Causes of Interannual–Decadal Variability in the Meridional Overturning Circulation of the Midlatitude North Atlantic Ocean
By Arne Biastoch, C. Böning, Julia Getzlaff, J. Molines, Gurvan Madec. 2008
270 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/309a7fdf571954444e8d8da7f5e8c7b6a0422071
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
- John Marshall
- Gokhan Danabasoglu
- M. Buckley
- S. Yeager
- Alicia Karspeck
- C. Böning
- Arne Biastoch
- E. van Sebille
In Global and Planetary Change
- M. Buckley
- John Marshall
- S. Yeager
- Gokhan Danabasoglu
- Alicia Karspeck
- E. van Sebille
- Jochem Marotzke
- Arne Biastoch
In Oceanography
- M. Buckley
- John Marshall
- Gokhan Danabasoglu
- S. Yeager
- Alicia Karspeck
- C. Böning
- Arne Biastoch
- S. Hüttl-Kabus
Citations in the corpus
- Deep water formation, the subpolar gyre, and the meridional overturning circulation in the subpolar North Atlantic (2011, methodology): “The maximum overturning in this model of 16 Sv is located further south (Biastoch et al., 2008). When analyzing high-resolution (1/121) North Atlantic (FLAME) and global ocean-ice (ORCA) models, Biastoch et al. (2008) examined the cause for interannual to decadal variability of the AMOC.”
- The Impact of the North Atlantic Oscillation on Climate through Its Influence on the Atlantic Meridional Overturning Circulation (2016, unknown): “A rich history of modeling studies (Delworth et al. 1993; Visbeck et al. 1998; Zhu and Jungclaus 2008; Park and Latif 2008; Biastoch et al. 2008; Vellinga and Wu 2004; Frankcombe et al. 2010; Danabasoglu et al. 2012; Medhaug et al. 2012; Menary et al. 2012; Kwon and Frankignoul 2012; Tulloch and…”
- Continuous, Array-Based Estimates of Atlantic Ocean Heat Transport at 26.5°N (2011, background): “For example, Biastoch et al. (2008) examined the relationship between the mean MHT and MOC strength in several published, high-resolution OGCMs, and found, for a set of models with realistic MOC strengths of 16.8 to 19.1 Sv at 258N, corresponding mean MHT values of 0.95 to 1.14 PW.”
- Lagrangian validation of numerical drifter trajectories using drifting buoys: Application to the Agulhas system (2009, methodology): “The 1/10 AG01 model is a two-way nested grid inside the ORCA model, that spans the greater Agulhas region (20 W–70 E; 47 S– 7 S) (Biastoch et al., 2008a,b).”
- Predicted slowdown in the rate of Atlantic sea ice loss (2015, background): “Variations in the winter buoyancy forcing of the subpolar Atlantic Ocean associated with the NAO are believed to generate significant decadal variance in AMOC strength [Häkkinen, 1999; Biastoch et al., 2008; Lohmann et al., 2009; Yeager and Danabasoglu, 2014].”
- Observations, inferences, and mechanisms of the Atlantic Meridional Overturning Circulation: A review (2016, background): “Other studies find that buoyancy anomalies are communicated rapidly in accord with expectations from boundary wave theory [Biastoch et al., 2008a].”