31 citations as recorded by crossref.

1. Intercomparison of Ground- and Satellite-Based Total Ozone Data Products at Marambio Base, Antarctic Peninsula Region K. Čížková et al.
2. Projecting ozone hole recovery using an ensemble of chemistry–climate models weighted by model performance and independence M. Amos et al.
3. Incorporating diversity in cloud-computing: a novel paradigm and architecture for enhancing the performance of future cloud radio access networks A. Periola
4. Large uncertainties in global hydroxyl projections tied to fate of reactive nitrogen and carbon L. Murray et al.
5. Potential of future stratospheric ozone loss in the midlatitudes under global warming and sulfate geoengineering S. Robrecht et al.
6. Very short-lived halogens amplify ozone depletion trends in the tropical lower stratosphere J. Villamayor et al.
7. Key drivers of ozone change and its radiative forcing over the 21st century F. Iglesias-Suarez et al.
8. Reappraisal of the Climate Impacts of Ozone‐Depleting Substances O. Morgenstern et al.
9. Diverse policy implications for future ozone and surface UV in a changing climate A. Butler et al.
10. Evaluating stratospheric ozone and water vapour changes in CMIP6 models from 1850 to 2100 J. Keeble et al.
11. Is our dynamical understanding of the circulation changes associated with the Antarctic ozone hole sensitive to the choice of reanalysis dataset? A. Orr et al.
12. A brief review of health-related issues occurring in urban areas related to global warming of 1.5°C J. Bartholy & R. Pongrácz
13. Polar stratospheric clouds initiated by mountain waves in a global chemistry–climate model: a missing piece in fully modelling polar stratospheric ozone depletion A. Orr et al.
14. On ozone trend detection: using coupled chemistry–climate simulations to investigate early signs of total column ozone recovery J. Keeble et al.
15. Projected future changes in bomb cyclones by the HighResMIP-PRIMAVERA multimodel ensemble J. Gao et al.
16. Prescribing Zonally Asymmetric Ozone Climatologies in Climate Models: Performance Compared to a Chemistry‐Climate Model C. Rae et al.
17. The Response of the Ozone Layer to Quadrupled CO2 Concentrations G. Chiodo et al.
18. The recent signs of total column ozone recovery over mid-latitudes: The effects of the Montreal Protocol mandate S. Ningombam et al.
19. Diagnosing the radiative and chemical contributions to future changes in tropical column ozone with the UM-UKCA chemistry–climate model J. Keeble et al.
20. Non‐additive response of the high‐latitude Southern Hemisphere climate to aerosol forcing in a climate model with interactive chemistry J. Pope et al.
21. Ozone—climate interactions and effects on solar ultraviolet radiation A. Bais et al.
22. Attribution of Stratospheric and Tropospheric Ozone Changes Between 1850 and 2014 in CMIP6 Models G. Zeng et al.
23. Effect of lower stratospheric temperature on total ozone column (TOC) during the ozone depletion and recovery phases S. Ningombam et al.
24. Glacial melt disturbance shifts community metabolism of an Antarctic seafloor ecosystem from net autotrophy to heterotrophy U. Braeckman et al.
25. Twenty-first-century Southern Hemisphere impacts of ozone recovery and climate change from the stratosphere to the ocean I. Ivanciu et al.
26. Tropospheric Ozone Assessment Report: Assessment of global-scale model performance for global and regional ozone distributions, variability, and trends P. Young et al.
27. Future changes in surface ozone over the Mediterranean Basin in the framework of the Chemistry-Aerosol Mediterranean Experiment (ChArMEx) N. Jaidan et al.
28. Sulfur dioxide emissions in Portugal: Prediction, estimation and air quality regulation using machine learning V. Ribeiro
29. Impact of Methane Emissions on Future Stratospheric Ozone Recovery N. Liu et al.
30. Quantifying contributions of ozone changes to global and arctic warming during the second half of the twentieth century Y. Hu et al.
31. Reconstruction and analysis of erythemal UV radiation time series from Hradec Králové (Czech Republic) over the past 50 years K. Čížková et al.