mapping (GCCM) model for spatial causal inference. GCCM effectively detects causation in complex systems using spatial data, overcoming limitations of temporal models.
Area of Science:
- Earth System Science
- Complex Systems Analysis
- Spatial Data Science
Background:
- Temporal causation models face limitations with non-time-series or low-variation data, common in Earth systems.
- Existing spatial causation models inadequately explore rich spatial cross-sectional data.
- The generalized embedding theorem suggests causal links between variables within the same dynamic system.
Purpose of the Study:
- To propose a novel Geographical Convergent Cross Mapping (GCCM) model for spatial causal inference.
- To address the limitations of temporal models in Earth system science by utilizing spatial cross-sectional data.
- To develop a method for detecting and characterizing spatial causal relationships in complex systems.
Main Methods:
- Reconstruction of dynamic system state space from observational data.
- Application of cross-mapping prediction within the reconstructed state space.
- Development and testing of the Geographical Convergent Cross Mapping (GCCM) model.
Main Results:
- GCCM successfully detects weak-to-moderate causations even with insignificant correlations.
- The model identifies primary causation direction in strongly coupled variables.
- GCCM overcomes the mirroring effect, revealing bidirectional asymmetric causation.
Conclusions:
- The Geographical Convergent Cross Mapping (GCCM) model offers a robust approach to spatial causal inference.
- GCCM enhances the analysis of complex systems by leveraging spatial cross-sectional data.
- This method provides new insights into causality in Earth systems where temporal data is limited.
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