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1. The role of stratospheric ozone for Arctic-midlatitude linkages

2. Origin of Tropospheric Air Masses in the Tropical West Pacific and related transport processes inferred from balloon-borne Ozone and Water Vapour observations from Palau

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3. Near‐Complete Local Reduction of Arctic Stratospheric Ozone by Severe Chemical Loss in Spring 2020

4. Origin of Tropospheric Air Masses in the Tropical West Pacific identified by Balloon-borne Ozone and Water Vapor Measurements from Palau

5. Pollution trace gas distributions and their transport in the Asian monsoon upper troposphere and lowermost stratosphere during the StratoClim campaign 2017

6. Near complete local reduction of Arctic stratospheric ozone by severe chemical loss in spring 2020

7. Climate change favours large seasonal loss of Arctic ozone

8. A quantitative analysis of the reactions involved in stratospheric ozone depletion in the polar vortex core

9. Update of the Polar SWIFT model for polar stratospheric ozone loss (Polar SWIFT version 2)

10. Ammonium nitrate particles formed in upper troposphere from ground ammonia sources during Asian monsoons

11. The Extrapolar SWIFT model (version 1.0): fast stratospheric ozone chemistry for global climate models

12. A Lagrangian convective transport scheme including a simulation of the time air parcels spend in updrafts

13. Polar stratospheric cloud evolution and chlorine activation measured by CALIPSO and MLS, and modeled by ATLAS

14. Update of the SWIFT model for polar stratospheric ozone loss (SWIFT version 2)

15. A quantitative analysis of the reactions involved in stratospheric polar ozone depletion

16. Technical Note: SWIFT – a fast semi-empirical model for polar stratospheric ozone loss

17. The link between springtime total ozone and summer UV radiation in Northern Hemisphere extratropics

18. Influence of transport and mixing in autumn on stratospheric ozone variability over the Arctic in early winter

19. Persistence of ozone anomalies in the Arctic stratospheric vortex in autumn

20. Sensitivity of stratospheric Bry to uncertainties in very short lived substance emissions and atmospheric transport

21. Unprecedented Arctic ozone loss in 2011

22. The Lagrangian chemistry and transport model ATLAS: simulation and validation of stratospheric chemistry and ozone loss in the winter 1999/2000

23. Water vapour transport in the tropical tropopause region in coupled Chemistry-Climate Models and ERA-40 reanalysis data

24. First quasi-Lagrangian in-situ measurements of Antarctic Polar springtime ozone: observed ozone loss rates from the Concordiasi long-duration balloon campaign

25. A~tropical West Pacific OH minimum and implications for stratospheric composition

26. SMILES zonal and diurnal variation climatology of stratospheric and mesospheric trace gasses: O 3 , HCl, HNO 3 , ClO, BrO, HOCl, HO 2 , and temperature

27. The spring 2011 final stratospheric warming above Eureka: anomalous dynamics and chemistry

28. Uncertainties in modeling heterogeneous chemistry and Arctic ozone depletion in the winter 2009/2010

29. Relative importance of dynamical and chemical contributions to Arctic wintertime ozone

30. Polar stratospheric chlorine kinetics from a self-match flight during SOLVE-II/EUPLEX

31. Variations of the residual circulation in the northern hemispheric winter

32. A process-oriented regression model for column ozone

33. Statistical modeling of total ozone: Selection of appropriate explanatory variables

34. Ozonesonde observations in the Arctic during 1989–2003: Ozone variability and trends in the lower stratosphere and free troposphere

35. On the turnaround of stratospheric ozone trends deduced from the reevaluated Umkehr record of Arosa, Switzerland

36. Variability and trends in total and vertically resolved stratospheric ozone

37. Variability and trends in total and vertically resolved stratospheric ozone based on the CATO ozone data set

38. On the possible causes of recent increases in NH total ozone from a statistical analysis of satellite data from 1979 to 2003

39. Influence of tropospheric SO2emissions on particle formation and the stratospheric humidity

40. Integrated equivalent latitude as a proxy for dynamical changes in ozone column