Variability of the Atlantic meridional overturning circulation in CCSM4

By Gokhan Danabasoglu, S. Yeager, Young‐Oh Kwon, Joseph J. Tribbia, A. Phillips, J. Hurrell. 2012

177 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/bba176ea3a54ae6e6674d4dcbff6c942263ffdb9

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. John Marshall
2. M. Buckley
3. Gokhan Danabasoglu
4. S. Yeager
5. Alicia Karspeck
6. F. Zeng
7. Joseph J. Tribbia
8. T. Delworth

In Global and Planetary Change

1. M. Buckley
2. John Marshall
3. S. Yeager
4. Gokhan Danabasoglu
5. T. Delworth
6. F. Zeng
7. Alicia Karspeck
8. R. Sutton

In Oceanography

1. M. Buckley
2. John Marshall
3. Gokhan Danabasoglu
4. S. Yeager
5. T. Delworth
6. Alicia Karspeck
7. R. Sutton
8. F. Zeng

Citations in the corpus

• A delayed oscillator model for the quasi-periodic multidecadal variability of the NAO (2015, unknown): “Several recent studies have used the CCSM4 pre-industrial control simulations to investigate the Atlantic multidecadal variability and found that the model performs reasonably well in capturing the variability (Danabasoglu et al. 2012; Zan-chettin et al. 2014).”
• The Central Role of Ocean Dynamics in Connecting the North Atlantic Oscillation to the Extratropical Component of the Atlantic Multidecadal Oscillation (2017, background): “Extensive prior work has shown that AMOC variations occur in models on decadalto-multidecadal time scales and that these AMOC variations produce monopole SST patterns in the Atlantic that resemble the observedAMO(Delworth et al. 1993; Knight 2005; Danabasoglu et al. 2012).”
• A decadal prediction case study: Late twentieth-century North Atlantic Ocean heat content (2012, methodology): “The atmospheric model has a finite-volume dynamical core with a nominal 18 horizontal resolution and 26 vertical levels, and the ocean model has a nominal 18 horizontal resolution with 60 vertical levels (Danabasoglu et al. 2012a).”
• The Impact of the North Atlantic Oscillation on Climate through Its Influence on the Atlantic Meridional Overturning Circulation (2016, unknown): “These factors tend to enhance the AMOC (Danabasoglu et al. 2012).”
• A Review of the Role of the Atlantic Meridional Overturning Circulation in Atlantic Multidecadal Variability and Associated Climate Impacts (2019, background): “Linkage Indicated by Modeling Results The linkage between multidecadal AMOC variability and AMV has been found in many unforced CGCM control simulations (e.g., Ba et al., 2014; Brown et al., 2016; Danabasoglu et al., 2012; Delworth & Mann, 2000; Drews & Greatbatch, 2016, 2017; Keenlyside et al., 201”
• Observations, inferences, and mechanisms of the Atlantic Meridional Overturning Circulation: A review (2016, background): “…2000; Mignot and Frankignoul, 2005; Guemas and Salas-Mélia, 2008; Danabasoglu, 2008; Danabasoglu et al., 2012], and (3) the first principle component time series of the (generally annual mean or low-pass-filtered) AMOC [Dong and Sutton, 2005; Danabasoglu, 2008; Danabasoglu et al., 2012].”