Publication Abstracts
Robinson 1985
Robinson, W.A., 1985: A model of the wave 1-wave 2 vacillation in the winter stratosphere. J. Atmos. Sci., 42, 2289-2304, doi:10.1175/1520-0469(1985)042<2289:AMOTWV>2.0.CO;2.
A three-dimensional, severely truncated, quasi-geostrophic model in a beta channel is used to explore the dynamics of the observed anticorrelation between the amplitudes of planetary waves 1 and 2 in the Northern Hemisphere winter stratosphere. The model, which includes interactions among eight horizontal modes, generates realistic wave 1-wave 2 vacillations when westward traveling wave 1 interacts with stationary waves 1 and 2. It is found that while wave 1 oscillates in response to wave-mean flow interactions, the oscillations in the amplitude of wave 2 are driven primarily by wave-wave interactions. Experiments with a barotropic model revel that the timing of the strongest wave-wave interactions is determined by the wave 1 interaction with the mean flow.
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BibTeX Citation
@article{ro05600u,
author={Robinson, W. A.},
title={A model of the wave 1-wave 2 vacillation in the winter stratosphere},
year={1985},
journal={J. Atmos. Sci.},
volume={42},
pages={2289--2304},
doi={10.1175/1520-0469(1985)042%3C2289%3AAMOTWV%3E2.0.CO;2},
}
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RIS Citation
TY - JOUR ID - ro05600u AU - Robinson, W. A. PY - 1985 TI - A model of the wave 1-wave 2 vacillation in the winter stratosphere JA - J. Atmos. Sci. VL - 42 SP - 2289 EP - 2304 DO - 10.1175/1520-0469(1985)042%3C2289%3AAMOTWV%3E2.0.CO;2 ER -
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