Calentamiento global (Spanish Wikipedia)

Analysis of information sources in references of the Wikipedia article "Calentamiento global" in Spanish language version.

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  • Clark, P. U., et al. (diciembre de 2008). «Executive Summary». Abrupt Climate Change. A Report by the U.S. Climate Change Science Program and the Subcommittee on Global Change Research (en inglés). Reston, Virginia, EE. UU.: U.S. Geological Survey. , pp. 1-7. Report websiteArchivado el 4 de mayo de 2013 en Wayback Machine.

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  • Granger Morgan, M. (Lead Author), H. Dowlatabadi, M. Henrion, D. Keith, R. Lempert, S. McBride, M. Small y T. Wilbanks (Contributing Authors) (2009). «Non-Technical Summary: BOX NT.1 Summary of Climate Change Basics». Synthesis and Assessment Product 5.2: Best practice approaches for characterizing, communicating, and incorporating scientific uncertainty in decisionmaking. A Report by the U.S. Climate Change Science Program and the Subcommittee on Global Change Research (en inglés). Washington, D.C., EE. UU.: National Oceanic and Atmospheric Administration. p. 11. Consultado el 1 de junio de 2011. 

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  • «Finland is warming faster than the rest of the world». Helsinki Times (en inglés). 15 de enero de 2015. Consultado el 27 de marzo de 2025. «Finland is warming fast – faster than scientists ever predicted and at nearly twice the rate of any other country on Earth – according to new research from the University of Eastern Finland and the Finnish Meteorological Society». 

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  • Aaron M. McCright and Riley E. Dunlap, «Challenging Global Warming as a Social Problem: An Analysis of the Conservative Movement's Counter-Claims», Social Problems (en inglés), noviembre de 2000, Vol. 47 Número 4, pp. 499-522. in JSTOR

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  • United Nations Environment Programme (noviembre de 2010). «Technical summary» (PDF). The Emissions Gap Report: Are the Copenhagen Accord pledges sufficient to limit global warming to 2 °C or 1.5 °C? A preliminary assessment (advance copy) (en inglés). UNEP website. Archivado desde el original el 25 de noviembre de 2010. Consultado el 11 de mayo de 2011. Esta publicación también está disponible en

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  • V. Ramanathan and G. Carmichael, supra note 1, at 221 («... emissions of black carbon are the second strongest contribution to current global warming, after carbon dioxide emissions.») Numerous scientists also calculate that black carbon may be second only to CO2 in its contribution to climate change, including Tami C. Bond & Haolin Sun, Can Reducing Black Carbon Emissions Counteract Global Warming, ENVIRON. SCI. TECHN. (2005), at 5921 («BC is the second or third largest individual warming agent, following carbon dioxide and methane.»); and J. Hansen, A Brighter Future, 53 CLIMATE CHANGE 435 (2002), available at [1]Archivado el 21 de octubre de 2011 en Wayback Machine. Calculating the climate forcing of BC at 1.0±0.5 W/m² Archivado el 21 de octubre de 2011 en Wayback Machine.

event.arc.nasa.gov

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  • ((National Academies of Sciences, Engineering, and Medicine)) (2011). «Synopsis». Climate Stabilization Targets: Emissions, Concentrations, and Impacts over Decades to Millennia. Washington, DC: The National Academies Press. p. 5. ISBN 978-0-309-15176-4. doi:10.17226/12877. «Box SYN-1: Sustained warming could lead to severe impacts». 

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  • Royal Society (13 de abril de 2005). Economic Affairs – Written Evidence. The Economics of Climate Change, the Second Report of the 2005–2006 session, produced by the UK Parliament House of Lords Economics Affairs Select Committee (en inglés). UK Parliament website. Consultado el 9 de julio de 2011.  Este documento también está disponible en formato PDF
  • Royal Society (13 de abril de 2005). Economic Affairs – Written Evidence. The Economics of Climate Change, the Second Report of the 2005–2006 session, produced by the UK Parliament House of Lords Economics Affairs Select Committee (en inglés). UK Parliament website. Consultado el 9 de julio de 2011.  Este documento también está disponible en formato PDF

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  • «Working Group I: The Physical Basis for Climate Change». IPCC. Archivado desde el original el 1 de mayo de 2007. «De nuevas estimaciones de los combinados forzantes radiactivos antropogénicos debido a gases de invernadero, aerosoles, y cambios en el uso de la tierra, siendo extremadamente posibles que las actividades humanas han ejercido una considerable influencia en el calentamiento neto del clima desde 1750.» 

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  • Ramanathan, V., et al. (2008). «Report Summary» (PDF). Atmospheric Brown Clouds: Regional Assessment Report with Focus on Asia (en inglés). United Nations Environment Programme. Archivado desde el original el 18 de julio de 2011. 
  • Ramanathan, V., et al. (2008). «Part III: Global and Future Implications» (PDF). Atmospheric Brown Clouds: Regional Assessment Report with Focus on Asia (en inglés). United Nations Environment Programme. Archivado desde el original el 18 de julio de 2011. 

unep.org

  • United Nations Environment Programme (noviembre de 2010). «Technical summary» (PDF). The Emissions Gap Report: Are the Copenhagen Accord pledges sufficient to limit global warming to 2 °C or 1.5 °C? A preliminary assessment (advance copy) (en inglés). UNEP website. Archivado desde el original el 25 de noviembre de 2010. Consultado el 11 de mayo de 2011. Esta publicación también está disponible en

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  • Saar Haas; Yaron Druckman (11 de enero de 2021). «Israel warming up almost twice as fast as rest of world, data shows». Ynet (en inglés). Consultado el 27 de marzo de 2025. «data from the Israeli environmental bodies reveals that Israel is warming up almost twice as fast as the rest of the world. Data collected by Israel Meteorological Service (IMS) and Knesset Research and Information Center shows the changes in the Israeli climate since the 1950s».