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Hegerl, Gabriele C.; et al.: Understanding and Attributing Climate Change (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change pp. 690. Intergovernmental Panel on Climate Change, 2007. május 7. [2018. május 8-i dátummal az eredetiből archiválva]. (Hozzáférés: 2007. május 20.) „Recent estimates (Figure 9.9) indicate a relatively small combined effect of natural forcings on the global mean temperature evolution of the seconds half of the 20th century, with a small net cooling from the combined effects of solar and volcanic forcings”
Summary for Policymakers (PDF). Climate Change 2007: Impacts, Adaptation and Vulnerability. Working Group II Contribution to the Intergovernmental Panel on Climate Change Fourth Assessment Report. Intergovernmental Panel on Climate Change, 2007. április 13. [2007. április 21-i dátummal az eredetiből archiválva]. (Hozzáférés: 2007. április 28.)
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McGuffie, K. und A. Henderson-Sellers (2001): Forty Years of Numerical Climate Modelling, in: International Journal of Climatology, Vol. 21 (PDF)
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Ammann, Caspar, Fortunat Joos, David Schimel, Bette Otto-Bliesner, and Robert Tomas (2007. április 25.). „Solar influence on climate during the past millennium: Results from ransient simulations with the NCAR Climate Simulation Model”. Proceedings of the National Academy of Sciences of the United States of America104 (10), 3713-3718. o. „However, because of a lack of interactive ozone, the model cannot fully simulate features discussed in (44)." "While the NH temperatures of the high-scaled experiment are often colder than the lower bound from proxy data, the modeled decadal-scale NH surface temperature for the medium-scaled case falls within the uncertainty range of the available temperature reconstructions. The medium-scaled simulation also broadly reproduces the main features seen in the proxy records." "Without anthropogenic forcing, the 20th century warming is small. The simulations with only natural forcing components included yield an early 20th century peak warming of ≈0.2 °C (≈1950 AD), which is reduced to about half by the end of the century because of increased volcanism.”
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Dlugolecki, Andrew; et al.: Climate Risk to Global Economy (PDF). CEO Briefing: UNEP FI Climate Change Working Group. United Nations Environment Programme, 2002 (Hozzáférés: 2007. április 29.)
Prentice, I., et al. (2001):The Carbon Cycle and Atmospheric Carbon Dioxide, in IPCC 2001: Climate Change 2001: The Scientific Basis (S.185), siehe onlineArchiválva2009. december 7-i dátummal a Wayback Machine-ben
Gemeinsame Stellungnahme der nationalen Wissenschaftsakademien der G8-Länder sowie Brasiliens, Indiens und Chinas (2005): Joint science academies’ statement: Global response to climate change(PDF)Archiválva2007. június 9-i dátummal a Wayback Machine-ben
Muscheler, Raimund, Fortunat Joos, Simon A. Müller und Ian Snowball (2005): How unusual is today’s solar activity?, in: Nature, Vol. 436, 28. Juli, S. E3-E4 (PDF)
Hegerl, Gabriele C.; et al.: Understanding and Attributing Climate Change (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change pp. 690. Intergovernmental Panel on Climate Change, 2007. május 7. [2018. május 8-i dátummal az eredetiből archiválva]. (Hozzáférés: 2007. május 20.) „Recent estimates (Figure 9.9) indicate a relatively small combined effect of natural forcings on the global mean temperature evolution of the seconds half of the 20th century, with a small net cooling from the combined effects of solar and volcanic forcings”
Summary for Policymakers (PDF). Climate Change 2007: Impacts, Adaptation and Vulnerability. Working Group II Contribution to the Intergovernmental Panel on Climate Change Fourth Assessment Report. Intergovernmental Panel on Climate Change, 2007. április 13. [2007. április 21-i dátummal az eredetiből archiválva]. (Hozzáférés: 2007. április 28.)