Breaking of Rossby waves in the stratosphere. Part I. Climatology and long-term variability
a:2:{s:4:"TYPE";s:4:"HTML";s:4:"TEXT";s:150:"O.Yu. Antokhina1,2, A.V. Gochakov1,3, O.S. Zorkal’tseva2, P.N. Antokhin1, V.N. Krupchatnikov3,4";}
1V.E. Zuev Institute of Atmospheric Optics of Siberian Branch of the Russian Academy of Science, Tomsk, Russia
2Institute of Solar-Terrestrial Physics of the Siberian Branch of the RAS, Irkutsk, Russia
3Siberian Regional Hydrometeorological Research Institute, Novosibirsk, Russia
4Institute of Computational Mathematics and Mathematical Geophysics of the Siberian Branch of the RAS, Novosibirsk, Russia
Keywords: planetary wave disruption, stratosphere, stratospheric polar vortex, sudden stratospheric warming, potential vorticity, contours of potential vorticity
Abstract
The processes of planetary wave breaking (Rossby Wave Breaking - RWB) significantly contribute to variability in stratospheric circulation. Employing a previously developed method for identifying RWB, adapted for stratospheric circulation, this study analyzes the climatology and long-term variability of RWB processes in the middle stratosphere. The method is based on the analysis of potential vorticity (PV) contour geometry at the 850-K level using ERA5 data within the PV range 0-400 PVU (Potential Vorticity Units) determined based on PV field climatology. It was demonstrated that RWB processes exhibit intraseasonal peculiarities. Most frequently, waves break in the northern regions of East Asia and the Pacific Ocean from October to December and in April to March. In January and February, no areas with prevailing RWB processes were identified. We obtained statistically significant increase in the number of RWB for the first half of winter (October-December) and for the end of the winter period (March and April). For mid-winter (January and February), insignificant negative trends were obtained.
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