Is the North Atlantic Oscillation a Breaking Wave

By Christian L. E. Franzke, Sukyoung Lee, S. Feldstein. 2004

247 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/c99ce31f8ef6af2bb2748b5ae03b065d82078a94

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. T. Woollings
2. E. Maloney
3. B. Hoskins
4. Chidong Zhang
5. Hai Lin
6. Xianan Jiang
7. C. DeMott
8. N. Klingaman

In Global and Planetary Change

1. T. Woollings
2. E. Maloney
3. B. Hoskins
4. Chidong Zhang
5. Hai Lin
6. Xianan Jiang
7. C. DeMott
8. N. Klingaman

Citations in the corpus

• Variability of the North Atlantic eddy‐driven jet stream (2010, unknown): “Several studies have linked variations in eddy forcing with Rossby wave breaking events ( Benedict et al. 2004; Franzke et al. 2004; Rivi`ere and Orlanski 2007; Martius et al. 2007; Strong and Magnusdottir 2008; Kunz et al. 2009).”
• Review of Tropical‐Extratropical Teleconnections on Intraseasonal Time Scales (2017, background): “Franzke et al. (2004) found that the variability of the NAO is related to midlatitude Rossby wave breaking.”
• Bidimensional Diagnostics, Variability, and Trends of Northern Hemisphere Blocking (2012, background): “On the other hand, other studies focused on the origin of the North Atlantic Oscillation found evidence of a relationship between the NAO and the occurrence of RWB (Benedict et al. 2004; Franzke et al. 2004; Riviere and Orlanski 2007; Kunz et al. 2009a,b).”
• A New Rossby Wave–Breaking Interpretation of the North Atlantic Oscillation (2008, methodology): “This process of wave breaking leading to NAO events has been simulated by perturbing a primitive equation model with perturbation patterns derived from Pacific storm track variations (Franzke et al. 2004).”
• Low‐frequency nonlinearity and regime behavior in the Northern Hemisphere extratropical atmosphere (2017, background): “Attention has, therefore, focused on synoptic time scales in understanding the dynamics of such patterns, in particular, the importance of Rossby wave breaking [e.g., Benedict et al., 2004; Franzke et al., 2004; Rivière and Orlanski, 2007; Martius et al., 2007].”
• Impact of ENSO on the Atmospheric Variability over the North Atlantic in Late Winter—Role of Transient Eddies (2012, background): “A few other studies has pointed out that anticyclonic and cyclonic breaking of the synoptic eddies could lead to the formation of the positive and negative phase of the NAO, respectively (e.g., Benedict et al. 2004; Franzke et al. 2004; Rivière and Orlanski 2007).”
• An Observed Connection between the North Atlantic Oscillation and the Madden-Julian Oscillation (2009, background): “Franzke et al. (2004) pointed out that the NAO may be a result of midlatitude wave breaking.”
• Breaking Waves at the Tropopause in the Wintertime Northern Hemisphere: Climatological Analyses of the Orientation and the Theoretical LC1/2 Classification (2007, background): “This is in good agreement with the findings of Benedict et al. (2004) and Franzke et al. (2004), who detect cyclonic wave breaking in the extratropical western Atlantic (Fig.”
• Fifty Years of Research on the Madden‐Julian Oscillation: Recent Progress, Challenges, and Perspectives (2020, background): “Earlier studies found that the AO/NAO variability is associated with wave mean flow interactions and wave breaking in the extratropics (e.g., Franzke et al., 2004; Limpasuvan & Hartmann, 1999).”