The Formation of Wider and Deeper Clouds as a Result of Cold-Pool Dynamics

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Mechanisms for convection triggering by cold pools (2015, unknown): “As noted by various authors [e.g., Tompkins, 2001; Schlemmer and Hohenegger, 2014; Li et al., 2014], the edges of cold pools contain air parcels in which falling precipitation evaporated in the subcloud layer and, accordingly, are colder and moister than the horizontal average.”
Mechanisms of convective cloud organization by cold pools over tropical warm ocean during the AMIE/DYNAMO field campaign (2015, result): “This finding is in agreement with the "near environment" hypothesis proposed in previous studies [e.g., B€oing et al. 2012; Schlemmer and Hohenegger 2014].”
Large‐eddy simulations over Germany using ICON: a comprehensive evaluation (2017, background): “Thanks to increasing computational resources, increasingly larger domain cloud-resolving simulations are now possible (e.g. Hohenegger et al., 2008; Khairoutdinov et al., 2009; Love et al., 2011; Schlemmer and Hohenegger, 2014; Schalkwijk et al., 2015).”