Globális felmelegedés (Hungarian Wikipedia)

Analysis of information sources in references of the Wikipedia article "Globális felmelegedés" in Hungarian language version.

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  • "Warming of the climate system is unequivocal, as is now evident from observations of increases in global average air and ocean temperatures, widespread melting of snow and ice and rising global average sea level." IPCC, Synthesis Report Archiválva 2018. november 2-i dátummal a Wayback Machine-ben, Section 1.1: Observations of climate change Archiválva 2018. augusztus 4-i dátummal a Wayback Machine-ben, in IPCC AR4 SYR 2007.
  • 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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  • J.E. Harries, H.E. Brindley, P.J. Sagoo, R.J. Bantges (2001): Increases in greenhouse forcing inferred from the outgoing longwave radiation spectra of the Earth in 1970 and 1997, in: Nature, Vol. 410, S. 355-357, 15. März, online

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  • Soden, Brian J., Held, Isacc M. (2005. november 1.). „An Assessment of Climate Feedbacks in Coupled Ocean–Atmosphere Models” (PDF). Journal of Climate 19 (14), 3354-3360. o. (Hozzáférés: 2007. április 21.) „Interestingly, the true feedback is consistently weaker than the constant relative humidity value, implying a small but robust reduction in relative humidity in all models on average" "clouds appear to provide a positive feedback in all models” 

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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 America 104 (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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  • Stott, Peter A., Gareth S. Jones und John F.B. Mitchell (2003): Do Models Underestimate the Solar Contribution to Recent Climate Change? In: Journal of Climate, Volume 16, Dezember, S. 4079-4093 (PDF)

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  • Meehl, Gerald A., et al. (2005. március 18.). „How Much More Global Warming and Sea Level Rise”. Science 307 (5716), 1769–1772 10.1126/science.1106663. o. (Hozzáférés: 2007. február 11.)  
  • Siegenthaler, Urs, Thomas F. Stocker, Eric Monnin, Dieter Lüthi, Jakob Schwander, Bernhard Stauffer, Dominique Raynaud, Jean-Marc Barnola, Hubertus Fischer, Valérie Masson-Delmotte und Jean Jouzel (2005): Stable Carbon Cycle–Climate Relationship During the Late Pleistocene, in: Science, Vol. 310, No. 5752, S. 1313 – 1317, 25. November, siehe Abstract online
  • Naomi Oreskes (2004): The Scientific Consensus on Climate Change, in: Science Vol. 306 vom 4. Dezember (korrigiert: 21. Januar 2005) (PDF, 81 KB)

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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.)

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