Limit on carbon dioxide emission for a given climate impact
For the assessment of the biogeochemical cycle by which carbon is exchanged at the global level between sources and sinks in the biosphere, pedosphere, geosphere, hydrosphere, and atmosphere, also referred to as the Global Carbon Budget, see
Carbon cycle.
A carbon budget is a concept used in
climate policy to help set
emissions reduction targets in a fair and effective way. It examines the "maximum amount of cumulative net global anthropogenic carbon dioxide (CO2) emissions that would result in limiting
global warming to a given level".[2]: 2220 It can be expressed relative to the
pre-industrial period (the year 1750). In this case, it is the total carbon budget. Or it can be expressed from a recent specified date onwards. In that case it is the remaining carbon budget.[2]: 2220
A carbon budget that will keeping global warming below a specified temperature limit is also called an emissions budget or quota, or allowable emissions.[3][4][5] Apart from limiting the
global temperature increase, another objective of such an emissions budget can be to limit
sea level rise.[6]
Scientists combine estimates of various contributing factors to calculate the carbon budget. The estimates take into account the available scientific evidence as well as value judgments or choices.[7][8][9][10][11]
Global carbon budgets can be further sub-divided into national emissions budgets. This can help countries set their own emission goals. Emissions budgets indicate a finite amount of carbon dioxide that can be emitted over time, before resulting in dangerous levels of global warming. The change in global temperature is independent of the source of these emissions, and is largely independent of the timing of these emissions.[12][13]
To translate global carbon budgets to the country level, a set of value judgments have to be made on how to distribute the remaining carbon budget over all the different countries. This should take into account aspects of equity and fairness between countries[10][14] as well as other methodological choices.[14] There are many differences between nations, such as population size, level of industrialisation, historic emissions, and mitigation capabilities. For this reason, scientists are attempting to allocate global carbon budgets among countries using various principles of equity.[15]
"An assessment of carbon cycle sources and sinks on a global level, through the synthesis of evidence for fossil fuel and cement emissions, emissions and removals associated with land use and
land-use change, ocean and natural land sources and sinks of carbon dioxide (CO2), and the resulting change in atmospheric CO2 concentration. This is referred to as the global carbon budget."; or
"The maximum amount of cumulative net global anthropogenic CO2 emissions that would result in limiting global warming to a given level with a given probability, taking into account the effect of other anthropogenic climate forcers. This is referred to as the total carbon budget when expressed starting from the pre-industrial period, and as the remaining carbon budget when expressed from a recent specified date."
Global carbon budgets can be further divided into national emissions budgets, so that countries can set specific climate mitigation goals.
An emissions budget may be distinguished from an
emissions target, as an emissions target may be internationally or nationally set in accordance with objectives other than a specific global temperature and are commonly applied to the annual emissions in a single year as well.
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.[16]
Fossil CO2 emissions: global; territorial; by fuel type (incl cement); per capita[17]
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)[18] and the CONSTRAIN project.[19] In March 2022, before formal publication of the "Global Carbon Budget 2021"
preprint,[17] scientists reported, based on Carbon Monitor[20] (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.[21]
In April 2022, the now
reviewed and officially published
The Global Carbon Budget 2021 concluded that fossil CO2 emissions rebounded[22] 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.[17]
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"[18] 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.[21]
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.[23] 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.[24][25]
Scientific estimations of the remaining global emissions budgets/quotas differ due to varied methodological approaches, and considerations of thresholds.[26] Estimations might not include all amplifying
climate change feedbacks,[27][28][29][30] although the most authoritative carbon budget assessments as summarised by the
IPCC do account explicitly for these.[8][11] Scientists assess the size of remaining carbon budgets using estimates of:
Carbon budget estimates depend on the likelihood or probability of avoiding a temperature limit, and the assumed warming that is projected to be caused by non-CO2 emissions.[8][9][11][33] These estimates assume non-CO2 emissions are also reduced in line with deep
decarbonisation scenarios that reach global
net zero CO2 emissions.[8][9][11] Carbon budget estimates thus depend on how successful society is in reducing non-CO2 emissions together with carbon dioxide emissions. Scientists estimated that remaining carbon budgets can be 220 Gt CO2 higher or lower depending on how successful non-CO2 emissions are reduced.[11]
Estimated carbon budgets in GtCO2 from 2020 with likelihoods[11]: Table 5.8
Carbon budgets are applicable to the global level. To translate these global carbon budgets to the country level, a set of value judgments have to be made on how to distribute the total and remaining carbon budget. In light of the many differences between nations, including but not limited to population, level of industrialisation, national emissions histories, and mitigation capabilities, scientists have made attempts to allocate global carbon budgets among countries using methods that follow various principles of equity.[15] Allocating national emissions budgets is comparable to sharing the effort to reduce global emissions, underlined by some assumptions of state-level responsibility of climate change. Many authors have conducted quantitative analyses which allocate emissions budgets,[5][34][35][36][37] often simultaneously addressing disparities in historical GHG emissions between nations.
One guiding principle that is used to allocate global emissions budgets to nations is the principle of "
common but differentiated responsibilities and respective capabilities" that is included in the
United Nations Framework Convention on Climate Change (UNFCCC).[15] This principle is not defined in further detail in the UNFCCC but is broadly understood to recognize nations' different cumulative historical contributions to global emissions as well as their different development stages. From this perspective, those countries with greater emissions during a set time period (for example, since the pre-industrial era to the present) are the most responsible for addressing excess emissions, as are countries that are richer. Thus, their national emissions budgets have to be smaller than those from countries that have polluted less in the past, or are poorer. The concept of national historical responsibility for climate change has prevailed in the literature since the early 1990s[38][39] and has been part of the key international agreements on climate change (UNFCCC, the
Kyoto Protocol and the
Paris Agreement). Consequently, those countries with the highest cumulative historical emissions have the most responsibility to take the strongest actions[40] and help developing countries to mitigate their emissions and adapt to climate change. This principle is recognized in international treaties and has been part of the diplomatic strategies by developing countries, that argue that they need larger emissions budgets[41] to reduce inequity and achieve
sustainable development.
Another common equity principle for calculating national emissions budgets is the "
egalitarian" principle. This principle stipulates individuals should have equal rights, and therefore emissions budgets should be distributed proportionally according to state populations.[15] Some scientists have thus reasoned the use of national per-capita emissions in national emissions budget calculations.[34][35][36][42] This principle may be favoured by nations with larger or rapidly growing populations,[41] but raises the question whether individuals can have a right to pollute.[43]
A third equity principle that has been employed in national budget calculations considers national
sovereignty.[15] The "sovereignty" principle highlights the equal right of nations to pollute.[15] The grandfathering method for calculating national emissions budgets uses this principle. Grandfathering allocates these budgets proportionally according to emissions at a particular base year,[42] and has been used under international regimes such as the Kyoto Protocol[44] and the early phase of the European Union Emissions Trading Scheme (EU ETS)[45] This principle is often favoured by developed countries, as it allocates larger emissions budgets to them.[41] However, recent publications highlight that grandfathering is unsupported as an equity principle as it "creates 'cascading biases' against poorer states,[46] is not a 'standard of equity'[47]".[48] Other scholars have highlighted that "to treat states as the owners of emission rights has morally problematic consequences".[43]
Pathways to stay within carbon budget
The steps that can be taken to stay within one's carbon budget are explained within the concept of
climate change mitigation.
Solar energy and
wind power have the greatest potential for supplanting fossil fuels at the lowest cost compared to other options.[50] The availability of sunshine and wind is variable and can require
electrical grid ugrades, such as using
long-distance electricity transmission to group a range of power sources.[51]Energy storage can also be used to even out power output, and
demand management can limit power use when power generation is low. Cleanly generated
electricity can usually replace fossil fuels for powering transportation, heating buildings, and running industrial processes. Certain processes are more difficult to decarbonise, such as
air travel and
cement production.
Carbon capture and storage (CCS) can be an option to reduce net emissions in these circumstances, although fossil fuel power plants with CCS technology have not yet proven economical.[52]
Human land use changes such as
agriculture and deforestation cause about 1/4th of climate change. These changes impact how much CO2 is absorbed by plant matter and how much organic matter decays or burns to release CO2. These changes are part of the fast
carbon cycle, whereas fossil fuels release CO2 that was buried underground as part of the slow carbon cycle.
Methane is a short lived greenhouse gas that is produced by decaying organic matter and livestock, as well as fossil fuel extraction. Land use changes can also impact precipitation patterns and the
reflectivity of the surface of the Earth. It is possible to cut emissions from agriculture by reducing
food waste, switching to a more
plant-based diet (also referred to as
low-carbon diet), and by improving farming processes.[53]
Various policies can encourage climate change mitigation.
Carbon pricing systems have been set up that either
tax CO2 emissions or
cap total emissions and trade emission credits.
Fossil fuel subsidies can be eliminated in favor of clean
energy subsidies, and incentives offered for installing energy efficiency measures or switching to electric power sources.[54] Another issue is overcoming environmental objections when constructing new clean energy sources and making grid modifications. Current policies are insufficient as they would still result in global warming of about 2.7 °C by 2100.[55] This warming is significantly above the 2015
Paris Agreement's goal of limiting global warming to well below 2 °C and preferably to 1.5 °C.[56][57]
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