An Explicit Simulation of Tropical Cyclones with a Triply Nested Movable Mesh Primitive Equation Model: TCM3. Part II: Model Refinements and Sensitivity to Cloud Microphysics Parameterization*

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Sensitivity of Numerical Simulation of Early Rapid Intensification of Hurricane Emily (2005) to Cloud Microphysical and Planetary Boundary Layer Parameterizations (2008, methodology): “This result agrees with the numerical simulations from Lord et al. (1984) and Wang (2002) as mentioned in the introduction.”
Numerical Simulation of Hurricane Bonnie (1998). Part II: Sensitivity to Varying Cloud Microphysical Processes (2006, methodology): “Explicit hurricane simulations have now been performed using three-class ice microphysics schemes with the grid sizes of 1.5–6 km (e.g., Liu et al. 1997; Braun and Tao 2000; Wang 2001; Yau et al. 2004).”
The Maximum Intensity of Tropical Cyclones in Axisymmetric Numerical Model Simulations (2009, background): “3 The same tendency has been found in three-dimensional simulations that explicitly resolve asymmetries (see, e.g., Wang 2002b; Wu and Braun 2004; Yang et al. 2007).”