Long-term trends in synoptic-scale Rossby wave-breaking and the jet strength at tropopause levels
Francesco Isotta, Olivia Martius, M. Sprenger, Cornelia Schwierz
Abstract
Francesco Isotta, Olivia Martius, M. Sprenger, Cornelia Schwierz
Abstract
Breaking synoptic-scale Rossby waves are frequent features of the upper troposphere and lower stratosphere (UTLS) which affect both globaland regional-scale dynamics. Furthermore, they directly influence ozone distribution through meridional transport of ozone-rich air towards the south and ozone-poor air towards the north. Here, trends in the frequency of these breaking waves are assessed by analysing a 44-year climatology (1958–2002) of potential vorticity (PV) streamers on isentropic surfaces from 310 to 350 K. These streamers are viewed as breaking Rossby waves.
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Breaking synoptic-scale Rossby waves are frequent features of the upper troposphere and lower stratosphere (UTLS) which affect both globaland regional-scale dynamics. Furthermore, they directly influence ozone distribution through meridional transport of ozone-rich air towards the south and ozone-poor air towards the north. Here, trends in the frequency of these breaking waves are assessed by analysing a 44-year climatology (1958–2002) of potential vorticity (PV) streamers on isentropic surfaces from 310 to 350 K. These streamers are viewed as breaking Rossby waves.
Key concepts: Tropopause, Rossby wave, Stratosphere, Potential vorticity, Troposphere, Atmospheric sciences, Breaking wave, Climatology