A New Look at the Problem of Tropical Cyclones in Vertical Shear Flow: Vortex Resiliency
By P. Reasor, M. Montgomery, L. Grasso. 2004
270 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/f03dae52ed32207caf7f1eb9556bcb159266d84d
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Citations in the corpus
- A new paradigm for intensity modification of tropical cyclones: Thermodynamic impact of vertical wind shear on the inflow layer (2009, background): “Dispersion and subsequent inviscid damping of sheared VRWs can also lead to the rapid reduction of vortex tilt (Schecter and Montgomery, 2003; Reasor et al., 2004).”
- Tropical‐cyclone intensification and predictability in three dimensions (2008, background): “…(e.g. Frank and Ritchie, 1999; Reasor et al., 2000; Frank and Ritchie, 2001; Black et al., 2002; Schecter and Montgomery, 2003; Rogers et al., 2003; Reasor et al., 2004); others have examined the structure of vortex-wave * Correspondence to: Michael T. Montgomery, Department of Meteorology, Naval…”
- A Vortical Hot Tower Route to Tropical Cyclogenesis. (2006, background): “If the shear is not strong enough to tear the MCV apart (e.g., Reasor et al. 2004), the shear will stimulate convection near the radius of maximum tangential velocity in the downshear direction (Ritchie and Holland 1997, p. 1380; Trier et al. 2000).”
- Tropical cyclogenesis in a tropical wave critical layer: easterly waves (2008, background): “The proto-vortex of a nascent TC, however, lacks a strong transport barrier (cf. McIntyre, 1989, 1993; Montgomery and Kallenbach, 1997; Bassom and Gilbert, 1999; Moulin and Flor, 2005) and is vulnerable to dry-air intrusion and vertical shear (e.g., Reasor et al., 2004).”
- Multiscale Structure and Evolution of Hurricane Earl (2010) during Rapid Intensification (2015, background): “…with what has been shown in theoretical, numerical, and observational studies of vortices in shear (e.g., Jones 1995; Wang and Holland 1996; Rogers et al. 2003; Reasor et al. 2004; Reasor and Eastin 2012; Reasor et al. 2013), though those studies primarily considered vortices of hurricane strength.”
- Effect of environmental shear, sea‐surface temperature, and ambient moisture on the formation and predictability of tropical cyclones: An ensemble‐mean perspective (2014, background): “Recent dynamical and thermodynamical studies [Reasor and Montgomery, 2001; Reasor et al., 2004; Rappin and Nolan, 2012; Zhang and Tao, 2013] have discussed how the tilt, precession, and alignment of the TC vortex proceed under the influence of vertical wind shear.”