The Role of Entrainment in the Diurnal Cycle of Continental Convection

By A. D. Del Genio, Jingbo Wu. 2010

146 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/5ef391a2aebf82aa2df791e9ee08b26af27a2326

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Citations in the corpus

Influence of the subcloud layer on the development of a deep convective ensemble (2012, result): “This is in agreement with earlier studies by Khairoutdinov and Randall (2006), Romps and Kuang (2010a), and Del Genio and Wu (2010), who showed the absence of air”
A Comparison of TWP-ICE Observational Data with Cloud-Resolving Model Results (2012, background): “Among those focused primarily on dynamics and precipitation, several analyzed CRM dynamical behaviors under TWP-ICE conditions to inform GCM parameterization development [Wu et al., 2009; Del Genio and Wu, 2010; Wang and Liu, 2009].”
CORRIGENDUM of the MJO Transition from Shallow to Deep Convection in Cloudsat-Calipso Data and GISS GCM Simulations (2012, background): “Model E2 uses a mass flux cumulus parameterization with a cloudbase neutral buoyancy closure, a division of the mass flux into two plumes with different entrainment rates, a representation of convective downdrafts, and a diagnostic updraft speed (Del Genio et al. 2007) that interactively determines ”
Could Machine Learning Break the Convection Parameterization Deadlock? (2018, background): “In addition, the representation of the transition between shallow and deep convection is tightly related to changes in updraft entrainment [ Del Genio and Wu , 2010; D'Andrea et al. , 2014], in part due to the organization of the subcloud layer by cold pools [ Khairoutdinov and Randall , 2006;…”
Representing Equilibrium and Nonequilibrium Convection in Large-Scale Models (2014, background): “…observed diurnal cycle (as shown later), even when employing large entrainment rates in the convection scheme that are consistent with CRM data (Del Genio and Wu 2010; de Rooy et al. 2013), it is suggested that it does not reproduce the observed nonequilibrium be-tween the boundary layer forcing…”