Vortex Rossby waves in a numerically simulated tropical cyclone. Part I: Overall structure, potential vorticity, and kinetic energy budgets

By Yuqing Wang. 2002

236 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/8184b26e42dc49cf1acde491f7b2d779e6272587

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Citations in the corpus

Tropical cyclogenesis sensitivity to environmental parameters in radiative–convective equilibrium (2007, unknown): “While earlier cloud-resolving simulations showed realistic dynamics using resolutions of 5–6 km (Liu et al., 1997; Frank and Ritchie, 2001; Wang, 2002), the apparent realism of the inner-core processes has increased steadily as the grid spacing has been further decreased from 5 to 3 to 1.67 km…”
Evaluation of Planetary Boundary Layer Parameterizations in Tropical Cyclones by Comparison of In Situ Observations and High-Resolution Simulations of Hurricane Isabel (2003). Part I: Initialization, Maximum Winds, and the Outer-Core Boundary Layer (2009, background): “As the grid spacings have decreased from 6 to 5 km (e.g., Liu et al. 1997; Wang 2002), to 3 to 2 km (e.”
Nonhydrostatic, Three-Dimensional Perturbations to Balanced, Hurricane-Like Vortices. Part II: Symmetric Response and Nonlinear Simulations (2003, methodology): “This will require energy equations for the nonhydrostatic, symmetric, and asymmetric motions, similar to those presented by Wang (2002), and remains for future work.”
Effects of the Cold Core Eddy on Tropical Cyclone Intensity and Structure under Idealized Air–Sea Interaction Conditions (2013, background): “Since the asymmetric structures are dominated by low-number waves (Wang 2002), the azimuthal wavenumbers-1–3 maximum radar reflectivity difference between CLD24 and CTRL is shown in Fig.”
A new paradigm for intensity modification of tropical cyclones: Thermodynamic impact of vertical wind shear on the inflow layer (2009, background): “…to zero order by a standing VRW pattern, extending outwards to radii of 150 km–200 km. Previous studies have shown that propagating rain bands in the near-core region of an unforced model TC can be approximately described as balanced features (Chen and Yau, 2001; Wang, 2002; Chen et al., 2003).”
Influence of Environmental Humidity on Tropical Cyclone Size (2009, background): “This interpretation is consistent with that of Wang (2009) and Hence and Houze (2008) in the recognition of the inertially stable inside portion of the spiral band as being dynamically favorable for a balanced response to heating in spiral bands.”
Tropical‐cyclone intensification and predictability in three dimensions (2008, methodology): “…(e.g. Zhu et al., 2001; Zhu and Smith, 2002, 2003); those using hydrostatic three-dimensional models with explicit microphysics (e.g. Wang 2001, 2002a, 2002b); and those using non-hydrostatic axisymmetric cloud models (e.g. Willoughby et al., 1984; Rotunno and Emanuel, 1987; Persing…”
Vortex Rossby Waves in a Numerically Simulated Tropical Cyclone. Part II: The Role in Tropical Cyclone Structure and Intensity Changes* (2002, methodology): “The asymmetric structure in the inner core within a radius of about 60 km is dominated by wavenumber-1 vortex Rossby waves, as already shown in Wang (2001, 2002).”
Nonhydrostatic, Three-Dimensional Perturbations to Balanced, Hurricane-like Vortices. Part I: Linearized Formulation, Stability, and Evolution (2002, background): “…due to the ever-increasing resolution of both observational techniques (Kuo et al. 1999; Reasor et al. 2000; Kossin and Eastin 2001; Daida and Barnes 2000) and numerical simulations (Liu et al. 1997, 1999; Braun et al. 2000; Braun and Tau 2000; Fulton 2001; Chen and Yau 2001; Wang 2002a,b).”