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Dynamical evidence for causality between galactic cosmic rays and interannual variation in global temperature.
Anastasios A Tsonis1, Ethan R Deyle2, Robert M May3
1Department of Mathematical Sciences, University of Wisconsin-Milwaukee, Milwaukee, WI 53201; aatsonis@uwm.edu robert.may@zoo.ox.ac.uk gsugihara@ucsd.edu.
Galactic cosmic rays (CR) do not explain 20th-century global warming. However, CR do influence short-term global temperature variability, suggesting a role in climate system dynamics.
Area of Science:
- Climate Science
- Astrophysics
- Atmospheric Physics
Background:
- A 1959 hypothesis suggested solar activity influences climate via galactic cosmic rays (CR).
- Laboratory experiments demonstrate a theoretical mechanism linking CR flux to climate processes.
- The causal relationship between CR and climate remains a subject of scientific debate.
Purpose of the Study:
- To directly investigate the causal link between galactic cosmic rays (CR) and year-to-year global temperature changes.
- To assess the contribution of CR to the 20th-century global warming trend.
- To examine the influence of CR on short-term climate variability.
Main Methods:
- Analysis of observational time series data using convergent cross mapping.
- Direct examination of causal relationships between CR flux and global temperature.
- Statistical assessment of correlations and causal effects on different timescales.
Main Results:
- No measurable causal effect of CR on the overall 20th-century global warming trend was found.
- A significant, though modest, causal effect of CR on short interannual timescales (year-to-year variability) was identified.
- The findings suggest nonlinearities within the climate system influencing the CR-temperature relationship.
Conclusions:
- Galactic cosmic rays do not measurably contribute to the 20th-century global warming trend.
- CR act as a nontraditional forcing on short interannual timescales, influencing global temperature variability.
- The study highlights the complex, nonlinear interactions within the climate system and the potential role of CR in short-term climate dynamics.
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