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CMIP6 Models Predict Significant 21st Century Decline of the Atlantic Meridional Overturning Circulation

Geophysical research letters, 2020-06, Vol.47 (12), p.n/a

2020

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The North Atlantic Ocean Is in a State of Reduced Overturning

Geophysical research letters, 2018-02, Vol.45 (3), p.1527-1533

2018

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Meridional Connectivity of a 25‐Year Observational AMOC Record at 47°N

Geophysical research letters, 2023-08, Vol.50 (16), p.n/a

2023

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Aerosol‐Forced AMOC Changes in CMIP6 Historical Simulations

Geophysical research letters, 2020-07, Vol.47 (14), p.n/a

2020

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Irminger Sea Is the Center of Action for Subpolar AMOC Variability

Geophysical research letters, 2022-09, Vol.49 (17), p.n/a

2022

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Impact of ocean resolution and mean state on the rate of AMOC weakening

Climate dynamics, 2020-10, Vol.55 (7-8), p.1711-1732

2020

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Mechanisms and Impacts of a Partial AMOC Recovery Under Enhanced Freshwater Forcing

Geophysical research letters, 2019-03, Vol.46 (6), p.3308-3316

2019

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On the persistence and coherence of subpolar sea surface temperature and salinity anomalies associated with the Atlantic multidecadal variability

Geophysical research letters, 2017-08, Vol.44 (15), p.7865-7875

Zhang, Rong

2017

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Publisher Correction: Observation-based early-warning signals for a collapse of the Atlantic Meridional Overturning Circulation

Nature climate change, 2021-11, Vol.11 (11), p.1001-1001

Boers, Niklas

2021

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Internal multi-centennial variability of the Atlantic Meridional Overturning Circulation simulated by EC-Earth3

Climate dynamics, 2023-06, Vol.60 (11-12), p.3695-3712

2023

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Prediction of slowdown of the Atlantic Meridional Overturning Circulation in coupled model simulations

Climate dynamics, 2024-03

2024

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Deconstructing Future AMOC Decline at 26.5°N

Geophysical research letters, 2023-07, Vol.50 (14), p.n/a

2023

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Mass, Heat, and Freshwater Transport From Transoceanic Sections in the Atlantic Ocean at 30°S and 24.5°N: Single Sections Versus Box Models?

Geophysical research letters, 2023-06, Vol.50 (11), p.n/a

2023

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Routine Reversal of the AMOC in an Ocean Model Ensemble

Geophysical research letters, 2022-12, Vol.49 (24), p.n/a

2022

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North Atlantic overturning and water mass transformation in CMIP6 models

Climate dynamics, 2023-05, Vol.60 (9-10), p.2871-2891

2023

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Thirty Years of GOSHIP and WOCE Data: Atlantic Overturning of Mass, Heat, and Freshwater Transport

Geophysical research letters, 2022-02, Vol.49 (4), p.n/a

2022

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Constraining the Variability of the Atlantic Meridional Overturning Circulation During the Holocene

Geophysical research letters, 2019-10, Vol.46 (20), p.11338-11346

2019

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Atlantic meridional heat transports computed from balancing Earth's energy locally

Geophysical research letters, 2017-02, Vol.44 (4), p.1919-1927

2017

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Rapid Communication of Upper‐Ocean Salinity Anomaly to Deep Waters of the Iceland Basin Indicates an AMOC Short‐Cut

Geophysical research letters, 2022-02, Vol.49 (3), p.n/a

2022

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Hysteresis and Resilience of the AMOC in an Eddy‐Permitting GCM

Geophysical research letters, 2018-08, Vol.45 (16), p.8547-8556

2018

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Impacts and State‐Dependence of AMOC Weakening in a Warming Climate

Geophysical research letters, 2024-05, Vol.51 (10), p.n/a

2024

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Overturning Pathways Control AMOC Weakening in CMIP6 Models

Geophysical research letters, 2023-07, Vol.50 (14), p.n/a

2023

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Future Slower Reduction of Anthropogenic Aerosols Enhances Extratropical Ocean Surface Warming Trends

Geophysical research letters, 2024-04, Vol.51 (8), p.n/a

2024

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Sensitivity of the Atlantic Meridional Overturning Circulation to Model Resolution in CMIP6 HighResMIP Simulations and Implications for Future Changes

Journal of advances in modeling earth systems, 2020-08, Vol.12 (8), p.n/a

2020

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Abrupt Bølling‐Allerød Warming Simulated under Gradual Forcing of the Last Deglaciation

Geophysical research letters, 2019-10, Vol.46 (20), p.11397-11405

2019

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CMIP6 Models Predict Significant 21st Century Decline of the Atlantic Meridional Overturning Circulation

The North Atlantic Ocean Is in a State of Reduced Overturning

Meridional Connectivity of a 25‐Year Observational AMOC Record at 47°N

Aerosol‐Forced AMOC Changes in CMIP6 Historical Simulations

Irminger Sea Is the Center of Action for Subpolar AMOC Variability

Impact of ocean resolution and mean state on the rate of AMOC weakening

Mechanisms and Impacts of a Partial AMOC Recovery Under Enhanced Freshwater Forcing

On the persistence and coherence of subpolar sea surface temperature and salinity anomalies associated with the Atlantic multidecadal variability

Publisher Correction: Observation-based early-warning signals for a collapse of the Atlantic Meridional Overturning Circulation

Internal multi-centennial variability of the Atlantic Meridional Overturning Circulation simulated by EC-Earth3

Prediction of slowdown of the Atlantic Meridional Overturning Circulation in coupled model simulations

Deconstructing Future AMOC Decline at 26.5°N

Mass, Heat, and Freshwater Transport From Transoceanic Sections in the Atlantic Ocean at 30°S and 24.5°N: Single Sections Versus Box Models?

Routine Reversal of the AMOC in an Ocean Model Ensemble

North Atlantic overturning and water mass transformation in CMIP6 models

Thirty Years of GOSHIP and WOCE Data: Atlantic Overturning of Mass, Heat, and Freshwater Transport

Constraining the Variability of the Atlantic Meridional Overturning Circulation During the Holocene

Atlantic meridional heat transports computed from balancing Earth's energy locally

Rapid Communication of Upper‐Ocean Salinity Anomaly to Deep Waters of the Iceland Basin Indicates an AMOC Short‐Cut

Hysteresis and Resilience of the AMOC in an Eddy‐Permitting GCM

Impacts and State‐Dependence of AMOC Weakening in a Warming Climate

Overturning Pathways Control AMOC Weakening in CMIP6 Models

Future Slower Reduction of Anthropogenic Aerosols Enhances Extratropical Ocean Surface Warming Trends

Sensitivity of the Atlantic Meridional Overturning Circulation to Model Resolution in CMIP6 HighResMIP Simulations and Implications for Future Changes

Abrupt Bølling‐Allerød Warming Simulated under Gradual Forcing of the Last Deglaciation

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