A Benchmark Simulation for Moist Nonhydrostatic Numerical Models

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Influence of entrainment on the thermal stratification in simulations of radiative‐convective equilibrium (2013, methodology): “[6] We describe results from three-dimensional simulations of radiative-convective equilibrium (RCE) over a wide range of sea surface temperatures (SSTs) and atmospheric CO2 concentrations using version 16 of the Bryan Cloud Model [Bryan and Fritsch, 2002].”
Resolution Requirements for the Simulation of Deep Moist Convection (2003, methodology): “The numerical model used for this study is described in Bryan and Fritsch (2002) and Bryan (2002).”
Deep moist atmospheric convection in a subkilometer global simulation (2013, methodology): “Previous numerical studies using a limited numerical domain, but without parameterization, have demonstrated the resolution dependence of convection features [Weisman et al., 1997; Bryan and Fritsch, 2002; Petch et al., 2002; Bryan et al., 2003].”
The Maximum Intensity of Tropical Cyclones in Axisymmetric Numerical Model Simulations (2009, methodology): “The second formulation, derived by Bryan and Fritsch (2002) and hereafter referred to as the ‘‘conservative equation set,’’ allows the total mass and internal energy to be conserved in a reversible moist environment, and the appropriate formulations are P1 5 Rdcpm cpcym , P2 5 Rd cp Ly cymu p Rycpm…”