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- W2124526794 abstract "Stratospheric conditions affect the tropospheric circulation on a variety of time-scales. This article addresses two issues in stratosphere–troposphere interaction that are relevant for time-scales up to a week: the basic growth mechanisms involved and the role of the stratospheric shear. Idealized simulations are conducted of initially stratospheric perturbations that maximize tropospheric total disturbance energy with a lead time of 5 days, assuming linear quasi-geostrophic dynamics and simplified zonal flow. The evolution is analysed in terms of the basic interactions between three Rossby-wave components. On the f-plane (constant Coriolis parameter), the three-component analysis is very accurate (the error stays within 1% of vertically integrated total energy) because all available growth mechanisms are captured. Energy growth occurs initially through the Orr mechanism, subsequently through resonance and finally through (normal-mode) shear instability. On the β-plane (Coriolis parameter varying linearly with latitude), errors increase because westward retrogression of the untilting potential vorticity structure is neglected by the three-component model. Further study reveals that the tropospheric energy growth strongly depends on the value of the stratospheric shear. Copyright © 2011 Royal Meteorological Society" @default.
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- W2124526794 date "2011-01-01" @default.
- W2124526794 modified "2023-09-26" @default.
- W2124526794 title "Evolution of stratosphere-troposphere singular vectors" @default.
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- W2124526794 doi "https://doi.org/10.1002/qj.786" @default.
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