Influence of the subcloud layer on the development of a deep convective ensemble

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Mechanisms for convection triggering by cold pools (2015, background): “In recent years, different authors have suggested that the subcloud layer is a crucial component in the rapid transition from shallow to deep convection [Tompkins, 2001; Chaboureau et al., 2004; Khairoutdinov and Randall, 2006; Kuang and Bretherton, 2006; Zhang and Klein, 2010; Böing et al., 2012].”
Entrainment and detrainment in cumulus convection: an overview (2013, unknown): “The mesoscale organisation associated with the cold pools supports deep convection and accelerates the transition from shallow to deep convection (Böing et al., 2012).”
The Formation of Wider and Deeper Clouds as a Result of Cold-Pool Dynamics (2014, methodology): “Surface fluxes of heat and moisture are prescribed at the lower boundary to remain comparable to other LES studies on similar topics (Kuang and Bretherton 2006; Khairoutdinov and Randall 2006; Böing et al. 2012).”
Mechanisms of convective cloud organization by cold pools over tropical warm ocean during the AMIE/DYNAMO field campaign (2015, methodology): “, B€ oing et al., 2012; Khairoutdinov and Randall, 2006; Krueger, 1988]. Tompkins [2001] proposed a different mechanism that attributes the triggering to thermodynamic processes.”