Comparative Analysis of the Generalized Omega Equation and Generalized Vertical Motion Equation
Author:
Publisher
Springer Science and Business Media LLC
Subject
Atmospheric Science
Link
https://link.springer.com/content/pdf/10.1007/s00376-022-1435-5.pdf
Reference21 articles.
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2. Davies-Jones, R., 1991: The frontogenetical forcing of secondary circulations. Part I: The duality and generalization of the Q vector. J. Atmos. Sci., 48(4), 497–509, https://doi.org/10.1175/1520-0469(1991)048<0497:TFFOSC>2.0.CO;2.
3. Dixon, M. A. G., A. J. Thorpe, and K. A. Browning, 2003: Layer-wise attribution of vertical motion and the influence of potential-vorticity anomalies on synoptic development. Quart. J. Roy. Meteor. Soc., 129, 1761–1778, https://doi.org/10.1256/qj.02.83.
4. Gao, S. T., and Y. S. Zhou, 2019: Progress in dynamics of mesoscale vortex in recent years. Torrential Rain and Disasters, 38(5), 431–439, https://doi.org/10.3969/j.issn.1004-9045.2019.05.005. (in Chinese with English abstract)
5. Gao, S. T., X. R. Wang, and Y. S. Zhou, 2004: Generation of generalized moist potential vorticity in a frictionless and moist adiabatic flow. Geophys. Res. Lett., 31(12), L12113, https://doi.org/10.1029/2003GL019152.
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