What is linked, what is not
Each arc joins two phenomena tested on this site. Green and animated: clear link (correlation significant at 5 % after correcting for autocorrelation, or a response outside chance in an event study). Grey: inconclusive test. A statistical link alone does not establish causation.
- Clear link
- Inconclusive
Arc width from |r| of the stored result; several tests between the same phenomena are drawn as stacked arcs.
Show the data as a table
Show the data as a table
By cloud level and period
| Clouds (ISCCP-H) | 1983–2017, detrended | 1983–2017, raw | 1983–1994 | 1995–2017 |
|---|---|---|---|---|
| Low (IR) | 0.16 (p = 0.19) | -0.15 | 0.59 (p = 0.00) | -0.29 (p = 0.07) |
| Middle (IR) | -0.06 (p = 0.66) | -0.17 | -0.36 (p = 0.30) | 0.32 (p = 0.00) |
| High (IR) | 0.03 (p = 0.84) | -0.20 | 0.12 (p = 0.65) | 0.16 (p = 0.34) |
| Total cloud amount | 0.07 (p = 0.59) | -0.33 | 0.24 (p = 0.24) | 0.00 (p = 0.98) |
Cosmic-ray flux: monthly mean of the daily counts of the Oulu neutron monitor (months 80 % covered), as a % of the mean. Clouds: global means weighted by cos(latitude) of the ISCCP-H monthly files (NOAA NCEI, 1983–2017), low, middle and high infrared cloud types and total cloud amount. Both series are turned into anomalies (mean of each calendar month removed), then their linear trend is removed: the ISCCP record contains spurious trends due to changes of satellites and viewing angles (Evan et al., 2007).
Lag fixed at 0 in advance (ion nucleation would act within days); curve from −12 to +12 months shown. Bretherton et al. effective size; block bootstrap with 24-month blocks. Same calculation, without detrending as in the original papers, over 1983–1994 (period of the claim) then 1995–2017, and for the other cloud levels.
Computation parameters
{
"lag": "fixed at 0 a priori; curve from −12 to +12 months",
"clouds": "ISCCP-H global means weighted by cos(latitude), IR cloud types (low, middle, high) and total",
"filter": "anomalies from the mean of each calendar month, then linear trend removed (whole period)",
"bootstrap": {
"block": 24,
"draws": 1000
},
"statistic": "pearson",
"subperiods": "to 1995-01 (period of the original claim) and after, anomalies without detrending",
"cosmic_rays": "Oulu neutron monitor, monthly mean of the daily values (months 80 % covered), % from the mean"
}Inputs : oulu.nm.daily (22,811 pts, run #3730) · isccp.cloud.low.monthly (408 pts, run #4304) · isccp.cloud.mid.monthly (408 pts, run #4304) · isccp.cloud.high.monthly (408 pts, run #4304) · isccp.cloud.total.monthly (408 pts, run #4304)
- Oulu neutron monitor, daily corrected count rate (Sodankylä Geophysical Observatory)
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Oulu neutron monitor data, cosmicrays.oulu.fi, Sodankylä Geophysical Observatory of the University of Oulu (6NM64 standard neutron monitor at 65.05° N, 25.47° E, geomagnetic cutoff rigidity ≈ 0.8 GV).
· source page ↗
Licence : Research, educational and public non-commercial use; acknowledge cosmicrays.oulu.fi and the Sodankylä Geophysical Observatory (commercial use: contact the station manager) · retrieved on Oct 25, 2026 · SHA-256 fc2f77ecf31e… - ISCCP-H cloud amount, monthly global means (NOAA NCEI)
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Young, A. H., Knapp, K. R., Inamdar, A., Hankins, W., & Rossow, W. B. (2018). The International Satellite Cloud Climatology Project H-Series climate data record product. Earth System Science Data, 10, 583–593.
· doi:10.5194/essd-10-583-2018 · source page ↗
Licence : U.S. Government work, public domain; cite Young et al. (2018) · retrieved on Oct 26, 2026 · SHA-256 aaaa354f36d0… - Svensmark et al. (1997)
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Svensmark, H., & Friis-Christensen, E. (1997). Variation of cosmic ray flux and global cloud coverage — a missing link in solar-climate relationships. Journal of Atmospheric and Solar-Terrestrial Physics, 59, 1225–1232.
· doi:10.1016/S1364-6826(97)00001-1
Licence : Published literature; cited - Marsh et al. (2000)
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Marsh, N. D., & Svensmark, H. (2000). Low cloud properties influenced by cosmic rays. Physical Review Letters, 85, 5004–5007.
· doi:10.1103/PhysRevLett.85.5004
Licence : Published literature; cited - Sloan et al. (2008)
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Sloan, T., & Wolfendale, A. W. (2008). Testing the proposed causal link between cosmic rays and cloud cover. Environmental Research Letters, 3, 024001.
· doi:10.1088/1748-9326/3/2/024001
Licence : Published literature; cited - Laken et al. (2012)
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Laken, B. A., Pallé, E., Čalogović, J., & Dunne, E. M. (2012). A cosmic ray-climate link and cloud observations. Journal of Space Weather and Space Climate, 2, A18.
· doi:10.1051/swsc/2012018
Licence : Published literature; cited - Dunne (2016)
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Dunne, E. M., et al. (2016). Global atmospheric particle formation from CERN CLOUD measurements. Science, 354, 1119–1124.
· doi:10.1126/science.aaf2649
Licence : Published literature; cited - Evan et al. (2007)
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Evan, A. T., Heidinger, A. K., & Vimont, D. J. (2007). Arguments against a physical long-term trend in global ISCCP cloud amounts. Geophysical Research Letters, 34, L04701.
· doi:10.1029/2006GL028083
Licence : Published literature; cited