Spiral Bands in a Simulated Hurricane. Part I: Vortex Rossby Wave Verification

By Yongsheng Chen, M. Yau. 2001

203 citations recorded by the source corpus.

Subfields: Atmospheric Science, Oceanography

View Paper: https://www.semanticscholar.org/paper/68186b8499fd900af0a6570f4e349114f54c866b

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Citations in the corpus

Nonhydrostatic, Three-Dimensional Perturbations to Balanced, Hurricane-like Vortices. Part I: Linearized Formulation, Stability, and Evolution (2002, background): “This result is in direct contrast with Chen and Yau (2001) and Wang (2002a,b), who show that for low-Unauthenticated wavenumber vortex-Rossby waves in three-dimensional, full-physics simulations of hurricanes, positive (negative) vertical velocities generally led or were coincident with positive 6…”
Kinematic structure of convective-scale elements in the rainbands of Hurricanes Katrina and Rita (2005) (2008, background): “…and modeling studies suggest that the pattern of mesoscale rainbands is at least partly determined by vortex Rossby waves generated in the negative potential vorticity (PV) gradient that extends from the eyewall outward [Montgomery and Kallenbach, 1997; Chen and Yau, 2001; Chen et al., 2003].”
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).”
Clouds in Tropical Cyclones (2010, background): “Although vortex Rossby wave theory has largely been studied in the context of dry vortices (Montgomery and Kallenbach 1997), fullphysics models (Chen and Yau 2001; Chen et al. 2003; Braun et al. 2006) and coastal radar data (Corbosiero et al.”
How Do Outer Spiral Rainbands Affect Tropical Cyclone Structure and Intensity (2008, background): “Recent theoretical and modeling studies have focused mainly on the formation and characteristics of inner spiral rainbands (Montgomery and Kallenbach 1997; Chen and Yau 2001; Wang 2001, 2002a,b; Schecter and Montgomery 2004, 2006, 2007).”
Secondary eyewall formation in two idealized, full-physics modeled hurricanes (2008, methodology): “This method, termed the Empirical Normal Mode Method, has been utilized in high-resolution hurricane simulations to show that the sheared spiral bands outside the primary eyewall are composed primarily of sheared vortex Rossby waves [Chen and Yau, 2001; Chen et al., 2003].”
Vortex Rossby Waves in a Numerically Simulated Tropical Cyclone. Part II: The Role in Tropical Cyclone Structure and Intensity Changes* (2002, methodology): “More recently, Chen and Yau (2001) investigated the PV bands in the near core region of a hurricane simulated with the Pennsylvania State University–National Center for Atmospheric Research fifth-generation, nonhydrostatic Mesoscale Model (MM5) and verified the existence of vortex Rossby waves in a…”
Tropical‐cyclone intensification and predictability in three dimensions (2008, background): “2004); and others have examined the structure of vortexwave asymmetries supported by the vortex itself (Chen and Yau 2001; Chenet al. 2003, Wang 2002a, 2002b).”
A Multiscale Numerical Study of Hurricane Andrew (1992). Part V: Inner-Core Thermodynamics (2002, background): “…inﬂows and outﬂows are associated with the radial and azimuthal propagation of vortex-Rossby waves, as discussed in Part IV, the distribution and magnitude of LHR in the eyewall may need to be understood in the context of vortex-Rossby waves (Montgomery and Kallenbach 1997; Chen and Yau 2001).”