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William A. Komaromi and James D. Doyle

( Braun et al. 2013 ), HS3 made it possible to not only sample the entire depth of the outflow layer, but also to sample the region in which the radial outflow originates over the deepest convection, hereafter referred to as the outflow roots . Several studies have already examined data from GRIP, focusing on both genesis and rapid intensification (e.g., Davis and Ahijevych 2013 ; Zawislak and Zipser 2014 ; Helms and Hart 2015 ; Rogers et al. 2015 ). In this study, we focus on the full quality-controlled

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