Bistability of the Atlantic overturning circulation in a global climate model and links to ocean freshwater transport
By Ed Hawkins, L. Allison, J. Gregory, T. Woollings, Holger Pohlmann, B. D. de Cuevas. 2011
261 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/402330be796707ca7856f814c9fa7ce6f7ecc2e9
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In Atmospheric Science
- John Marshall
- M. Buckley
- Michael Ghil
- Jiacan Yuan
- Jürgen Kurths
- M. Latif
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In Global and Planetary Change
In Oceanography
- M. Buckley
- John Marshall
- M. Latif
- Michael Ghil
- Valerio Lucarini
- Chih-Pei Chang
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- J. Wallace
Citations in the corpus
- A mathematical theory of climate sensitivity or, How to deal with both anthropogenic forcing and natural variability? (2015, background): “, 2011) and ocean reanalyses (Hawkins et al., 2011) confirm that the Atlantic Ocean’s THC is actually in this regime at the present time.”
- Tipping elements and climate–economic shocks: Pathways toward integrated assessment (2016, methodology): “AMOC also exhibits hysteresis: in order to restore the circulation once the system collapses, freshwater forcing must be reduced below a threshold that is smaller than the threshold originally required to cause the collapse [Rahmstorf, 1996, 2005; Hawkins et al., 2011].”
- The physics of climate variability and climate change (2019, background): “stability of the THC for (a) Earth models of intermediate complexity, reproduced with permission from Rahmstorf et al. (2005); and (b) for an IPCC-class climate model, reproduced with permission from Hawkins et al. (2011). Parameter controlling the freshwater input in the North Atlantic basin on the”
- Observations, inferences, and mechanisms of the Atlantic Meridional Overturning Circulation: A review (2016, background): “3), then the AMOC is in the bistable regime [Rahmstorf , 1996; Schaeffer et al., 2002; de Vries and Weber, 2005; Dijkstra, 2007; Huisman et al., 2010; Hawkins et al., 2011; Drijfhout et al., 2011; Weaver et al., 2012; Deshayes et al., 2013; Liu and Liu, 2014].”
- Interacting tipping elements increase risk of climate domino effects under global warming (2020, methodology): “More complex Earth system models including a fully implicit ocean model (Huisman et al., 2010), Earth system models of intermediate complexity (EMICs, e.g. CLIMBER; Rahmstorf et al., 2005) and an atmosphere–ocean general circulation model (AOGCM, e.g. the FAMOUS model; Hawkins et al., 2011) have sho”