What is the Paris Agreement Long-Term Temperature Goal?
The Long-Term Temperature Goal of the Paris Agreement is one goal, establishing 1.5°C global mean temperature rise above pre-industrial levels as the long-term warming limit, which caters for two interpretations:
- establishing a 1.5°C limit that should not be exceeded, or
- allowing for a temporarily exceedance (overshoot) of the 1.5°C limit, whilst requiring warming should always remain “well below 2°C”.
In the latter case, the Long-Term Temperature Goal requires the continuous pursuit of efforts towards 1.5°C, whilst holding warming well below 2°C. This means unambiguously that peak warming must be “well below 2°C” and that there is an obligation to reduce global mean temperatures below 1.5°C in the case of a temporary overshoot.
The view that there are two temperature limits, an upper and a lower, embedded in the Paris Agreement’s Long-Term Temperature Goal is a misunderstanding. Specifically, the decoupling of the 1.5°C warming limit from the “hold warming well below 2°C” element of the Paris Agreement’s temperature goal language to create the sense that there is an upper and lower limit to ‘choose from’ in the Paris Agreement is incorrect. There is just the one goal.
The Paris Agreement’s Long-Term Temperature Goal is an operationalisation of the ultimate objective of the UNFCCC, which is to prevent dangerous anthropogenic interference with the climate system. It is meant to enhance “the implementation of the Convention, including its objective”, which is important and relevant to understanding its meaning in practical terms.
It is important to note that the Temperature Goal in the Paris Agreement does not speak to stabilisation of temperatures, but rather presents upper limits for warming. The question of temperature stabilisation was deliberately not addressed or included anywhere in the Paris Agreement.
Achieving the Paris Agreement goals would mean that temperatures decline again after peak 21st century levels. These declining temperatures are essential for reducing the long-term impacts of climate change such as ocean acidification (via reducing CO2 concentrations), sea level rise, as well as reducing the risk of triggering tipping points of the earth system. Ocean acidification is an important and potentially dangerous interference with the climate system.
How to interpret “holding warming to well below 2°C”?
Holding warming to “well below 2°C” is best understood as having a 90% or higher chance of limiting warming to 2°C, or as being “very likely” in IPCC terminology. This is in line with emission pathways that have a 33-66% chance (or are ‘as likely as not’) to limit warming to 1.5°C.
The use of “well below 2°C” in the Paris Agreement is a significant strengthening of previous “below 2°C” language, adopted at the 2010 climate summit in Cancun. The science that informed the adoption of the Paris Agreement was the IPCC Fifth Assessment Report (AR5). In the AR5, and the wider scientific literature that fed into it, the “below 2°C” Cancun language was identified as having only a 66% probability of staying below 2°C (this translates as “likely” in IPCC terminology). Crucially, these “below 2°C” pathways have about an 80% probability of exceeding 1.5°C. Therefore, the former goal of holding warming below 2°C cannot be considered Paris Agreement compatible.
Pathways consistent with holding warming below 2°C would show an average peak warming of 1.8°C. There would be a 33% probability of exceeding 2°C of warming under these pathways. It is important to highlight that in some literature, the “well below 2°C” limit is interpreted simply in terms of a temperature difference (for example, a limit to an average warming of 1.7°C or 1.8°C).
Pathways with a 66% chance of limiting warming to 1.8°C have been assessed in the 2020 UNEP Gap Report. Such pathways still have a higher than 10% chance of exceeding 2°C and are likely to exceed 1.5°C. A classification of such pathways as “well below 2°C” pathways is therefore questionable.
How does the Temperature Goal relate to the Mitigation Goal?
In addition to the Long-Term Temperature goal, the Paris Agreement also sets a mitigation goal in Article 4.1. The Temperature Goal sets the objective of the Paris Agreement and establishes 1.5°C as the long-term warming limit and Article 4.1 is designed to operationalise the Temperature Goal goal in terms of a global emissions pathway based upon the best available science.
The elements of the Mitigation Goal are to peak emissions as soon as possible, rapidly reduce thereafter and achieve net zero greenhouse gas emissions in the second half of the century. The timing and rate of reductions are to be achieved based on the best available science consistent with meeting the Long-Term Temperature Goal.
In order to provide scientific guidance on these key issues, the UNFCCC requested the IPCC to prepare the Special Report on Global Warming of 1.5°C. Concluded in 2018, this report provides an assessment and mitigation benchmarks for pathways that are “as likely as not” (between 33% and 66% chance) to limit warming to 1.5°C. These pathways are in the ‘low or no overshoot’ pathway category. These ‘low or no overshoot’ pathways provide a “very likely” (>90%) chance to hold warming to “well below 2°C”. We consider emission pathways with these characteristics compatible with the Paris Agreement.
The Sixth Assessment Report of the IPCC Working Group I (IPCC AR6 WGI) did not systematically assess different emission pathways – this will be done in the forthcoming Working Group III report of the IPCC AR6. The WGI report nevertheless confirmed key findings on 1.5°C pathways from the IPCC Special Report on 1.5°C, and assesses an even higher chance of ‘low or no overshoot’ pathways to hold warming to “well below 2°C”.
How does the 1.5°C Temperature Goal relate to achieving net zero greenhouse gas emissions?
Limiting warming to 1.5°C implies reaching net zero CO2 emissions globally around 2050 with deep reductions in emissions of non-CO2 greenhouse gases, particularly methane. Achieving net zero for all greenhouse gas emissions, as set out in Article 4.1 of the Paris Agreement, will need to happen in the second half of the 21st century. This requires net negative CO2 emissions, or CO2 removal to compensate for emissions of non-CO2 gases considered difficult to fully eliminate, such as methane from farming activities.
These timings are linked to meeting the Long-Term Temperature Goal in accordance with the best available science.
A long-term temperature decline would follow from sustained net zero greenhouse gas emissions, in line with pursuing efforts to limit warming to 1.5°C in case of a temperature overshoot. Such a temperature decline from peak 21st century levels is essential to reducing the long-term impacts of climate change such as ocean acidification (via reducing CO2 concentrations), sea level rise as well as reducing the risk of triggering tipping points of the earth system.
What science has informed the adoption of the Paris Agreement goals?
The IPCC AR5 provided the ‘best available science’ at the time of the Paris Agreement and informed the assessment of climate impacts at different temperature levels that underlies the Temperature Goal.
The Temperature Goal is also explicitly linked to assessments of the risks and impacts of climate change undertaken by the UNFCCC’s 2013-2015 Periodic Review, which looked at the adequacy of the previous long-term goal of holding warming below 2°C. The Review concluded that the “guardrail” concept, where up to 2°C of warming was considered safe, was inadequate and should rather be seen as an upper limit – a line that needs to be stringently defended – and that efforts should be made to “push the defense line as low as possible,” noting that a warming limit of 1.5 °C would come closer to a “safer guardrail.”
Based on their assessment of the science as reflected in the Periodic Review, governments decided in Paris, 2015, that the long-term goal of the UNFCCC should be strengthened (see decision 10/CP.21). The impact assessment underlying the adoption of the Temperature Goal is therefore well-linked to the “best available science” at the time, i.e. as reflected in the IPCC AR5, and metrics and approaches used.
How do the revised estimates of historical warming in the AR6 report affect the Temperature Goal?
The IPCC Fifth Assessment Report (AR5) assessment used observed estimates based on the HadCRUT4 dataset for the historic warming that was assessed as 0.6°C between the 1850-1900 and 1986-2005 periods. Future impacts of climate change were assessed relative to the 1986-2005 reference period.
However, since the AR5, the scientific community has revised the historic warming estimate since 1850-1900. The IPCC AR6 clarifies in its Summary for Policymakers of the 2021 Working Group I report: “Since AR5, methodological advances and new datasets have provided a more complete spatial representation of changes in surface temperature, including in the Arctic. These and other improvements have additionally increased the estimate of global surface temperature change by approximately 0.1°C, but this increase does not represent additional physical warming since the AR5.”
This change, which only reflects improved ways of measuring warming rather than actual physical changes, and how it relates to the Paris Agreement goal is a question of value judgements and political guidance. The UNFCCC Periodic Review of the Long-Term Temperature Goal, now in its second phase (2020-2022) provides for an opportunity to assess the AR6 findings and its implication for the goal.
Which greenhouse gases metric should be used to account under the Paris Agreement?
For many years, the equivalence between CO2 and non-CO2 emissions in the UNFCCC has been calculated based on the Global Warming Potentials of each greenhouse gas over a period of 100 years – called GWP100 (read more about greenhouse gas metrics in Schleussner et al. 2019.). This allows each volume of emissions to be quantified in terms of CO2e (CO2 equivalent), so that the balance between emissions and removals required to achieve net zero could be calculated. The Paris Agreement rulebook agreed upon in Katowice established GWP100 as the metric for reporting under the Paris Agreement.
Some gases, such as methane (CH4), have a short atmospheric lifetime and a strong near-term warming effect. When their remaining emissions are compensated by removals of CO2 (a less strong but long-lived greenhouse gas) and a balance is achieved, continuing CO2 removals will lead to a decline in temperature. Such a temperature decline is fully consistent with the continuation of “pursuing efforts” to limit warming to 1.5°C under an overshoot interpretation.