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Current fossil fuel infrastructure does not yet commit us to 1.5 °C warming

Nature communications, 2019-01, Vol.10 (1), p.101-10, Article 101

2019

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Asymmetry in the climate–carbon cycle response to positive and negative CO2 emissions

Nature climate change, 2021-07, Vol.11 (7), p.613-617

2021

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What determines the warming commitment after cessation of CO2 emissions?

Environmental research letters, 2017-01, Vol.12 (1), p.015002

2017

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Accounting for the climate benefit of temporary carbon storage in nature

Nature communications, 2023-09, Vol.14 (1), p.5485-5485, Article 5485

2023

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The time lag between a carbon dioxide emission and maximum warming increases with the size of the emission

Environmental research letters, 2015-03, Vol.10 (3), p.31001

2015

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The proportionality of global warming to cumulative carbon emissions

Nature (London), 2009-06, Vol.459 (7248), p.829-832

2009

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The effectiveness of net negative carbon dioxide emissions in reversing anthropogenic climate change

Environmental research letters, 2015-09, Vol.10 (9), p.94013

2015

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On the proportionality between global temperature change and cumulative CO2 emissions during periods of net negative CO2 emissions

Environmental research letters, 2016, Vol.11 (5), p.055006

2016

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Focus on cumulative emissions, global carbon budgets and the implications for climate mitigation targets

Environmental research letters, 2018-01, Vol.13 (1), p.10201

2018

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Temporary nature-based carbon removal can lower peak warming in a well-below 2 °C scenario

Communications earth & environment, 2022-12, Vol.3 (1), p.1-8, Article 65

2022

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Setting cumulative emissions targets to reduce the risk of dangerous climate change

Proceedings of the National Academy of Sciences - PNAS, 2009-09, Vol.106 (38), p.16129-16134

2009

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Sensitivity of carbon budgets to permafrost carbon feedbacks and non-CO2 forcings

Environmental research letters, 2015-12, Vol.10 (12), p.125003

2015

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Stability of the Atlantic meridional overturning circulation: A model intercomparison

Geophysical research letters, 2012-10, Vol.39 (20), p.n/a

2012

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Path Independence of Carbon Budgets When Meeting a Stringent Global Mean Temperature Target After an Overshoot

Earth's future, 2019-12, Vol.7 (12), p.1283-1295

2019

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The influence of non-CO2 forcings on cumulative carbon emissions budgets

Environmental research letters, 2018-03, Vol.13 (3), p.034039

2018

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Delaying methane mitigation increases the risk of breaching the 2 °C warming limit

Communications earth & environment, 2023-12, Vol.4 (1), p.250-8, Article 250

2023

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Expert judgements on the response of the Atlantic meridional overturning circulation to climate change

Climatic change, 2007-06, Vol.82 (3-4), p.235-265

2007

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Expert judgments about transient climate response to alternative future trajectories of radiative forcing

Proceedings of the National Academy of Sciences - PNAS, 2010-07, Vol.107 (28), p.12451-12456

2010

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The Role of Poleward-Intensifying Winds on Southern Ocean Warming

Journal of climate, 2007-11, Vol.20 (21), p.5391-5400

2007

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Projected local rain events due to climate change and the impacts on waterborne diseases in Vancouver, British Columbia, Canada

Environmental health, 2019-12, Vol.18 (1), p.116-116, Article 116

2019

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Nonlinearity of Carbon Cycle Feedbacks

Journal of climate, 2011-08, Vol.24 (16), p.4255-4275

2011

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Long term climate implications of 2050 emission reduction targets

Geophysical research letters, 2007-10, Vol.34 (19), p.L19703-n/a

2007

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Corrigendum: Sensitivity of carbon budgets to permafrost carbon feedbacks and non-CO2 forcings (2015 Environ. Res. Lett. 10 125003)

Environmental research letters, 2016-01, Vol.11 (1), p.019501

2016

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Carbon-cycle feedbacks of changes in the Atlantic meridional overturning circulation under future atmospheric CO2

Global biogeochemical cycles, 2008-09, Vol.22 (3), p.GB3024-n/a

2008

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Current fossil fuel infrastructure does not yet commit us to 1.5 °C warming

Asymmetry in the climate–carbon cycle response to positive and negative CO2 emissions

What determines the warming commitment after cessation of CO2 emissions?

Accounting for the climate benefit of temporary carbon storage in nature

The time lag between a carbon dioxide emission and maximum warming increases with the size of the emission

The proportionality of global warming to cumulative carbon emissions

The effectiveness of net negative carbon dioxide emissions in reversing anthropogenic climate change

On the proportionality between global temperature change and cumulative CO2 emissions during periods of net negative CO2 emissions

Focus on cumulative emissions, global carbon budgets and the implications for climate mitigation targets

Temporary nature-based carbon removal can lower peak warming in a well-below 2 °C scenario

Setting cumulative emissions targets to reduce the risk of dangerous climate change

Sensitivity of carbon budgets to permafrost carbon feedbacks and non-CO2 forcings

Stability of the Atlantic meridional overturning circulation: A model intercomparison

Long-Term Climate Change Commitment and Reversibility: An EMIC Intercomparison

Path Independence of Carbon Budgets When Meeting a Stringent Global Mean Temperature Target After an Overshoot

The influence of non-CO2 forcings on cumulative carbon emissions budgets

Delaying methane mitigation increases the risk of breaching the 2 °C warming limit

Expert judgements on the response of the Atlantic meridional overturning circulation to climate change

Expert judgments about transient climate response to alternative future trajectories of radiative forcing

The Role of Poleward-Intensifying Winds on Southern Ocean Warming

Projected local rain events due to climate change and the impacts on waterborne diseases in Vancouver, British Columbia, Canada

Nonlinearity of Carbon Cycle Feedbacks

Long term climate implications of 2050 emission reduction targets

Corrigendum: Sensitivity of carbon budgets to permafrost carbon feedbacks and non-CO2 forcings (2015 Environ. Res. Lett. 10 125003)

Carbon-cycle feedbacks of changes in the Atlantic meridional overturning circulation under future atmospheric CO2

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