Adjustment of the coupled ocean–atmosphere system to a sudden change in the Thermohaline Circulation
184 citations recorded by the source corpus.
Subfields: Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/6fcaeb14809751eeaa8ab071b2651efeb2b52004
How researchers see this paper
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In Global and Planetary Change
- S. Yeager
- Gokhan Danabasoglu
- A. Timmermann
- R. Sutton
- Eric Guilyardi
- Shang-Ping Xie
- Johann Jungclaus
- Young‐Oh Kwon
In Oceanography
- Gokhan Danabasoglu
- S. Yeager
- A. Timmermann
- R. Sutton
- Eric Guilyardi
- Young‐Oh Kwon
- Soon-Il An
- Rong‐Hua Zhang
Citations in the corpus
- ENSO suppression due to weakening of the North Atlantic thermohaline circulation (2005, background): “The potential impact of THC changes on the El Niño–Southern Oscillation (ENSO) phenomenon transmitted also by large-scale atmospheric changes has been described briefly in Dong and Sutton (2002).”
- A Review of the Role of the Atlantic Meridional Overturning Circulation in Atlantic Multidecadal Variability and Associated Climate Impacts (2019, background): “…in the tropics) and La Niña‐like cooling over the eastern tropical Pacific (Dong et al., 2006; Kucharski et al., 2016; Ruprich‐Robert et al., 2017), similar to the changes induced by a weakening of the AMOC in CGCMs but with an opposite sign (e.g., Dong & Sutton, 2002; Zhang & Delworth, 2005).”
- The influence of a weakening of the atlantic meridional overturning circulation on ENSO (2006, background): “Atmospheric teleconnections from the tropical Atlantic play a crucial role in generating oceanic and atmospheric anomalies in the eastern tropical Pacific (Dong and Sutton 2002; Zhang and Delworth 2005).”
- Mechanism of interdecadal thermohaline circulation variability in a coupled ocean : Atmosphere GCM (2005, background): “As shown in Dong and Sutton (2002b) in a 100-yr simulation with the same model (but with suppressed air–sea interaction in the tropical Pacific and Indian Oceans), variability in the northward transport of heat in the Atlantic is primarily governed by fluctuations of the advection of mean…”