Characteristics of the Atlantic Storm-Track Eddy Activity and Its Relation with the North Atlantic Oscillation

By G. Rivière, I. Orlanski. 2005

260 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/06acb800fb07048703e6d83e56cecffb78f62043

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Citations in the corpus

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].”
Importance of Resolving Kuroshio Front and Eddy Influence in Simulating the North Pacific Storm Track (2017, background): “Previous studies have shown that accumulative effects of winter storms can contribute to large-scale mean atmospheric circulation changes (Benedict et al. 2004; Feldstein 2003; Riviere and Orlanski 2007; Vallis and Gerber 2008).”
Northern hemisphere storm tracks during the last glacial maximum in the PMIP2 ocean-atmosphere coupled models: energetic study, seasonal cycle, precipitation (2009, background): “2.4), following Orlanski (2003) and Rivière and Orlanski (2007).”
The Link between Rossby Wave Breakings and Weather Regime Transitions (2011, background): “Since then, several studies have confirmed the dynamical link between RWB and the NAO in different ways (Rivière and Orlanski 2007; Martius et al. 2007; Woolings et al. 2008; Strong and Magnusdottir 2008; Kunz et al. 2009).”
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).”
Tropospheric Rossby Wave Breaking and the NAO/NAM (2008, methodology): “5b), even though they use a different algorithm for detecting RWB, which results in fewer RWB counts.”
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 Dynamical Interpretation of the Poleward Shift of the Jet Streams in Global Warming Scenarios (2011, background): “of the North Atlantic Oscillation is shown to be accompanied by more AWB (CWB) than usual and longer (shorter) waves (Rivière and Orlanski 2007).”