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Slowing down as an early warning signal for abrupt climate change

Proceedings of the National Academy of Sciences - PNAS, 2008-09, Vol.105 (38), p.14308-14312

2008

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Carbon–Concentration and Carbon–Climate Feedbacks in CMIP5 Earth System Models

Journal of climate, 2013-08, Vol.26 (15), p.5289-5314

2013

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The Land Use Model Intercomparison Project (LUMIP) contribution to CMIP6: rationale and experimental design

Geoscientific Model Development, 2016-09, Vol.9 (9), p.2973-2998

2016

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Nitrogen cycling in CMIP6 land surface models: progress and limitations

Biogeosciences, 2020-10, Vol.17 (20), p.5129-5148

2020

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Twenty-First-Century Compatible CO₂ Emissions and Airborne Fraction Simulated by CMIP5 Earth System Models under Four Representative Concentration Pathways

Journal of climate, 2013-07, Vol.26 (13), p.4398-4413

2013

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Global climate response to idealized deforestation in CMIP6 models

Biogeosciences, 2020-11, Vol.17 (22), p.5615-5638

2020

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C4MIP – The Coupled Climate–Carbon Cycle Model Intercomparison Project: experimental protocol for CMIP6

Geoscientific Model Development, 2016-08, Vol.9 (8), p.2853-2880

2016

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Climate and carbon cycle changes from 1850 to 2100 in MPI‐ESM simulations for the Coupled Model Intercomparison Project phase 5

Journal of advances in modeling earth systems, 2013-07, Vol.5 (3), p.572-597

2013

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CO₂-Induced Sahel Greening in Three CMIP5 Earth System Models

Journal of climate, 2014-09, Vol.27 (18), p.7163-7184

2014

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Geoengineering climate by stratospheric sulfur injections: Earth system vulnerability to technological failure

Climatic change, 2009-02, Vol.92 (3-4), p.243-259

2009

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Evaluation of soil carbon dynamics after forest cover change in CMIP6 land models using chronosequences

Environmental research letters, 2021-07, Vol.16 (7), p.74030

2021

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Uncertainty in land carbon budget simulated by terrestrial biosphere models: the role of atmospheric forcing

Environmental research letters, 2022-09, Vol.17 (9), p.94033

2022

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Snowfall-albedo feedbacks could have led to deglaciation of snowball Earth starting from mid-latitudes

Communications earth & environment, 2021-12, Vol.2 (1), Article 91

2021

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Assessing climate forcings of the Earth system for the past millennium

Geophysical research letters, 2003-03, Vol.30 (6), p.1276-n/a

2003

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Simulation of an abrupt change in Saharan vegetation in the Mid-Holocene

Geophysical research letters, 1999-07, Vol.26 (14), p.2037-2040

1999

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The Influence of Vegetation-Atmosphere-Ocean Interaction on Climate During the Mid-Holocene

Science (American Association for the Advancement of Science), 1998-06, Vol.280 (5371), p.1916-1919

1998

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The climate and vegetation of Marine Isotope Stage 11 – Model results and proxy-based reconstructions at global and regional scale

Quaternary international, 2014-10, Vol.348, p.247-265

2014

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Simulation of climate, ice sheets and CO2 evolution during the last four glacial cycles with an Earth system model of intermediate complexity

Climate of the past, 2017-11, Vol.13 (12), p.1695-1716

2017

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Simulation of climate, ice sheets and CO 2 evolution during the last four glacial cycles with an Earth system model of intermediate complexity

Climate of the past, 2017-11, Vol.13 (12), p.1695-1716

2017

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Harmonising plant functional type distributions for evaluating Earth system models

Climate of the past, 2019-02, Vol.15 (1), p.335-366

2019

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Simulated methane emissions from Arctic ponds are highly sensitive to warming

Biogeosciences, 2023-07, Vol.20 (14), p.2837-2855

2023

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What was the source of the atmospheric CO2 increase during the Holocene?

Biogeosciences, 2019-07, Vol.16 (13), p.2543-2555

2019

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Effects of orbital forcing, greenhouse gases and ice sheets on Saharan greening in past and future multi-millennia

Climate of the past, 2022-08, Vol.18 (8), p.1897-1914

2022

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Diverging responses of high-latitude CO2 and CH4 emissions in idealized climate change scenarios

The cryosphere, 2021-03, Vol.15 (2), p.1097-1130

2021

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Slowing down as an early warning signal for abrupt climate change

Carbon–Concentration and Carbon–Climate Feedbacks in CMIP5 Earth System Models

The Land Use Model Intercomparison Project (LUMIP) contribution to CMIP6: rationale and experimental design

Nitrogen cycling in CMIP6 land surface models: progress and limitations

Twenty-First-Century Compatible CO₂ Emissions and Airborne Fraction Simulated by CMIP5 Earth System Models under Four Representative Concentration Pathways

Global climate response to idealized deforestation in CMIP6 models

C4MIP – The Coupled Climate–Carbon Cycle Model Intercomparison Project: experimental protocol for CMIP6

Climate and carbon cycle changes from 1850 to 2100 in MPI‐ESM simulations for the Coupled Model Intercomparison Project phase 5

CO₂-Induced Sahel Greening in Three CMIP5 Earth System Models

Geoengineering climate by stratospheric sulfur injections: Earth system vulnerability to technological failure

Evaluation of soil carbon dynamics after forest cover change in CMIP6 land models using chronosequences

Uncertainty in land carbon budget simulated by terrestrial biosphere models: the role of atmospheric forcing

Snowfall-albedo feedbacks could have led to deglaciation of snowball Earth starting from mid-latitudes

Assessing climate forcings of the Earth system for the past millennium

Simulation of an abrupt change in Saharan vegetation in the Mid-Holocene

The Influence of Vegetation-Atmosphere-Ocean Interaction on Climate During the Mid-Holocene

The climate and vegetation of Marine Isotope Stage 11 – Model results and proxy-based reconstructions at global and regional scale

Simulation of climate, ice sheets and CO2 evolution during the last four glacial cycles with an Earth system model of intermediate complexity

Simulation of climate, ice sheets and CO 2 evolution during the last four glacial cycles with an Earth system model of intermediate complexity

Carbon–concentration and carbon–climate feedbacks in CMIP6 models and their comparison to CMIP5 models

Harmonising plant functional type distributions for evaluating Earth system models

Simulated methane emissions from Arctic ponds are highly sensitive to warming

What was the source of the atmospheric CO2 increase during the Holocene?

Effects of orbital forcing, greenhouse gases and ice sheets on Saharan greening in past and future multi-millennia

Diverging responses of high-latitude CO2 and CH4 emissions in idealized climate change scenarios

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