IPCC Fifth Assessment Report

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Average IPCC AR5 climate model projections for 2081-2100 relative to 1986-2005, under low and high emission scenarios Projected Change in Temperatures.svg
Average IPCC AR5 climate model projections for 2081–2100 relative to 1986–2005, under low and high emission scenarios

The Fifth Assessment Report (AR5) of the United Nations Intergovernmental Panel on Climate Change (IPCC) is the fifth in a series of such reports and was completed in 2014. [1] As had been the case in the past, the outline of the AR5 was developed through a scoping process which involved climate change experts from all relevant disciplines and users of IPCC reports, in particular representatives from governments. Governments and organizations involved in the Fourth Report were asked to submit comments and observations in writing with the submissions analysed by the panel. [2] [3] Projections in AR5 are based on "Representative Concentration Pathways" (RCPs). [4] The RCPs are consistent with a wide range of possible changes in future anthropogenic greenhouse gas emissions. Projected changes in global mean surface temperature and sea level are given in the main RCP article.

Contents

The IPCC Fifth Assessment Report followed the same general format as the Fourth Assessment Report, with three Working Group reports and a Synthesis report. [5] [1] The report was delivered in stages, starting with the report from Working Group I in September 2013. [5] It reported on the physical science basis, based on 9,200 peer-reviewed studies. [6] [7] The Synthesis Report was released on 2 November 2014, [8] in time to pave the way for negotiations on reducing carbon emissions at the UN Climate Change Conference in Paris during late 2015.

The report's Summary for Policymakers stated that warming of the climate system is 'unequivocal' with changes unprecedented over decades to millennia, including warming of the atmosphere and oceans, loss of snow and ice, and sea level rise. Greenhouse gas emissions, driven largely by economic and population growth, have led to greenhouse gas concentrations that are unprecedented in at least the last 800,000 years. These, together with other anthropogenic drivers, are "extremely likely" (where that means more than 95% probability) to have been the dominant cause of the observed global warming since the mid-20th century. [9]

Conclusions of the fifth assessment report are summarized below:

Current status

Global Emissions by Economic Sector 1 ipcc 5th report economic sector impact on environment en.svg
Global Emissions by Economic Sector

The Fifth Assessment Report (AR5) consists of three Working Group (WG) Reports and a Synthesis Report. The first Working Group Report was published in 2013 and the rest were completed in 2014. The summaries for policy makers were released on 27 September 2013 for the first report, [19] on 31 March 2014 for the second report entitled "Impacts, Adaptation, and Vulnerability", [20] and on 14 April 2014 for the third report entitled "Mitigation of Climate Change". [21]

The AR5 provides an update of knowledge on the scientific, technical and socio-economic aspects of climate change.

More than 800 authors, selected from around 3,000 nominations, were involved in writing the report. Lead authors' meetings and a number of workshops and expert meetings, in support of the assessment process, were held. A schedule of AR5 related meetings, review periods, and other important dates was published. [22]

A key statement of the report was that: [9]

Continued emission of greenhouse gases will cause further warming and long-lasting changes in all components of the climate system, increasing the likelihood of severe, pervasive and irreversible impacts for people and ecosystems. Limiting climate change would require substantial and sustained reductions in greenhouse gas emissions which, together with adaptation, can limit climate change risks.

Authors and editors

The IPCC was established in 1988 by the World Meteorological Organization (WMO) and the United Nations Environment Programme (UNEP) to assess scientific, technical and socio-economic information concerning climate change, its potential effects and options for adaptation and mitigation.

In March 2010, the IPCC received approximately 3,000 author nominations from experts around the world. At the bureau session held in Geneva, 19–20 May 2010, the three working groups presented their selected authors and review editors for the AR5. Each of the selected scientists, specialists and experts was nominated in accordance with IPCC procedures, by respective national IPCC focal-points, by approved observer organizations, or by the bureau. The IPCC received 50% more nominations of experts to participate in AR5 than it did for AR4. A total of 559 authors and review editors had been selected for AR4 from 2,000 proposed nominees. On 23 June 2010 the IPCC announced the release of the final list of selected coordinating lead authors, comprising 831 experts who were drawn from fields including meteorology, physics, oceanography, statistics, engineering, ecology, social sciences and economics. In comparison to the Fourth Assessment Report (AR4), participation from developing countries was increased, reflecting the ongoing efforts to improve regional coverage in the AR5. About 30% of authors came from developing countries or economies in transition. More than 60% of the experts chosen were new to the IPCC process, bringing fresh knowledge and perspectives.

Climate change 2013: report overview

On 23 June 2010, the IPCC announced the release of the final list of selected coordinating lead authors, comprising 831 experts. The working group reports would be published during 2013 and 2014. These experts would also provide contributions to the Synthesis Report published in late 2014. [23]

The Fifth Assessment Report (Climate Change 2013) would be released in four distinct sections:

Working group I contribution

The full text of Climate Change 2013: The Physical Science Basis was released in an unedited form on Monday, 30 September 2013. It was over 2,000 pages long and cited 9,200 scientific publications. [24] The full, edited report was released online in January 2014 and published in physical form by Cambridge University Press later in the year. [25]

Summary for Policymakers

A concise overview of Working Group I's findings was published as the Summary for Policymakers on 27 September 2013. The level of confidence in each finding was rated on a confidence scale, qualitatively from very low to very high and, where possible, quantitatively from exceptionally unlikely to virtually certain (determined based on statistical analysis and expert judgement). [26]

Likelihood scale used in the report
TermLikelihood of the outcome
Virtually certain99–100 % probability
Extremely likely95–100 % probability
Very likely90–100 % probability
Likely66–100 % probability
More likely than not50–100 % probability
About as likely as not33 to 66% probability
Unlikely0–33 % probability
Very unlikely0–10 % probability
Extremely unlikely0–5 % probability
Exceptionally unlikely0–1 % probability

The principal findings were: [19]

General
  • Warming of the atmosphere and ocean system is unequivocal. Many of the associated impacts such as sea level change (among other metrics) have occurred since 1950 at rates unprecedented in the historical record.
  • There is a clear human influence on the climate
  • It is extremely likely that human influence has been the dominant cause of observed warming since 1950, with the level of confidence having increased since the fourth report.
  • IPCC pointed out that the longer we wait to reduce our emissions, the more expensive it will become. [27]
Historical climate metrics
  • It is likely (with medium confidence) that 1983–2013 was the warmest 30-year period for 1,400 years.
  • It is virtually certain the upper ocean warmed from 1971 to 2010. This ocean warming accounts, with high confidence, for 90% of the energy accumulation between 1971 and 2010.
  • It can be said with high confidence that the Greenland and Antarctic ice sheets have been losing mass in the last two decades and that Arctic sea ice and Northern Hemisphere spring snow cover have continued to decrease in extent.
  • There is high confidence that the sea level rise since the middle of the 19th century has been larger than the mean sea level rise of the prior two millennia.
  • Concentration of greenhouse gases in the atmosphere has increased to levels unprecedented on earth in 800,000 years.
  • Total radiative forcing of the earth system, relative to 1750, is positive and the most significant driver is the increase in CO2's atmospheric concentration.
Models
This video presents projections of 21st century temperature and precipitation patterns based on a buildup of greenhouse gases with a combined effect equivalent to 650ppm of atmospheric CO2, a scenario the IPCC called "RCP4.5". The changes shown compare the model projections to the average temperature and precipitation benchmarks observed from 1971 to 2000.

Climate model simulations in support of AR5 use a different approach to account for increasing greenhouse gas concentrations than in the previous report. Instead of the scenarios from the Special Report on Emissions Scenarios the models are performing simulations for various Representative Concentration Pathways.

AR5 relies on the Coupled Model Intercomparison Project Phase 5 (CMIP5), an international effort among the climate modeling community to coordinate climate change experiments. [28] Most of the CMIP5 and Earth System Model (ESM) simulations for AR5 WRI were performed with prescribed CO2 concentrations reaching 421 ppm (RCP2.6), 538 ppm (RCP4.5), 670 ppm (RCP6.0), and 936 ppm (RCP 8.5) by the year 2100. (IPCC AR5 WGI, page 22).

  • Climate models have improved since the prior report.
  • Model results, along with observations, provide confidence in the magnitude of global warming in response to past and future forcing.
Projections
  • Further warming will continue if emissions of greenhouse gases continue.
  • The global surface temperature increase by the end of the 21st century is likely to exceed 1.5 °C relative to the 1850 to 1900 period for most scenarios, and is likely to exceed 2.0 °C for many scenarios
  • The global water cycle will change, with increases in disparity between wet and dry regions, as well as wet and dry seasons, with some regional exceptions.
  • The oceans will continue to warm, with heat extending to the deep ocean, affecting circulation patterns.
  • Decreases are very likely in Arctic sea ice cover, Northern Hemisphere spring snow cover, and global glacier volume
  • Global mean sea level will continue to rise at a rate very likely to exceed the rate of the past four decades
  • Changes in climate will cause an increase in the rate of CO2 production. Increased uptake by the oceans will increase the acidification of the oceans.
  • Future surface temperatures will be largely determined by cumulative CO2, which means climate change will continue even if CO2 emissions are stopped.

The summary also detailed the range of forecasts for warming, and climate impacts with different emission scenarios. Compared to the previous report, the lower bounds for the sensitivity of the climate system to emissions were slightly lowered, though the projections for global mean temperature rise (compared to pre-industrial levels) by 2100 exceeded 1.5 °C in all scenarios. [29] [30]

In August 2020 scientists reported that observed ice-sheet losses in Greenland and Antarctica track worst-case scenarios of the IPCC Fifth Assessment Report's sea-level rise projections. [31] [32] [33] [34]

Reception

On 14 December 2012, drafts of the Working Group 1 (WG1) report were leaked and posted on the Internet. [35] The release of the summary for policymakers occurred on 27 September 2013. [19] Halldór Thorgeirsson, a UN official, warned that, because big companies are known to fund the undermining of climate science, scientists should be prepared for an increase in negative publicity at the time. "Vested interests are paying for the discrediting of scientists all the time. We need to be ready for that," he said. [36]

Marking the finalization of the Physical Science Basis UN Secretary General Ban Ki-moon addressed the IPCC at Stockholm on 27 September 2013. He stated that "the heat is on. We must act". Jennifer Morgan, from the World Resources Institute, said "Hopefully the IPCC will inspire leadership, from the Mom to the business leader, to the mayor to the head of state." [37] US Secretary of State John Kerry responded to the report saying "This is yet another wakeup call: those who deny the science or choose excuses over action are playing with fire." [38]

Reporting on the publication of the report, The Guardian said that: [39]

In the end it all boils down to risk management. The stronger our efforts to reduce greenhouse gas emissions, the lower the risk of extreme climate impacts. The higher our emissions, the larger climate changes we'll face, which also means more expensive adaptation, more species extinctions, more food and water insecurities, more income losses, more conflicts, and so forth.

The New York Times reported that: [40]

In Washington, President Obama's science adviser, John P. Holdren, cited increased scientific confidence "that the kinds of harm already being experienced from climate change will continue to worsen unless and until comprehensive and vigorous action to reduce emissions is undertaken worldwide."

It went on to say that Ban Ki-moon, the United Nations secretary general, had declared his intention to call a meeting of heads of state in 2014 to develop such a treaty. The last such meeting, in Copenhagen in 2009, the NY Times reported, had ended in disarray. [40]

See also

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References

  1. 1 2 IPCC (2014) The IPCC's Fifth Assessment Report (AR5) leaflet
  2. ↑ "Report of the 31st Session of the IPCC" (PDF). IPCC. Agenda item 3; Annex III. Archived (PDF) from the original on 2023-12-03.
  3. ↑ "Scope, Content and Process for the Preparation of the Synthesis Report (SYR) of the IPCC Fifth Assessment Report (AR5)" (PDF). IPCC.
  4. ↑ Collins, M.; et al. (2013). Climate Change 2013: The Physical Science Basis (Working Group I contribution to the IPCC Fifth Assessment Report). Chapter 12: Long-term Climate Change: Projections, Commitments and Irreversibility (Section 12.3.1.3): Cambridge University Press. pp. 1045–1047. ISBN   978-1-107-66182-0.{{cite book}}: CS1 maint: location (link)
  5. 1 2 IPCC, 2014: Climate Change 2014: Synthesis Report. Contribution of Working Groups I, II and III to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Core Writing Team, R. K. Pachauri and L. A. Meyer (eds.)]. IPCC, Geneva, Switzerland, 151 pp.
  6. ↑ Nesbit, Jeff (2013). "Settled Science".
  7. ↑ Redfearn, Graham (2013-09-27). "IPCC climate change report by numbers". Planet Oz. Guardian.
  8. ↑ "Fossil fuels should be 'phased out by 2100' says IPCC". BBC. 2014-11-02. Retrieved 2014-11-02.
  9. 1 2 "Climate Change 2014 Synthesis Report Summary for Policymakers" (PDF). IPCC. Retrieved 2015-08-01.
  10. ↑ IPCC (11 November 2013): B. Observed Changes in the Climate System, in: Summary for Policymakers, in: IPCC AR5 WG1 2013 , p. 4
  11. ↑ IPCC (11 November 2013): B.5 Carbon and Other Biogeochemical Cycles, in: Summary for Policymakers, in: IPCC AR5 WG1 2013 , p. 11
  12. 1 2 IPCC (11 November 2013): D. Understanding the Climate System and its Recent Changes, in: Summary for Policymakers, in: IPCC AR5 WG1 2013 , p. 15
  13. ↑ IPCC (11 November 2013): Footnote 2, in: Summary for Policymakers , in: IPCC AR5 WG1 2013 , p. 4
  14. 1 2 IPCC (25 June 2014): B-1. Key risks across Sectors and Regions, in: Summary for Policymakers, in:IPCC AR5 WG2 A 2014 , p. 14
  15. ↑ IPCC (25 June 2014):C-1. Principles for Effective Adaptation, in: Summary for Policymakers, in: IPCC AR5 WG2 A 2014 , p. 25
  16. ↑ IPCC: SPM.3 Trends in stocks and flows of greenhouse gases and their drivers, in: Summary for Policymakers, in: IPCC AR5 WG3 2014 , p. 8
  17. ↑ IPCC Victor, D., et al., Executive Summary of Chapter 1: Introductory Chapter, in: Chapter 1: Introductory Chapter, in: IPCC AR5 WG3 2014 , p. 113
  18. ↑ IPCC (2 July 2014): SPM.4.1 Long‐term mitigation pathways, in: Summary for Policymakers, in: IPCC AR5 WG3 2014 , p. 12
  19. 1 2 3 4 "Climate Change 2013: The Physical Science Basis".
  20. ↑ "Threat from global warming heightened in latest U.N. report". Reuters. 2014-03-31. Retrieved 2014-03-31.
  21. ↑ "Climate change report: reactions to the final instalment of the IPCC analysis" in The Guardian
  22. ↑ "Activities: Fifth Assessment report". IPCC. Archived from the original on 2014-05-06. Retrieved 2012-12-15.
  23. ↑ "IPCC website". IPCC. Retrieved 2013-09-27.
  24. ↑ Readfearn, Graham (2013-09-27). "Planet Ozblog badge Previous Blog home IPCC climate change report by numbers". The Guardian. Retrieved 2013-09-27.
  25. ↑ "IPCC PRESS RELEASE" (PDF). IPCC. 2013-09-27. Archived from the original (PDF) on 2014-05-06. Retrieved 2013-10-01.
  26. ↑ M. D. Mastrandrea, C. B. Field, T. F. Stocker, O. Edenhofer, K. L. Ebi, D. J. Frame, H. Held, E. Kriegler, K. J. Mach, P. R. Matschoss, G.-K. Plattner, G. W. Yohe, and F. W. Zwiers, Guidance Note for Lead Authors of the IPCC Fifth Assessment Report on Consistent Treatment of Uncertainties Archived 27 April 2017 at the Wayback Machine , Intergovernmental Panel on Climate Change, 2010.
  27. ↑ Climate dollars and sense – preventing global warming is the cheap option The Guardian 22 April 2014
  28. ↑ "CMIP5 Coupled Model Intercomparison Project". WCRP World Climate Research Programme. Archived from the original on 2009-09-01. Retrieved 2013-10-01.
  29. ↑ McGrath, Matt (2013-09-27). "IPCC climate report: humans 'dominant cause' of warming". BBC News. Retrieved 2013-09-27.
  30. ↑ Gillis, Justin (2013-09-27). "Climate Panel Says Upper Limit on Emissions Is Nearing". New York Times. Retrieved 2013-09-27.
  31. ↑ "Sea level rise from ice sheets track worst-case climate change scenario". phys.org. Retrieved 2020-09-08.
  32. ↑ "Earth's ice sheets tracking worst-case climate scenarios". The Japan Times. 2020-09-01. Archived from the original on 2021-08-02. Retrieved 2020-09-08.
  33. ↑ "Ice sheet melt on track with 'worst-case climate scenario'". www.esa.int. Retrieved 2020-09-08.
  34. ↑ Slater, Thomas; Hogg, Anna E.; Mottram, Ruth (2020-08-31). "Ice-sheet losses track high-end sea-level rise projections". Nature Climate Change. 10 (10): 879–881. Bibcode:2020NatCC..10..879S. doi:10.1038/s41558-020-0893-y. ISSN   1758-6798. S2CID   221381924 . Retrieved 2020-09-08.
  35. ↑ Andrew C. Revkin (2012-12-13). "Leak of Climate Panel Drafts Speaks to Need for New Process". New York Times. Retrieved 2013-02-06.
  36. ↑ Harvey, Fiona; Readfern, Graham (2013-09-20). "Big business funds effort to discredit climate science, warns UN official". The Guardian. Retrieved 2013-09-21.
  37. ↑ Doyle, Alister (2013-09-26). "Climate change stars fade, even if risks rise". Reuters. Retrieved 2016-10-21.
  38. ↑ Harvey, Fiona (2013-09-27). "IPCC climate report: 'the heat is on – we must act'". The Guardian. Retrieved 2013-09-27.
  39. ↑ Nuccitelli, Dana (2014-03-31). "IPCC report warns of future climate change risks, but is spun by contrarians". The Guardian. Retrieved 2015-08-01.
  40. 1 2 "U.N. Climate Panel Endorses Ceiling on Global Emissions". The New York Times. 2013-09-27. Retrieved 2015-08-01.

Sources

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