Earth Syst. Sci. Data, 12, 3529–3544, 2020 https://doi.org/10.5194/essd-12-3529-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Year-round record of near-surface ozone and O3 enhancement events (OEEs) at Dome A, East Antarctica Minghu Ding1,2;, Biao Tian1;, Michael C. B. Ashley3, Davide Putero4, Zhenxi Zhu5, Lifan Wang5, Shihai Yang6, Chuanjin Li2, and Cunde Xiao2,7 1State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081, China 2State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China 3School of Physics, University of New South Wales, Sydney 2052, Australia 4CNR–ISAC, National Research Council of Italy, Institute of Atmospheric Sciences and Climate, corso Fiume 4, 10133, Turin, Italy 5Purple Mountain Observatory, Chinese Academy of Sciences, Nanjing 210034, China 6Nanjing Institute of Astronomical Optics & Technology, Chinese Academy of Sciences, Nanjing 210042, China 7State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875, China These authors contributed equally to this work. Correspondence: Minghu Ding (
[email protected]) Received: 26 May 2020 – Discussion started: 5 August 2020 Revised: 4 October 2020 – Accepted: 9 November 2020 – Published: 18 December 2020 Abstract. Dome A, the summit of the East Antarctic Ice Sheet, is an area challenging to access and is one of the harshest environments on Earth. Up until recently, long-term automated observations from Dome A (DA) were only possible with very low power instruments such as a basic meteorological station.