Quasi-coincident observations of polar stratospheric clouds by ground-based lidar and CALIOP at Concordia (Dome C, Antarctica) from 2014 to 2018

• Published in: Atmospheric Chemistry and Physics
• Main Authors: Snels, Marcel, Colao, Francesco, Cairo, Francesco, Shuli, Ilir, Scoccione, Andrea, De Muro, Mauro, Pitts, Michael, Poole, Lamont, Di Liberto, Luca
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2021
• Subjects: article; Verlagsveröffentlichung; Antarctic; The Antarctic; Concordia Station; Antarc*; Antarctica
• Online Access: https://doi.org/10.5194/acp-21-2165-2021; https://noa.gwlb.de/receive/cop_mods_00055608; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00055259/acp-21-2165-2021.pdf; https://acp.copernicus.org/articles/21/2165/2021/acp-21-2165-2021.pdf

Polar stratospheric clouds (PSCs) have been observed from 2014 to 2018 from the lidar observatory at the Antarctic Concordia station (Dome C), included as a primary station in the NDACC (Network for Detection of Atmospheric Climate Change). Many of these measurements have been performed in coincidence with overpasses of the satellite-borne CALIOP (Cloud Aerosol Lidar with Orthogonal Polarization) lidar, in order to perform a comparison in terms of PSC detection and composition classification. Good agreement has been obtained, despite intrinsic differences in observation geometry and data sampling. This study reports, to our knowledge, the most extensive comparison of PSC observations by ground-based and satellite-borne lidars. The PSCs observed by the ground-based lidar and CALIOP form a complementary and congruent dataset and allow us to study the seasonal and interannual variations in PSC occurrences at Dome C. Moreover, a strong correlation with the formation temperature of NAT (nitric acid trihydrate), TNAT, calculated from local temperature, pressure, and H2O and HNO3 concentrations is shown. PSCs appear at Dome C at the beginning of June up to 26 km and start to disappear in the second half of August, when the local temperatures start to rise above TNAT. Rare PSC observations in September coincide with colder air masses below 18 km.