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Julian F. Quinting and Christian M. Grams

trajectories has significantly advanced our understanding of WCBs and their effect on the large-scale flow (e.g., Eckhardt et al. 2004 ; Grams et al. 2011 ; Madonna et al. 2014b ; Martínez-Alvarado et al. 2016 ). The inflow of WCBs is located in a cyclone’s warm sector ahead of the cold front (label 1 in Fig. 1 ). At this stage, air parcels still reside predominantly in the planetary boundary layer. WCB inflow is typically characterized by strong moisture flux convergence and a band of high water

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