ภาวะโลกร้อน (Thai Wikipedia)

Analysis of information sources in references of the Wikipedia article "ภาวะโลกร้อน" in Thai language version.

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  • "Summary for Policymakers" (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. February 5, 2007. สืบค้นเมื่อ 2007-02-02. แนวโน้มใน 100 ปี (1906–2005) ที่ 0.74 องศาเซลเซียส [0.56–0.92 องศาเซลเซียส] ได้มากขึ้นกว่าแนวโน้มที่สอดคล้องของ ปี 1901–2000 ของอุณหภูมิเฉลี่ยที่ 0.6 องศาเซลเซียส [0.4–0.8 องศาเซลเซียส]
  • Hegerl, Gabriele C. (May 7, 2007). "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. Intergovernmental Panel on Climate Change. p. 690. คลังข้อมูลเก่าเก็บจากแหล่งเดิม (PDF)เมื่อ May 8, 2018. สืบค้นเมื่อ 2007-05-20.
  • Forster, Piers (February 5, 2007). "Changes in Atmospheric Constituents and in Radiative Forcing" (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. pp. 188–193. สืบค้นเมื่อ 2007-09-17.
  • "IPCC WG1 AR4 Report — Chapter 1: Historical Overview of Climate Change Science" (PDF). IPCC WG1 AR4 Report. IPCC. 2007. pp. 97 (pdf page 5 of 36). คลังข้อมูลเก่าเก็บจากแหล่งเดิม (PDF)เมื่อ November 26, 2018. สืบค้นเมื่อ 2007-10-07.
  • "Working group I, section 3.2.2.2 of the 2007 IPPC page 243" (PDF). คลังข้อมูลเก่าเก็บจากแหล่งเดิม (PDF)เมื่อ October 23, 2017. สืบค้นเมื่อ 2008-01-30.
  • "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. April 13, 2007. คลังข้อมูลเก่าเก็บจากแหล่งเดิม (PDF)เมื่อ 2018-01-13. สืบค้นเมื่อ 2007-04-28.

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  • Ammann, Caspar (April 6, 2007). "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): 3713–3718. คลังข้อมูลเก่าเก็บจากแหล่งเดิม (PDF)เมื่อ June 24, 2008. สืบค้นเมื่อ 2008-01-20. 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.
  • Hansen, James (September 26, 2006). "Global temperature change" (PDF). PNAS. 103 (39): 14288–14293. doi:10.1073/pnas.060291103. คลังข้อมูลเก่าเก็บจากแหล่งเดิม (PDF)เมื่อ June 4, 2007. สืบค้นเมื่อ 2007-04-20.

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