Vortex Rossby Waves in a Numerically Simulated Tropical Cyclone. Part II: The Role in Tropical Cyclone Structure and Intensity Changes*

By Yuqing Wang. 2002

222 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/eca00b266f84811a7878bf029696937ffb7ce1fc

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Roger K. Smith
2. M. Montgomery
3. George H. Bryan
4. D. Nolan
5. Nguyen Van Sang
6. Yuqing Wang
7. R. Rotunno
8. Gary M. Lackmann

In Global and Planetary Change

1. M. Montgomery
2. Roger K. Smith
3. George H. Bryan
4. D. Nolan
5. Nguyen Van Sang
6. R. Rotunno
7. Yuqing Wang
8. K. A. Hill

In Oceanography

1. Roger K. Smith
2. M. Montgomery
3. D. Nolan
4. Yuqing Wang
5. George H. Bryan
6. Nguyen Van Sang
7. K. A. Hill
8. Gary M. Lackmann

Citations in the corpus

• Vortex Rossby waves in a numerically simulated tropical cyclone. Part I: Overall structure, potential vorticity, and kinetic energy budgets (2002, background): “The complex interactions and feedbacks between the vortex Rossby waves and the eyewall convection and their role structure and intensity changes of the simulated tropical cyclone will be addressed in Part II (Wang 2002) of this series.”
• Why Rolls are Prevalent in the Hurricane Boundary Layer (2005, background): “Even so, recent studies suggest that hurricane rainbands are not associated with BL instabilities (Chen and Yau 2001; Wang 2002).”
• Influence of Environmental Humidity on Tropical Cyclone Size (2009, background): “…studies have demonstrated that vortex Rossby waves can alter TC intensity via wave mean–flow interaction (e.g., Montgomery and Kallenbach 1997; Möller and Montgomery 1999; Wang 2002b; Chen et al. 2003) and the inward transport of diabatically generated PV (e.g., Wang 2002a; Chen and Yau 2001).”
• 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).”
• The Maximum Intensity of Tropical Cyclones in Axisymmetric Numerical Model Simulations (2009, background): “3 The same tendency has been found in three-dimensional simulations that explicitly resolve asymmetries (see, e.g., Wang 2002b; Wu and Braun 2004; Yang et al. 2007).”
• 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…”