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Multiscale atmospheric dynamics: cross-frequency phase-amplitude coupling in the air temperature
1Department of Nonlinear Dynamics and Complex Systems, Institute of Computer Science, Academy of Sciences of the Czech Republic, Pod vodárenskou věží 2, 182 07 Prague 8, Czech Republic.
European temperature variability is influenced by long-term climate oscillations. Slow climate cycles (6-11 year periods) impact shorter-term temperature fluctuations, causing variations of 1-2°C across Europe.
Area of Science:
- Climate Science
- Data Analysis
- Statistical Physics
Background:
- Understanding climate dynamics across different timescales is crucial for accurate temperature variability analysis.
- European temperature records provide valuable data for studying long-term climate patterns.
Purpose of the Study:
- To investigate interactions between different temporal scales in European surface air temperature data.
- To identify influences of slow oscillatory phenomena on interannual temperature variability.
Main Methods:
- Conditional mutual information was used to detect interactions between temporal scales.
- Fourier-transform and multifractal surrogate data methods were employed for statistical testing.
Main Results:
- Information transfer from larger to smaller time scales was observed.
- The phase of 6-11 year oscillations influences variability amplitudes on scales of months to 4-5 years.
- Slow oscillations affect interannual temperature variability by 1-2°C across large European areas.
Conclusions:
- Long-term climate oscillations significantly impact shorter-term temperature variability in Europe.
- The findings highlight the interconnectedness of climate dynamics across various timescales.
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