There are different future climate change scenarios (here shown in terms of global temperatures, on the right), depending on the amount of greenhouse gases emitted and pledges made under the Paris Agreement (on the left); data from 2015.[1][2]


Climate change scenarios or socioeconomic scenarios are projections of future greenhouse gas (GHG) emissions used by analysts to assess future vulnerability to climate change.[3] Scenarios and pathways are created by scientists[4] to survey any long term routes and explore the effectiveness of mitigation and helps us understand what the future may hold. This will allow us to envision the future of human environment system.[4] Producing scenarios requires estimates of future population levels, economic activity, the structure of governance, social values, and patterns of technological change. Economic and energy modelling (such as the World3 or the POLES models) can be used to analyze and quantify the effects of such drivers.

Scientists can develop separate international, regional and national climate change scenarios. These scenarios are designed to help stakeholders understand what kinds of decisions will have meaningful effects on climate change mitigation or adaptation. Most countries developing adaptation plans or Nationally Determined Contributions will commission scenario studies in order to better understand the decisions available to them.

International goals for mitigating climate change through international processes like the Paris Agreement are based on reviews of these scenarios. For example, the Special Report on Global Warming of 1.5 °C was released in 2018 order to reflect more up-to-date models of emissions, Nationally Determined Contributions, and impacts of climate change than its predecessor IPCC Fifth Assessment Report published in 2014 before the Paris Agreement.[5]

Purpose

Climate change scenarios can be thought of as stories of possible futures. They allow the description of factors that are difficult to quantify, such as governance, social structures, and institutions. There is considerable variety among scenarios, ranging from variants of sustainable development, to the collapse of social, economic, and environmental systems.[6]

A baseline scenario is used as a reference for comparison against an alternative scenario, e.g., a mitigation scenario.[7] A wide range of quantitative projections of greenhouse gas emissions have been produced.[8] The "SRES" scenarios are "baseline" emissions scenarios (i.e., they assume that no future efforts are made to limit emissions),[9] and have been frequently used in the scientific literature (see Special Report on Emissions Scenarios for details).

Tools

Shared Socioeconomic Pathways

This section is an excerpt from Shared Socioeconomic Pathways.[edit]
Predicted atmospheric CO₂ concentrations for different shared socioeconomic pathways (SSPs) across the 21st century (projected by MAGICC7, a simple/reduced complexity climate model). Each data point represents an average of simulated values generated from five integrated assessment models.[10]

Shared Socioeconomic Pathways (SSPs) are climate change scenarios of projected socioeconomic global changes up to 2100 as defined in the IPCC Sixth Assessment Report on climate change in 2021.[11] They are used to derive greenhouse gas emissions scenarios with different climate policies.[12][13][14] The SSPs provide narratives describing alternative socio-economic developments. These storylines are a qualitative description of logic relating elements of the narratives to each other.[12] In terms of quantitative elements, they provide data accompanying the scenarios on national population, urbanization and GDP (per capita).[15] The SSPs can be quantified with various Integrated Assessment Models (IAMs) to explore possible future pathways both with regards to socioeconomic and climate pathways.[13][14][15]

The five scenarios are:

  • SSP1: Sustainability ("Taking the Green Road")
  • SSP2: "Middle of the Road"
  • SSP3: Regional Rivalry ("A Rocky Road")
  • SSP4: Inequality ("A Road Divided")
  • SSP5: Fossil-fueled Development ("Taking the Highway") [16]

Representative Concentration Pathway

This section is an excerpt from Representative Concentration Pathway.[edit]
Different RCP scenarios result in different predicted greenhouse gas concentrations in the atmosphere (from 2000 to 2100). RCP8.5 would result in the highest greenhouse gas concentration (measured as CO2-equivalents).

A Representative Concentration Pathway (RCP) is a greenhouse gas concentration (not emissions) trajectory adopted by the IPCC. Four pathways were used for climate modeling and research for the IPCC Fifth Assessment Report (AR5) in 2014. The pathways describe different climate change scenarios, all of which are considered possible depending on the amount of greenhouse gases (GHG) emitted in the years to come. The RCPs – originally RCP2.6, RCP4.5, RCP6, and RCP8.5 – are labelled after a possible range of radiative forcing values in the year 2100 (2.6, 4.5, 6, and 8.5 W/m2, respectively).[17][18][19] The higher values mean higher greenhouse gas emissions and therefore higher global temperatures and more pronounced effects of climate change. The lower RCP values, on the other hand, are more desirable for humans but require more stringent climate change mitigation efforts to achieve them.

A short description of the four RCPs is as follows: RCP 1.9 is a pathway that limits global warming to below 1.5 °C, the aspirational goal of the Paris Agreement.[20] RCP 2.6 is a "very stringent" pathway.[20] RCP 3.4 represents an intermediate pathway between the "very stringent" RCP2.6 and less stringent mitigation efforts associated with RCP4.5.[21] RCP 4.5 is described by the IPCC as an intermediate scenario.[22] In RCP 6, emissions peak around 2080, then decline.[23] RCP7 is a baseline outcome rather than a mitigation target.[20] In RCP 8.5 emissions continue to rise throughout the 21st century.[24]: Figure 2, p. 223 

Since IPCC's Fifth Assessment report the original pathways are being considered together with Shared Socioeconomic Pathways: as are new RCPs such as RCP1.9, RCP3.4 and RCP7.[20]

Factors affecting future GHG emissions

No strong patterns were found in the relationship between economic activity and GHG emissions. Economic growth was found to be compatible with increasing or decreasing GHG emissions. In the latter case, emissions growth is mediated by increased energy efficiency, shifts to non-fossil energy sources, and/or shifts to a post-industrial (service-based) economy.

Factors affecting the emission projections include:

  • Population projections: All other factors being equal, lower population projections result in lower emissions projections.
  • Economic development: Economic activity is a dominant driver of energy demand and thus of GHG emissions.
  • Energy use: Future changes in energy systems are a fundamental determinant of future GHG emissions.
    • Energy intensity: This is the total primary energy supply (TPES) per unit of GDP.[25] In all of the baseline scenarios assessments, energy intensity was projected to improve significantly over the 21st century. The uncertainty range in projected energy intensity was large.[26]
    • Carbon intensity: This is the CO2 emissions per unit of TPES. Compared with other scenarios, Fisher et al. (2007) found that the carbon intensity was more constant in scenarios where no climate policy had been assumed.[26] The uncertainty range in projected carbon intensity was large. At the high end of the range, some scenarios contained the projection that energy technologies without CO2 emissions would become competitive without climate policy. These projections were based on the assumption of increasing fossil fuel prices and rapid technological progress in carbon-free technologies. Scenarios with a low improvement in carbon intensity coincided with scenarios that had a large fossil fuel base, less resistance to coal consumption, or lower technology development rates for fossil-free technologies.
  • Land-use change: Land-use change plays an important role in climate change, impacting on emissions, sequestration and albedo. One of the dominant drivers in land-use change is food demand. Population and economic growth are the most significant drivers of food demand.[27]

In producing scenarios, an important consideration is how social and economic development will progress in developing countries.[26] If, for example, developing countries were to follow a development pathway similar to the current industrialized countries, it could lead to a very large increase in emissions. Emissions do not only depend on the growth rate of the economy. Other factors include the structural changes in the production system, technological patterns in sectors such as energy, geographical distribution of human settlements and urban structures (this affects, for example, transportation requirements), consumption patterns (e.g., housing patterns, leisure activities, etc.), and trade patterns the degree of protectionism and the creation of regional trading blocks can affect availability to technology.

In the majority of studies, the following relationships were found (but are not proof of causation):[6]

  • Rising GHGs: This was associated with scenarios having a growing, post-industrial economy with globalization, mostly with low government intervention and generally high levels of competition. Income equality declined within nations, but there was no clear pattern in social equity or international income equality.
  • Falling GHGs: In some of these scenarios, GDP rose. Other scenarios showed economic activity limited at an ecologically sustainable level. Scenarios with falling emissions had a high level of government intervention in the economy. The majority of scenarios showed increased social equity and income equality within and among nations.

Scenarios for different degrees of mitigation efforts

Scenarios of global greenhouse gas emissions. If all countries achieve their current Paris Agreement pledges, average warming by 2100 will go far beyond the target of the Paris Agreement to keep warming "well below 2°C".

Climate change mitigation scenarios are possible futures in which global warming is reduced by deliberate actions, such as a comprehensive switch to energy sources other than fossil fuels. These are actions that minimize emissions so atmospheric greenhouse gas concentrations are stabilized at levels that restrict the adverse consequences of climate change. Using these scenarios, the examination of the impacts of different carbon prices on an economy is enabled within the framework of different levels of global aspirations.[28]

A typical mitigation scenario is constructed by selecting a long-range target, such as a desired atmospheric concentration of carbon dioxide (CO2), and then fitting the actions to the target, for example by placing a cap on net global and national emissions of greenhouse gases.

An increase of global temperature by more than 2 °C has come to be the majority definition of what would constitute intolerably dangerous climate change with efforts to limit the temperature increase to 1.5 °C above pre-industrial levels per the Paris Agreement. Some climate scientists are increasingly of the opinion that the goal should be a complete restoration of the atmosphere's preindustrial condition, on the grounds that too protracted a deviation from those conditions will produce irreversible changes.

Stabilization wedges

A stabilization wedge is an action which incrementally reduces projected emissions. The name is derived from the triangular shape of the gap between reduced and unreduced emissions trajectories when graphed over time. For example, a reduction in electricity demand due to increased efficiency means that less electricity needs to be generated and thus fewer emissions need to be produced. The term originates in the Stabilization Wedge Game. As a reference unit, a stabilization wedge is equal to the following examples of mitigation initiatives: deployment of two hundred thousand 10 MW wind turbines; completely halting the deforestation and planting of 300 million hectares of trees; the increase in the average energy efficiency of all the world's buildings by 25 percent; or the installation of carbon capture and storage facilities in 800 large coal-fired power plants.[29] Pacala and Socolow proposed in their work, Stabilization Wedges, that seven wedges are required to be delivered by 2050 – at current technologies – to make a significant impact on the mitigation of climate change.[30] There are, however, sources that estimate the need for 14 wedges because Pacala and Socolow's proposal would only stabilize carbon dioxide emissions at current levels but not the atmospheric concentration, which is increasing by more than 2 ppm/year.[29] In 2011, Socolow revised their earlier estimate to nine.[31]

Target levels of CO2

Carbon budget and emission reduction scenarios needed to reach the two-degree target agreed to in the Paris Agreement (without net negative emissions, based on peak emissions)[32]

Contributions to climate change, whether they cool or warm the Earth, are often described in terms of the radiative forcing or imbalance they introduce to the planet's energy budget. Now and in the future, anthropogenic carbon dioxide is believed to be the major component of this forcing, and the contribution of other components is often quantified in terms of "parts-per-million carbon dioxide equivalent" (ppm CO2e), or the increment/decrement in carbon dioxide concentrations which would create a radiative forcing of the same magnitude.

450 ppm

The BLUE scenarios in the IEA's Energy Technology Perspectives publication of 2008 describe pathways to a long-range concentration of 450 ppm. Joseph Romm has sketched how to achieve this target through the application of 14 wedges.[33]

World Energy Outlook 2008, mentioned above, also describes a "450 Policy Scenario", in which extra energy investments to 2030 amount to $9.3 trillion over the Reference Scenario. The scenario also features, after 2020, the participation of major economies such as China and India in a global cap-and-trade scheme initially operating in OECD and European Union countries. Also the less conservative 450 ppm scenario calls for extensive deployment of negative emissions, i.e. the removal of CO2 from the atmosphere. According to the International Energy Agency (IEA) and OECD, "Achieving lower concentration targets (450 ppm) depends significantly on the use of BECCS".[34]

550 ppm

This is the target advocated (as an upper bound) in the Stern Review. As approximately a doubling of CO2 levels relative to preindustrial times, it implies a temperature increase of about three degrees, according to conventional estimates of climate sensitivity. Pacala and Socolow list 15 "wedges", any 7 of which in combination should suffice to keep CO2 levels below 550 ppm.[35]

The International Energy Agency's World Energy Outlook report for 2008 describes a "Reference Scenario" for the world's energy future "which assumes no new government policies beyond those already adopted by mid-2008", and then a "550 Policy Scenario" in which further policies are adopted, a mixture of "cap-and-trade systems, sectoral agreements and national measures". In the Reference Scenario, between 2006 and 2030 the world invests $26.3 trillion in energy-supply infrastructure; in the 550 Policy Scenario, a further $4.1 trillion is spent in this period, mostly on efficiency increases which deliver fuel cost savings of over $7 trillion.[36]

Other greenhouse gases

Greenhouse gas concentrations are aggregated in terms of carbon dioxide equivalent. Some multi-gas mitigation scenarios have been modeled by Meinshausen et al.[37]

This section is an excerpt from Climate change mitigation § Needed emissions cuts.[edit]

The annual "Emissions Gap Report" by UNEP stated in 2022 that it was necessary to almost halve emissions. "To get on track for limiting global warming to 1.5°C, global annual GHG emissions must be reduced by 45 per cent compared with emissions projections under policies currently in place in just eight years, and they must continue to decline rapidly after 2030, to avoid exhausting the limited remaining atmospheric carbon budget."[38]: xvi  The report commented that the world should focus on broad-based economy-wide transformations and not incremental change.[38]: xvi 

In 2022, the Intergovernmental Panel on Climate Change (IPCC) released its Sixth Assessment Report on climate change. It warned that greenhouse gas emissions must peak before 2025 at the latest and decline 43% by 2030 to have a good chance of limiting global warming to 1.5 °C (2.7 °F).[39][40] Or in the words of Secretary-General of the United Nations António Guterres: "Main emitters must drastically cut emissions starting this year".[41]
This section is an excerpt from Climate change mitigation § Pledges.[edit]

Climate Action Tracker described the situation on 9 November 2021 as follows. The global temperature will rise by 2.7 °C by the end of the century with current policies and by 2.9 °C with nationally adopted policies. The temperature will rise by 2.4 °C if countries only implement the pledges for 2030. The rise would be 2.1 °C with the achievement of the long-term targets too. Full achievement of all announced targets would mean the rise in global temperature will peak at 1.9 °C and go down to 1.8 °C by the year 2100.[42] Experts gather information about climate pledges in the Global Climate Action Portal - Nazca. The scientific community is checking their fulfilment.[43]

There has not been a definitive or detailed evaluation of most goals set for 2020. But it appears the world failed to meet most or all international goals set for that year.[44][45]

One update came during the 2021 United Nations Climate Change Conference in Glasgow. The group of researchers running the Climate Action Tracker looked at countries responsible for 85% of greenhouse gas emissions. It found that only four countries or political entities – the EU, UK, Chile and Costa Rica – have published a detailed official policy‑plan that describes the steps to realise 2030 mitigation targets. These four polities are responsible for 6% of global greenhouse gas emissions.[46]

In 2021 the US and EU launched the Global Methane Pledge to cut methane emissions by 30% by 2030. The UK, Argentina, Indonesia, Italy and Mexico joined the initiative. Ghana and Iraq signaled interest in joining. A White House summary of the meeting noted those countries represent six of the top 15 methane emitters globally.[47] Israel also joined the initiative.[48]
This section is an excerpt from Carbon budget § Recent and currently remaining carbon budget.[edit]
Historical (unrestrained) carbon budget: Cumulative contributions to the global carbon budget since 1850 illustrate how source and sink components have been out of balance, causing an approximately 50% rise in atmospheric CO2.[49]
Fossil CO2 emissions: global; territorial; by fuel type (incl cement); per capita[50]

Several organisations provide annual updates to the remaining carbon budget, including the Global Carbon Project, the Mercator Research Institute on Global Commons and Climate Change (MCC)[51] and the CONSTRAIN project.[52] In March 2022, before formal publication of the 'Global Carbon Budget 2021' preprint,[50] scientists reported, based on Carbon Monitor[53] (CM) data, that after COVID-19-pandemic-caused record-level declines in 2020, global CO2 emissions rebounded sharply by 4.8% in 2021, indicating that at the current trajectory, the carbon budget for a ⅔ likelihood for limiting warming to 1.5 °C would be used up within 9.5 years.[54]

In April 2022, the now reviewed and officially published The Global Carbon Budget 2021 concluded that fossil CO2 emissions rebounded[55] from pandemic levels by around +4.8% relative to 2020 emissions – returning to 2019 levels.

It identifies three major issues for improving reliable accuracy of monitoring, shows that China and India surpassed 2019 levels (by 5.7% and 3.2%) while the EU and the US stayed beneath 2019 levels (by 5.3% and 4.5%), quantifies various changes and trends, for the first time provides models' estimates that are linked to the official country GHG inventories reporting, and suggests that the remaining carbon budget at 1. Jan 2022 for a 50% likelihood to limit global warming to 1.5 °C (albeit a temporary exceedence is to be expected) is 120 GtC (420 GtCO2) – or 11 years of 2021 emissions levels.[50]

This does not mean that likely 11 years remain to cut emissions but that if emissions stayed the same, instead of increasing like in 2021, 11 years of constant GHG emissions would be left in the hypothetical scenario that all emissions suddenly ceased in the 12th year. (The 50% likelihood may be describable as a kind of minimum plausible deniability requirement as lower likelihoods would make the 1.5 °C goal "unlikely".) Moreover, other trackers show (or highlight) different amounts of carbon budget left, such as the MCC, which as of May 2022 shows '7 years 1 month left'[51] and different likelihoods have different carbon budgets: a 83% likelihood would mean 6.6 ±0.1 years left (ending in 2028) according to CM data.[54]

In October 2023 a group of researchers updated the carbon budget including the CO2 emitted at 2020-2022 and new findings about the role of reduced presence of polluting particles in the atmosphere.[56] They found we can emit 250 GtCO2 or 6 years of emissions at current level starting from January 2023, for having a 50% chance to stay below 1.5 degrees. For reaching this target humanity will need to zero CO2 emissions by the year 2034. To have a 50% chance of staying below 2 degrees humanity can emit 1220 GtCO2 or 30 years of emissions at current level.[57][58]

Previous predictions

UNEP 2011 synthesis report

The United Nations Environment Programme (UNEP, 2011)[59]: 7  looked at how world emissions might develop out to the year 2020 depending on different policy decisions. To produce their report, UNEP (2011)[59]: 8  convened 55 scientists and experts from 28 scientific groups across 15 countries.

Projections, assuming no new efforts to reduce emissions or based on the "business-as-usual" hypothetical trend,[60] suggested global emissions in 2020 of 56 gigatonnes CO
2-equivalent (GtCO
2-eq), with a range of 55-59 GtCO
2-eq.[59]: 12  In adopting a different baseline where the pledges to the Copenhagen Accord were met in their most ambitious form, the projected global emission by 2020 will still reach the 50 gigatonnes CO
2.[61] Continuing with the current trend, particularly in the case of low-ambition form, there is an expectation of 3° Celsius temperature increase by the end of the century, which is estimated to bring severe environmental, economic, and social consequences.[62]

The report also considered the effect on emissions of policies put forward by UNFCCC Parties to address climate change. Assuming more stringent efforts to limit emissions lead to projected global emissions in 2020 of between 49 and 52 GtCO
2-eq, with a median estimate of 51 GtCO
2-eq.[59]: 12  Assuming less stringent efforts to limit emissions lead to projected global emissions in 2020 of between 53 and 57 GtCO
2-eq, with a median estimate of 55 GtCO
2-eq.[59]: 12 

National climate (change) projections

National climate (change) projections (also termed "national climate scenarios" or "national climate assessments") are specialized regional climate projections, typically produced for and by individual countries. What distinguishes national climate projections from other climate projections is that they are officially signed off by the national government, thereby being the relevant national basis for adaptation planning. Climate projections are commonly produced over several years by countries' national meteorological services or academic institutions working on climate change.

Typically distributed as a single product, climate projections condense information from multiple climate models, using multiple greenhouse gas emission pathways (e.g. Representative Concentration Pathways) to characterize different yet coherent climate futures. Such a product highlights plausible climatic changes through the use of narratives, graphs, maps, and perhaps raw data. Climate projections are often publicly available for policy-makers, public and private decision makers, as well as researchers to undertake further climate impact studies, risk assessments, and climate change adaptation research. The projections are updated every few years, in order to incorporate new scientific insights and improved climate models.

National climate projections form the basis of national climate adaptation and climate resilience plans, which are reported to UNFCCC and used in IPCC assessments.

Design

To explore a wide range of plausible climatic outcomes and to enhance confidence in the projections, national climate change projections are often generated from multiple general circulation models (GCMs). Such climate ensembles can take the form of perturbed physics ensembles (PPE), multi-model ensembles (MME), or initial condition ensembles (ICE).[63] As the spatial resolution of the underlying GCMs is typically quite coarse, the projections are often downscaled, either dynamically using regional climate models (RCMs), or statistically. Some projections include data from areas which are larger than the national boundaries, e.g. to more fully evaluate catchment areas of transboundary rivers. Some countries have also produced more localized projections for smaller administrative areas, e.g. States in the United States, and Länder in Germany.

Various countries have produced their national climate projections with feedback and/or interaction with stakeholders.[64] Such engagement efforts have helped tailoring the climate information to the stakeholders' needs, including the provision of sector-specific climate indicators such as degree-heating days.

Examples

Over 30 countries have reported national climate projections / scenarios in their most recent National Communications to United Nations Framework Convention on Climate Change. Many European governments have also funded national information portals on climate change.[65]

For countries which lack adequate resources to develop their own climate change projections, organisations such as UNDP or FAO have sponsored development of projections and national adaptation programmes (NAPAs).[73][74]

See also

References

  1. ↑ USGCRP. Climate Science Special Report (Report). U.S. Global Change Research Program, Washington, DC. pp. 1–470.
  2. ↑ Fawcett, Allen A.; Iyer, Gokul C.; Clarke, Leon E.; Edmonds, James A.; Hultman, Nathan E.; McJeon, Haewon C.; Rogelj, Joeri; Schuler, Reed; Alsalam, Jameel; Asrar, Ghassem R.; Creason, Jared; Jeong, Minji; McFarland, James; Mundra, Anupriya; Shi, Wenjing (2015-12-04). "Can Paris pledges avert severe climate change?". Science. 350 (6265): 1168–1169. doi:10.1126/science.aad5761. ISSN 0036-8075.
  3. ↑ Carter, T.R.; et al. (2001). "Developing and Applying Scenarios. In: Climate Change 2001: Impacts, Adaptation and Vulnerability. Contribution of Working Group II to the Third Assessment Report of the Intergovernmental Panel on Climate Change [J.J. McCarthy et al. Eds.]". Cambridge University Press, Cambridge, U.K., and New York, N.Y., U.S.A. Archived from the original on 2018-10-05. Retrieved 2010-01-10.
  4. 1 2 "IPCC AR6 WG3 Ch3" (PDF). Archived from the original (PDF) on 2022-12-04. Retrieved 2022-04-05.
  5. ↑ Press release: Special Report on Global Warming of 1.5°C (PDF) (Report). Incheon, Republic of Korea: Intergovernmental Panel on Climate Change (IPCC). 8 October 2018. Retrieved 7 October 2018.
  6. 1 2 Morita, T.; et al. (2001). "Greenhouse Gas Emission Mitigation Scenarios and Implications. In: Climate Change 2001: Mitigation. Contribution of Working Group III to the Third Assessment Report of the Intergovernmental Panel on Climate Change [B. Metz et al. Eds.]". Cambridge University Press, Cambridge, U.K., and New York, N.Y., U.S.A. Archived from the original on 2018-10-05. Retrieved 2010-01-10.
  7. ↑ IPCC (2007c). "Annex. In: Climate Change 2007: Mitigation. Contribution of Working Group III to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [B. Metz et al. Eds.]". Cambridge University Press, Cambridge, U.K., and New York, N.Y., U.S.A. Archived from the original on 2018-10-05. Retrieved 2009-05-20.
  8. ↑ Fisher; et al., "Chapter 3: Issues related to mitigation in the long-term context", Archived copy, Sec. 3.1 Emissions scenarios, archived from the original on 2018-11-16, retrieved 2012-09-08{{citation}}: CS1 maint: archived copy as title (link), in IPCC AR4 WG3 (2007)
  9. ↑ Morita; et al., "Chapter 2, Greenhouse Gas Emission Mitigation Scenarios and Implications", Archived copy, Sec. 2.5.1.1 IPCC Emissions Scenarios and the SRES Process, archived from the original on 2013-07-06, retrieved 2012-09-08{{citation}}: CS1 maint: archived copy as title (link), in IPCC TAR WG3 (2001).
  10. ↑ Meinshausen, M., Nicholls, Z. R. J., Lewis, J., Gidden, M. J., Vogel, E., Freund, M., Beyerle, U., Gessner, C., Nauels, A., Bauer, N., Canadell, J. G., Daniel, J. S., John, A., Krummel, P. B., Luderer, G., Meinshausen, N., Montzka, S. A., Rayner, P. J., Reimann, S., . . . Wang, R. H. J. (2020). The shared socio-economic pathway (SSP) greenhouse gas concentrations and their extensions to 2500. Geoscientific Model Development, 13(8), 3571–3605. https://doi.org/10.5194/gmd-13-3571-2020 Archived 2023-04-16 at the Wayback Machine
  11. ↑ "Climate Change 2021 - The Physical Science Basis" (PDF). ipcc.ch. Archived (PDF) from the original on 13 August 2021. Retrieved 15 August 2021.
  12. 1 2 "Shared Socioeconomic Pathways (SSPs)" (PDF)..
  13. 1 2 Riahi, Keywan; van Vuuren, Detlef P.; Kriegler, Elmar; Edmonds, Jae; O’Neill, Brian C.; Fujimori, Shinichiro; Bauer, Nico; Calvin, Katherine; Dellink, Rob; Fricko, Oliver; Lutz, Wolfgang (2017-01-01). "The Shared Socioeconomic Pathways and their energy, land use, and greenhouse gas emissions implications: An overview". Global Environmental Change. 42: 153–168. doi:10.1016/j.gloenvcha.2016.05.009. hdl:10044/1/78069. ISSN 0959-3780.
  14. 1 2 Rogelj, Joeri; Popp, Alexander; Calvin, Katherine V.; Luderer, Gunnar; Emmerling, Johannes; Gernaat, David; Fujimori, Shinichiro; Strefler, Jessica; Hasegawa, Tomoko; Marangoni, Giacomo; Krey, Volker (2018). "Scenarios towards limiting global mean temperature increase below 1.5 °C". Nature Climate Change. 8 (4): 325–332. Bibcode:2018NatCC...8..325R. doi:10.1038/s41558-018-0091-3. hdl:1874/372779. ISSN 1758-678X. S2CID 56238230. Archived from the original on 2022-04-23. Retrieved 2022-04-23.
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  17. ↑ "Representative Concentration Pathways (RCPs)". IPCC. Retrieved 13 February 2019.
  18. ↑ Richard Moss; et al. (2008). Towards New Scenarios for Analysis of Emissions, Climate Change, Impacts, and Response Strategies (PDF). Geneva: Intergovernmental Panel on Climate Change. p. 132.
  19. ↑ Weyant, John; Azar, Christian; Kainuma, Mikiko; Kejun, Jiang; Nakicenovic, Nebojsa; Shukla, P.R.; La Rovere, Emilio; Yohe, Gary (April 2009). Report of 2.6 Versus 2.9 Watts/m2 RCPP Evaluation Panel (PDF). Geneva, Switzerland: IPCC Secretariat.
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  21. ↑ "Explainer: How 'Shared Socioeconomic Pathways' explore future climate change". Carbon Brief. April 19, 2018.
  22. ↑ "Topic 2: Future changes, risks and impacts". IPCC 5th Assessment Synthesis Report. Box 2.2, figure 1.
  23. ↑ "Socio-Economic Data and Scenarios".
  24. ↑ Meinshausen, Malte; Smith, S. J.; Calvin, K.; Daniel, J. S.; Kainuma, M. L. T.; Lamarque, J-F.; Matsumoto, K.; Montzka, S. A.; Raper, S. C. B.; Riahi, K.; Thomson, A.; Velders, G. J. M.; van Vuuren, D.P. P. (2011). "The RCP greenhouse gas concentrations and their extensions from 1765 to 2300". Climatic Change. 109 (1–2): 213–241. Bibcode:2011ClCh..109..213M. doi:10.1007/s10584-011-0156-z. ISSN 0165-0009.
  25. ↑ Rogner, H.-H.; et al. (2007). "Introduction. In: Climate Change 2007: Mitigation. Contribution of Working Group III to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [B. Metz et al. Eds.]". Cambridge University Press, Cambridge, U.K., and New York, N.Y., U.S.A. Archived from the original on 2018-10-05. Retrieved 2009-05-20.
  26. 1 2 3 Fisher, B.S.; et al. (2007). "Issues related to mitigation in the long term context. In: Climate Change 2007: Mitigation. Contribution of Working Group III to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [B. Metz et al. Eds.]". Cambridge University Press, Cambridge, U.K., and New York, N.Y., U.S.A. Archived from the original on 2018-10-05. Retrieved 2009-05-20.
  27. ↑ Fisher, B.S.; et al. (2007). ""3.2.1.6 Land-use change and land-use management." In [book chapter]: "Issues related to mitigation in the long term context." In [book]: "Climate Change 2007: Mitigation. Contribution of Working Group III to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [B. Metz et al. Eds.]". Print version: Cambridge University Press, Cambridge, U.K., and New York, N.Y., U.S.A.. This version: IPCC website. Archived from the original on 2010-04-25. Retrieved 2010-03-18.
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