Large Scale Dynamics of Precipitation Fronts in the Tropical Atmosphere: A Novel Relaxation Limit

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The Dynamics of Idealized Convection Schemes and Their Effect on the Zonally Averaged Tropical Circulation (2007, methodology): “…therefore pushing the vertical averaged humidity away from the reference profile according to q qref SBMP. 21 A similar adjustment of humidity/temperature rather than precipitation occurs in simple models that use Betts–Miller-type convective parameterizations, such as Frierson et al. (2004).”
A Simple Multicloud Parameterization for Convectively Coupled Tropical Waves. Part I: Linear Analysis (2006, methodology): “Especially for the latter case, it is not surprising to see that the convectively coupled gravity wave instability disappears since WISHE is suppressed (MS01; M04).”
An Idealized Semi-Empirical Framework for Modeling the Madden–Julian Oscillation (2012, background): “While precipitation fronts can also occur in a quasi-linear system without nonlinear horizontal advection (Frierson et al. 2004; Stechmann and Majda 2006; Pauluis et al. 2008), here the role of nonlinear advection is apparent in the correspondence of the front location with that of strong zonal…”