Positive potential vorticity anomalies propagate westwards in the atmosphere.
Is it true that positive potential vorticity anomalies propagate westwards in the atmosphere?
Yes. Positive potential vorticity anomalies, such as troughs and ridges associated with Rossby wave packets in the atmosphere, propagate westward relative to the mean flow or via upstream wave dispersion.
Verdict: SUPPORTED · 3 sources for, 0 against · Last checked
The retrieved papers examine potential vorticity dynamics, Rossby wave packets, and their propagation mechanisms in the atmosphere, consistently supporting the principle that PV anomalies propagate westward in the context of Rossby wave dynamics and wave packet evolution.
Get citation
Teubler, F. & Riemer, M. (2016). Dynamics of Rossby Wave Packets in a Quantitative Potential Vorticity–Potential Temperature Framework. doi.org. https://doi.org/10.1175/jas-d-15-0162.1
See more details
Get citation
Harvey, B. J., Methven, J., & Ambaum, M. H. P. (2016). Rossby wave propagation on potential vorticity fronts with finite width. doi.org. https://doi.org/10.1017/jfm.2016.180
Get citation
Teubler, F. & Riemer, M. (2020). Potential-Vorticity Dynamics of Troughs and Ridges within Rossby Wave Packets during a 40-year reanalysis period. doi.org. https://doi.org/10.5194/wcd-2020-52
What does the evidence say?
The retrieved papers examine potential vorticity dynamics, Rossby wave packets, and their propagation mechanisms in the atmosphere, consistently supporting the principle that PV anomalies propagate westward in the context of Rossby wave dynamics and wave packet evolution.
Receipt History
Challenge the receipt
Citation formatting by citeproc-js (Frank Bennett) and the Citation Style Language project. Source and licenses.
Terms · Privacy · How verdicts work