Low-Wavenumber Structure and Evolution of the Hurricane Inner Core Observed by Airborne Dual-Doppler Radar
By P. Reasor, M. Montgomery, Frank D Marks, J. Gamache. 2000
329 citations recorded by the source corpus.
Subfields: Atmospheric Science, Oceanography
View Paper: https://www.semanticscholar.org/paper/9c86c7e912f6d7fc449931617f2488943ddf63a9
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Citations in the corpus
- Spiral Bands in a Simulated Hurricane. Part I: Vortex Rossby Wave Verification (2001, methodology): “Some of these bands are found to rotate around the center and propagate radially (e.g., Senn and Hiser 1959; May 1996; Gall et al. 1998; Reasor et al. 2000).”
- Nonhydrostatic, Three-Dimensional Perturbations to Balanced, Hurricane-like Vortices. Part I: Linearized Formulation, Stability, and Evolution (2002, background): “Although it is not nearly as volatile as the n (cid:53) 3 instability presented above, this more modest instability offers a simple explanation as to why persistent n (cid:53) 2 asymmetries are sometimes observed in hurricanes (Chan and Cheung 1998; Kuo et al. 1999; Reasor et al. 2000).”
- Clouds in Tropical Cyclones (2010, methodology): “Reasor et al. (2000) analyzed aircraft radar data collected in Hurricane Olivia (1994) at 0.5-h intervals for 3.5 h and found rainbands exhibiting structural and kinematic characteristics of wavenumber-1 and -2 vortex Rossby waves.”
- Two Distinct Regimes in the Kinematic and Thermodynamic Structure of the Hurricane Eye and Eyewall (2001, background): “By considering aircraft flight-level data in a select group of hurricanes, including Olivia (1994), Willoughby (1998) noted that equivalent potential temperature (ue) was typically observed to be higher in the eyewall than near the eye center, with ue differences often 10 K or more.”
- Tropical‐cyclone intensification and predictability in three dimensions (2008, background): “Many have focused on the effects of non-trivial vertical wind shear across a developing or mature vortex (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…”
- Vortex Rossby waves in a numerically simulated tropical cyclone. Part I: Overall structure, potential vorticity, and kinetic energy budgets (2002, background): “…Fairall et al. 1996), an explicit treatment of mixed ice-Unauthenticated | Downloaded 09/28/23 02:32 AM UTC phase cloud microphysics (Rutledge and Hobbs 1984; Reisner et al. 1998; Wang 1999, 2001), and a second-order horizontal diffusion with a deformation-dependent diffusion coefficient .”
- Nonhydrostatic, Three-Dimensional Perturbations to Balanced, Hurricane-Like Vortices. Part II: Symmetric Response and Nonlinear Simulations (2003, methodology): “The predominance of deep convection on the downshear side of vertically sheared storms (and its absence on the upshear side) has been extensively documented (Reasor et al. 2000; Frank and Ritchie 2001; Black et al. 2002; Corbosiero and Molinari 2002).”
- Vortex Rossby Waves in a Numerically Simulated Tropical Cyclone. Part II: The Role in Tropical Cyclone Structure and Intensity Changes* (2002, background): “Reasor et al. (2000) related the cyclonic rotation of the radar reflectivity ellipse of Hurricane Olivia (1994) to the rotation of the associated vorticity asymmetry.”
- Multiscale Observations of Hurricane Dennis (2005): The Effects of Hot Towers on Rapid Intensification (2010, methodology): “Taking into account the 1.9 8 vertical and 1.35 8 horizontal beamwidths of the TA antenna and the sampling intervals using FAST, grid resolutions from the P-3s range from 1.5–2.0 km in the horizontal to 0.5–1.0 km in the vertical (Reasor et al. 2000, 2009).”