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1.
Nat Commun ; 15(1): 1885, 2024 Feb 29.
Artigo em Inglês | MEDLINE | ID: mdl-38424076

RESUMO

Earth System Models (ESMs) continue to diagnose a wide range of carbon budgets for each level of global warming. Here, we present emergent constraints on the carbon budget as a function of global warming, which combine the available ESM historical simulations and future projections for a range of scenarios, with observational estimates of global warming and anthropogenic CO2 emissions to the present day. We estimate mean and likely ranges for cumulative carbon budgets for the Paris targets of 1.5 °C and 2 °C of global warming of 812 [691, 933] PgC and 1048 [881, 1216] PgC, which are more than 10% larger than the ensemble mean values from the CMIP6 models. The linearity between cumulative emissions and global warming is found to be maintained at least until 4 °C, and is consistent with an effective Transient Climate Response to Emissions (eTCRE) of 2.1 [1.8, 2.6] °C/1000PgC, from a global warming of 1.2 °C onwards.

5.
Nature ; 580(7802): E4, 2020 04.
Artigo em Inglês | MEDLINE | ID: mdl-32269337

RESUMO

An amendment to this paper has been published and can be accessed via a link at the top of the paper.

7.
Nature ; 571(7765): 335-342, 2019 07.
Artigo em Inglês | MEDLINE | ID: mdl-31316194

RESUMO

Research reported during the past decade has shown that global warming is roughly proportional to the total amount of carbon dioxide released into the atmosphere. This makes it possible to estimate the remaining carbon budget: the total amount of anthropogenic carbon dioxide that can still be emitted into the atmosphere while holding the global average temperature increase to the limit set by the Paris Agreement. However, a wide range of estimates for the remaining carbon budget has been reported, reducing the effectiveness of the remaining carbon budget as a means of setting emission reduction targets that are consistent with the Paris Agreement. Here we present a framework that enables us to track estimates of the remaining carbon budget and to understand how these estimates can improve over time as scientific knowledge advances. We propose that application of this framework may help to reconcile differences between estimates of the remaining carbon budget and may provide a basis for reducing uncertainty in the range of future estimates.


Assuntos
Atmosfera/química , Dióxido de Carbono/análise , Aquecimento Global/prevenção & controle , Aquecimento Global/estatística & dados numéricos , Objetivos , Modelos Teóricos , Temperatura , Planeta Terra , Política Ambiental/legislação & jurisprudência , Retroalimentação , Aquecimento Global/legislação & jurisprudência , Atividades Humanas/legislação & jurisprudência , Cooperação Internacional/legislação & jurisprudência , Paris , Reprodutibilidade dos Testes , Fatores de Tempo , Incerteza
8.
Nature ; 493(7430): 79-83, 2013 Jan 03.
Artigo em Inglês | MEDLINE | ID: mdl-23282364

RESUMO

For more than a decade, the target of keeping global warming below 2 °C has been a key focus of the international climate debate. In response, the scientific community has published a number of scenario studies that estimate the costs of achieving such a target. Producing these estimates remains a challenge, particularly because of relatively well known, but poorly quantified, uncertainties, and owing to limited integration of scientific knowledge across disciplines. The integrated assessment community, on the one hand, has extensively assessed the influence of technological and socio-economic uncertainties on low-carbon scenarios and associated costs. The climate modelling community, on the other hand, has spent years improving its understanding of the geophysical response of the Earth system to emissions of greenhouse gases. This geophysical response remains a key uncertainty in the cost of mitigation scenarios but has been integrated with assessments of other uncertainties in only a rudimentary manner, that is, for equilibrium conditions. Here we bridge this gap between the two research communities by generating distributions of the costs associated with limiting transient global temperature increase to below specific values, taking into account uncertainties in four factors: geophysical, technological, social and political. We find that political choices that delay mitigation have the largest effect on the cost-risk distribution, followed by geophysical uncertainties, social factors influencing future energy demand and, lastly, technological uncertainties surrounding the availability of greenhouse gas mitigation options. Our information on temperature risk and mitigation costs provides crucial information for policy-making, because it clarifies the relative importance of mitigation costs, energy demand and the timing of global action in reducing the risk of exceeding a global temperature increase of 2 °C, or other limits such as 3 °C or 1.5 °C, across a wide range of scenarios.


Assuntos
Conservação de Recursos Energéticos/métodos , Conservação de Recursos Energéticos/tendências , Aquecimento Global/prevenção & controle , Probabilidade , Temperatura , Aquecimento Global/economia , Modelos Teóricos , Política , Incerteza
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