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Updated: Apr 18, 2026

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Detrended partial-cross-correlation analysis: a new method for analyzing correlations in complex system
Naiming Yuan1, Zuntao Fu2, Huan Zhang3
11] Chinese Academy of Meteorological Science, Beijing, 100081, China [2] Department of Geography, Climatology, Climate Dynamics and Climate Change, Justus Liebig University Giessen, Senckenbergstrasse 1, 35390 Giessen, Germany [3] Lab for Climate and Ocean-Atmosphere Studies, Dept. of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, 100871, China.
A new method, detrended partial-cross-correlation analysis (DPCCA), quantifies relations between non-stationary signals by removing external influences. DPCCA reveals significant correlations between climate patterns and Yangtze River rainfall, aiding complex system analysis.
Area of Science:
- Complex Systems Analysis
- Time Series Analysis
- Climate Science
Background:
- Non-stationary signals often exhibit complex interdependencies.
- Existing methods like DCCA may not fully isolate intrinsic relationships due to confounding factors.
Purpose of the Study:
- Introduce detrended partial-cross-correlation analysis (DPCCA) to quantify relationships between two non-stationary signals.
- Remove the influence of other signals to reveal intrinsic correlations.
- Apply DPCCA to climate data to demonstrate its utility in natural complex systems.
Main Methods:
- Developed detrended partial-cross-correlation analysis (DPCCA) by integrating partial-correlation technique into DCCA.
- Conducted numerical tests to validate DPCCA's ability to handle non-stationary signals and isolate intrinsic relationships.
- Applied DPCCA to analyze the influence of Pacific Decadal Oscillation (PDO) and Nino3 Sea Surface Temperature Anomaly (Nino3-SSTA) on Summer Rainfall over the middle-lower reaches of the Yangtze River (SRYR).
Main Results:
- Numerical tests confirmed DPCCA's effectiveness in handling non-stationary signals and identifying intrinsic correlations.
- DPCCA identified significant correlations between SRYR and Nino3-SSTA on 6-8 year time scales (1951-2012).
- DPCCA revealed significant correlations between SRYR and PDO on 35-year time scales.
Conclusions:
- DPCCA is a valuable method for analyzing relationships within complex systems, particularly for non-stationary time series.
- The findings provide new evidence for the influence of PDO and Nino3-SSTA on Yangtze River summer rainfall.
- The method's ability to isolate physically explainable correlations enhances its applicability in environmental and climate research.
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