Rapid Development of the Tropical Cyclone Warm Core

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Rapid Intensification of a Sheared Tropical Storm (2010, methodology): “This is consistent with the results of Vigh and Schubert (2009) described above.”
Multiscale Structure and Evolution of Hurricane Earl (2010) during Rapid Intensification (2015, background): “5) and the heating thus has a comparatively large impact on TC intensification (Shapiro and Willoughby 1982; Schubert and Hack 1982; Hack and Schubert 1986; Nolan et al. 2007; Vigh and Schubert 2009; Pendergrass and Willoughby 2009).”
Sensitivity of tropical‐cyclone models to the surface drag coefficient in different boundary‐layer schemes (2014, methodology): “…of azimuthally-averaged tangential wind speed, Vg, at a height of 2 km for the four schemes considered and for the three ‡‡A more strict constraint on steady balance flow may be obtained from the geopotential tendency equation derived by Shapiro and Montgomery (1993) and Vigh and Schubert (2009).”
Recent Developments in the Fluid Dynamics of Tropical Cyclones (2017, unknown): “…prescribed diabatic heating, there are widely held arguments that attribute the increasingly rapid intensiﬁcation of tropical cyclones to the increasing efﬁciency of diabatic heating in the cyclone’s inner-core region associated with deep convection (e.g., Vigh & Schubert 2009, Rozoff et al. 2012).”