Intensification of tilted atmospheric vortices by asymmetric diabatic heating
Tom D\"orffel, Ariane Papke, Rupert Klein, Natalia Ernst, Piotr, Smolarkiewicz

TL;DR
This paper extends the nonlinear theory of tilted vortices under asymmetric diabatic heating to low Coriolis parameters, and supports the theory with 3D simulations showing how heat release orientation affects tropical cyclone tilt and intensity.
Contribution
It generalizes the existing theory to low Coriolis regimes and demonstrates the impact of asymmetric heating on vortex dynamics through numerical simulations.
Findings
Asymmetric heating can intensify or weaken vortices depending on orientation.
The theory is valid for vortices up to low hurricane strength.
Heating orientation influences cyclone tilt and steering mechanisms.
Abstract
P\"aschke et al. (JFM, 701, 137--170 (2012)) studied the nonlinear dynamics of strongly tilted vortices subject to asymmetric diabatic heating by asymptotic methods. They found, \ia, that an azimuthal Fourier mode~1 heating pattern can intensify or attenuate such a vortex depending on the relative orientation of tilt and heating asymmetries. The theory originally addressed the gradient wind regime which, asymptotically speaking, corresponds to vortex Rossby numbers of order unity in the limit. Formally, this restricts the applicability of the theory to rather weak vortices in the near equatorial region. It is shown below that said theory is, in contrast, uniformly valid for vanishing Coriolis parameter and thus applicable to vortices up to low hurricane strengths. In addition, the paper presents an extended discussion of the asymptotics as regards their physical interpretation and their…
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Taxonomy
TopicsTropical and Extratropical Cyclones Research · Climate variability and models · Meteorological Phenomena and Simulations
