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Kuan-Ting O, Robert Wood, and Christopher S. Bretherton

observations near the top of the planetary boundary layer (PBL), scaled strongly with vertical motion within active cumulus (Cu; Wood et al. 2011 ). Further, and within POCs were found to be extremely low (~5 cm −3 in the mean), demonstrating that in-cloud collision–coalescence can be efficient in depleting and , especially in the upper MBL and prompting characterization of these layers as ultraclean layers (UCLs; Sharon et al. 2006 ; Wood et al. 2011 ). In Wood et al. (2018 , hereafter Part

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