Research Article

The Role of Rossby-Wave Propagation in a North American Extreme Cold Event

Figure 5

Longitude-pressure cross-sections of the daily 50°–70°N mean zonal anomaly of geopotential height (contours; gpm), WAF (vectors: >60 m2 s−2 only), and WAFz (shading; m2 s−2) of PWs 1 and 2 in January 2014 ((a1)–(a5)). ((b1)–(b5)) As in ((a1)–(a5)), respectively, but for the geopotential height anomaly (contours; m) and temperature (shading; K). WAF components are scaled by horizontally and by vertically.