Atmosphere, Volume 16, Issue 9
2025 September - 118 articles
Cover Story: The stratosphere–troposphere exchange (STE) of air mass and ozone modulates the composition, radiative balance, and dynamics of both atmospheric layers. With tropospheric ozone concentrations expected to increase in a warming climate, it is increasingly important to accurately quantify the upward and downward ozone fluxes between the troposphere and the stratosphere. A previous study applied a lower stratosphere mass budget approach, with the 380 K isentropic surface serving as the upper boundary of the lowermost stratosphere. This study employs a dynamic isentropic surface fitted to the tropical tropopause, providing an update to the results using the static 380 K boundary. With our refined methodology, we obtain a higher estimate of the global net downward ozone flux into the troposphere than previously reported. View this paper - Issues are regarded as officially published after their release is announced to the table of contents alert mailing list .
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