Tropospheric Rossby Wave Breaking and the NAO/NAM

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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).”
Bidimensional Diagnostics, Variability, and Trends of Northern Hemisphere Blocking (2012, methodology): “(2012), appears to be consistent with the areas of wave breaking defined in the literature (Tyrlis and Hoskins 2008b; Strong and Magnusdottir 2008).”
The Link between Rossby Wave Breakings and Weather Regime Transitions (2011, methodology): “Indeed, during AWBs, eddy momentum fluxes are essentially poleward and the zonal flow is accelerated (decelerated) north (south) of the latitude of breaking whereas during CWBs, momentum fluxes are mainly equatorward and accelerate (decelerate) the zonal flow south (north) of the latitude of breakin”
Extreme moisture transport into the Arctic linked to Rossby wave breaking (2014, background): “Although these studies focused on the subtropics, their results suggest a possible relationship between extreme moisture transport into the Arctic and RWB events which are abundant in the middle-to-high latitudes [e.g., Strong and Magnusdottir, 2008; Liu et al., 2014].”