Climate Change Attribution Using Empirical Decomposition of Climatic Data
arXiv:1206.5845 · doi:10.2174/1874282301105010074
Abstract
The climate change attribution problem is addressed using empirical decomposition. Cycles in solar motion and activity of 60 and 20 years were used to develop an empirical model of Earth temperature variations. The model was fit to the Hadley global temperature data up to 1950 (time period before anthropogenic emissions became the dominant forcing mechanism), and then extrapolated from 1951 to 2009. After subtraction of the model, the residuals showed an approximate linear upward trend after 1942. Herein we assume that the residual upward warming observed during the second half of the 20th century has been mostly induced by a worldwide rapid increase of anthropogenic emissions, urbanization and land use change. The warming observed before 1942 is relatively small and it is assumed to have been mostly naturally induced by a climatic recovery since the Little Ice Age of the 17th century and the Dalton Minimum at the beginning of the 19th century. The resulting full natural plus anthropogenic model fits the entire 160 year record very well. Residual analysis does not provide any evidence for a substantial cooling effect due to sulfate aerosols from 1940 to 1970. The cooling observed during that period may be due to a natural 60-year cycle, which is visible in the global temperature since 1850 and has been observed also in numerous multisecular climatic records. New solar activity proxy models are developed that suggest a mechanism for both the 60-year climate cycle and a portion of the long-term warming trend. Our results suggest that because current models underestimate the strength of natural multidecadal cycles in the temperature records, the anthropogenic contribution to climate change since 1970 should be around half of that previously claimed by the IPCC [2007]. A 21st Century forecast suggests that climate may warm less than 1^{\circ}C by 2100.
References in corpus (1)
Cited by in corpus (8)
- Multi-scale harmonic model for solar and climate cyclical variation throughout the Holocene based on Jupiter-Saturn tidal frequencies plus the 11-year solar dynamo cycle
- On the astronomical origin of the Hallstatt oscillation found in radiocarbon and climate records throughout the Holocene
- Multi-scale dynamical analysis (MSDA) of sea level records versus PDO, AMO, and NAO indexes
- Evidences for a quasi 60-year North Atlantic Oscillation since 1700 and its meaning for global climate change
- ACRIM total solar irradiance satellite composite validation versus TSI proxy models
- Discussion on the spectral coherence between planetary, solar and climate oscillations: a reply to some critiques
- Global temperatures and sunspot numbers. Are they related? Yes, but non linearly. A reply to Gil-Alana et al. (2014)
- Comment on "The influence of planetary attractions on the solar tachocline" by Callebaut, de Jager and Duhau