Breaking Waves at the Tropopause in the Wintertime Northern Hemisphere: Climatological Analyses of the Orientation and the Theoretical LC1/2 Classification

By Olivia Martius, C. Schwierz, H. Davies. 2007

139 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/9b74fb1704d8604d420c2a398c51c1cce8a58276

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Citations in the corpus

Tropospheric Rossby Wave Breaking and the NAO/NAM (2008, background): “2a, for example, overlap with regions where Martius et al. (2007) show a high frequency of anticyclonic PV streamers (LC1 events in their Fig.”
Wave‐breaking characteristics of midlatitude blocking (2012, background): “It has been acknowledged that blocking has been widely studied taking into account its cyclonic and anticyclonic nature (e.g. Martius et al., 2007; Gabriel and Peters, 2008; Kunz et al., 2009), however very little has yet been said on the magnitude of the air masses involved and their importance in…”
Variability of the North Atlantic eddy‐driven jet stream (2010, unknown): “Several studies have linked variations in eddy forcing with Rossby wavebreaking events (Benedict et al., 2004; Franzke et al., 2004; Riviére and Orlanski, 2007; Martius et al., 2007; Strong and Magnusdottir, 2008; Kunz et al., 2009).”
Dynamical feedbacks and the persistence of the NAO (2009, methodology): “This figure is consistent with the PV streamer analysis of Martius et al. (2007), who show that during the high phase of the NAO most wave breaking is of the LC1 type and occurs downstream and equatorward of the jet, while the low phase exhibits wave breaking of LC2 type and poleward of the jet…”
The Link between Rossby Wave Breakings and Weather Regime Transitions (2011, methodology): “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).”