Articles | Volume 12, issue 8
https://doi.org/10.5194/cp-12-1663-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-1663-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
18 Aug 2016
Research article |
| 18 Aug 2016
Hosed vs. unhosed: interruptions of the Atlantic Meridional Overturning Circulation in a global coupled model, with and without freshwater forcing
Nicolas Brown
Department of Earth and Planetary Science, McGill University, Montréal
QC H3A 2A7, Canada
Eric D. Galbraith
CORRESPONDING AUTHOR
Department of Earth and Planetary Science, McGill University, Montréal
QC H3A 2A7, Canada
Institut de Ciència i Tecnologia Ambientals (ICTA) and Department of Mathematics, Universitat Autonoma de Barcelona, 08193 Barcelona, Spain
ICREA, Pg. Lluís Companys 23, 08010 Barcelona, Spain
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2 citations as recorded by crossref.
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- Destabilization of glacial climate by the radiative impact of Atlantic Meridional Overturning Circulation disruptions E. Galbraith et al. 10.1002/2016GL069846
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Latest update: 18 Nov 2024
Short summary
An Earth system model is used to explore variability in the global impacts of AMOC disruptions. The model exhibits spontaneous AMOC oscillations under particular boundary conditions, which we compare with freshwater-forced disruptions. We find that the global impacts are similar whether the AMOC disruptions are spontaneous or forced. Freshwater forcing generally amplifies the global impacts, with tropical precipitation and the stability of polar haloclines showing particular sensitivity.
An Earth system model is used to explore variability in the global impacts of AMOC disruptions....
