3-D tomographic observations of Rossby wave breaking over the North Atlantic during the WISE aircraft campaign in 2017

• Published in: Atmospheric Chemistry and Physics
• Main Authors: Krasauskas, Lukas, Ungermann, Jörn, Preusse, Peter, Friedl-Vallon, Felix, Zahn, Andeas, Ziereis, Helmut, Rolf, Christian, Plöger, Felix, Konopka, Paul, Vogel, Bärbel, Riese, Martin
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2021
• Subjects: Atmosphärische Spurenstoffe; North Atlantic
• Online Access: https://elib.dlr.de/146023/; https://elib.dlr.de/146023/1/acp-21-10249-2021.pdf; https://acp.copernicus.org/articles/21/10249/2021/

This paper presents measurements of ozone, wa-ter vapour and nitric acid (HNO3) in the upper tropo-sphere/lower stratosphere (UTLS) over North Atlantic andEurope. The measurements were acquired with the Gim-balled Limb Observer for Radiance Imaging of the At-mosphere (GLORIA) during the Wave Driven IsentropicExchange (WISE) campaign in October 2017. GLORIAis an airborne limb imager capable of acquiring both 2-D data sets (curtains along the flight path) and, whenthe carrier aircraft is flying around the observed air mass,spatially highly resolved 3-D tomographic data. Here, wepresent a case study of a Rossby wave (RW) breakingevent observed during two subsequent flights 2 d apart. RWbreaking is known to steepen tracer gradients and facili-tate stratosphere–troposphere exchange (STE). Our measure-ments reveal complex spatial structures in stratospheric trac-ers (ozone and nitric acid) with multiple vertically stacked fil-aments. Backward-trajectory analysis is used to demonstratethat these features are related to several previous Rossbywave breaking events and that the small-scale structure ofthe UTLS in the Rossby wave breaking region, which is oth-erwise very hard to observe, can be understood as stirringand mixing of air masses of tropospheric and stratosphericorigin. It is also shown that a strong nitric acid enhancementobserved just above the tropopause is likely a result of NOxproduction by lightning activity. The measurements showedsignatures of enhanced mixing between stratospheric and tro-pospheric air near the polar jet with some transport of watervapour into the stratosphere. Some of the air masses seen in3-D data were encountered again 2 d later, stretched to verythin filament (horizontal thickness down to 30 km at some al-titudes) rich in stratospheric tracers. This repeated measure-ment allowed us to directly observe and analyse the progressof mixing processes in a thin filament over 2 d. Our resultsprovide direct insight into small-scale dynamics of the UTLSin the Rossby wave breaking region, which ...