Escalfament global (Catalan Wikipedia)

Analysis of information sources in references of the Wikipedia article "Escalfament global" in Catalan language version.

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aip.org

bbc.co.uk

news.bbc.co.uk

berkeley.edu

atmos.berkeley.edu

campo-nc.us

climate-lab-book.ac.uk

  • Hawkins, Ed. «Warming stripes». Climate Lab Book. [Consulta: 26 maig 2018].

doi.org

dx.doi.org

euractiv.com

europa.eu

register.consilium.europa.eu

fao.org

gencat.cat

canviclimatic.gencat.cat

geology.com

greenpeace.org.uk

grida.no

ipcc.ch

  • 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 p. 690. Intergovernmental Panel on Climate Change, 07-05-2007. Arxivat de l'original el 2018-05-08. [Consulta: 20 maig 2007]. «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 twentieth century, with a small net cooling from the combined effects of solar and volcanic forcings»
  • «Summary for Policymaker» (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. Intergovernmental Panel on Climate Change, 05-02-2007. [Consulta: 2 febrer 2007].

ipsnews.net

mit.edu

web.mit.edu

mongabay.com

news.mongabay.com

nationalpost.com

nih.gov

ncbi.nlm.nih.gov

  • Ammann, Caspar [et al]. «Solar influence on climate during the past millennium: Results from ransient simulations with the NCAR Climate Simulation Model» (PDF). Proceedings of the National Academy of Sciences of the United States of America, 104, 10, 06-04-2007, pàg. 3.713-3.718. DOI: 10.1073/pnas.0605064103. PMID: 17360418. «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.»

pace.edu

pilr.blogs.pace.edu

pik-potsdam.de

pnas.org

  • Ammann, Caspar [et al]. «Solar influence on climate during the past millennium: Results from ransient simulations with the NCAR Climate Simulation Model» (PDF). Proceedings of the National Academy of Sciences of the United States of America, 104, 10, 06-04-2007, pàg. 3.713-3.718. DOI: 10.1073/pnas.0605064103. PMID: 17360418. «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.»

royalsoc.ac.uk

royalsociety.org

sciencemag.org

thaindian.com

thoughtco.com

unfccc.int

usatoday.com

web.archive.org