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- W2079117514 abstract "Based on the discussion of the balanced, quasi-balanced and non-balanced dynamic characteristics in hurricanes life cycle, the potential vorticity (PV)-w inversion system is applied to analyze the hurricane Bonnie (1998), which exhibited the features of asymmetry and steady intensity. The results show that the basic vortex can be well described by the balanced flows derived through the nonlinear balanced model, whereas by adding the quasi-balanced ! equation, the quasi-balanced flows can reflect the structure of convergent inflow in planetary boundary layer (PBL), divergent outflow in upper troposphere, strong slantwise updraft in eyewall and subsidence motion in hurricane eye. Because the quasi-balanced flows can describe the organized severe convective systems with long life span and the correlative convergence motion have the same magnitude with vortex motion, the quasi-balanced flows have the co-existence feature of divergence and vorticity motions. It is found, however, that the inflow area in PBL and outflow area in upper-level contain significant unbalanced supergradient flows. Under the quasi-balanced downshear environments, the moving direction left of mesoscale severe convective bands has the favorable condition for the genesis and the development of convective cells, and the opposite of the right side. So the severe convective systems in eyewall and spiral rain bands weaken and die out as soon as propagating to moving direction right with the basic cyclonic rotational flows, which causes the formation and maintenance of asymmetric structure in eyewall and spiral rain bands." @default.
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- W2079117514 date "2008-05-01" @default.
- W2079117514 modified "2023-09-23" @default.
- W2079117514 title "The Diagnoses of Quasi-Balanced Flows in Asymmetric Intense Hurricane" @default.
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- W2079117514 doi "https://doi.org/10.1002/cjg2.1238" @default.
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