“…They are an obvious candidate for driving air stagnation events as they are characterised by a synopticscale, quasi-stationary anticyclone (Rex, 1950), and thus provide the weak winds and absence of precipitation that define air stagnation. Blocks have been shown to increase pollutant levels in Europe (Hamburger et al, 2011;Garrido-Perez et al, 2017;Ordoñez et al, 2017;Webber et al, 2017;Vautard et al, 2018), the United States (Comrie and Yarnal, 1992) and in Asia (Yun and Yoo, 2019). The position of the North Atlantic jet stream (Ordóñez et al, 2019), the presence of subtropical ridges (Garrido-Perez et al, 2017;Ordoñez et al, 2017) and the passage of midlatitude cyclones (Leibensperger et al, 2008;Tai et al, 2010Tai et al, , 2012Leung et al, 2018) can also influence air stagnation development and pollution levels.…”