The Maximum Intensity of Tropical Cyclones in Axisymmetric Numerical Model Simulations

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Air-Sea Enthalpy and Momentum Exchange at Major Hurricane Wind Speeds Observed during CBLAST (2012, unknown): “Recent studies suggest that these discrepancies between observations and E-PI theory may be largely due to gradient wind imbalance in the boundary layer (Smith et al. 2008; Bryan and Rotunno 2009).”
Sensitivity of tropical‐cyclone models to the surface drag coefficient in different boundary‐layer schemes (2014, methodology): “Although the calculations of Bryan and Rotunno (2009) largely support Emanuel’s theoretical predictions (their Figure 6), they used an axisymmetric model also.”
Recent Developments in the Fluid Dynamics of Tropical Cyclones (2017, unknown): “…with recently observed estimates from ﬂight-level data in major hurricanes (Zhang & Montgomery 2012), the numerical studies of Persing & Montgomery (2003) and Bryan & Rotunno (2009a) to exceed signiﬁcantly the theoretically predicted PI given by Equation 18 and its modiﬁcations summarized below.”
Resolving Tropical Cyclone Intensity in Models (2018, background): “As shown by Bryan and Rotunno (2009), strong horizontal mixing limits the inward penetration of angular momentum surfaces, thus limiting the tangential wind speed.”
Evaluation of an Analytical Model for the Maximum Intensity of Tropical Cyclones (2009, methodology): “Unauthenticated | Downloaded 12/31/22 01:22 PM UTC PM03; Persing and Montgomery 2005; Cram et al. 2007; Yang et al. 2007; Bryan and Rotunno 2009a).”