Chlorine partitioning near the polar vortex edge observed with ground-based FTIR and satellites at Syowa Station, Antarctica, in 2007 and 2011

• Published in: Atmospheric Chemistry and Physics
• Main Authors: H. Nakajima, I. Murata, Y. Nagahama, H. Akiyoshi, K. Saeki, T. Kinase, M. Takeda, Y. Tomikawa, E. Dupuy, N. B. Jones
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2020
• Subjects: Physics; QC1-999; Chemistry; QD1-999; Syowa Station; Antarc*; Antarctica
• Online Access: https://doi.org/10.5194/acp-20-1043-2020; https://doaj.org/article/8af9cb0d11f4463c944ff7c9c4e9e96e

We retrieved lower stratospheric vertical profiles of O 3 , HNO 3 , and HCl from solar spectra taken with a ground-based Fourier transform infrared spectrometer (FTIR) installed at Syowa Station, Antarctica (69.0 ∘ S, 39.6 ∘ E), from March to December 2007 and September to November 2011. This was the first continuous measurement of chlorine species throughout the ozone hole period from the ground in Antarctica. We analyzed temporal variation of these species combined with ClO, HCl, and HNO 3 data taken with the Aura MLS (Microwave Limb Sounder) satellite sensor and ClONO 2 data taken with the Envisat MIPAS (the Michelson Interferometer for Passive Atmospheric Sounding) satellite sensor at 18 and 22 km over Syowa Station. An HCl and ClONO 2 decrease occurred from the end of May at both 18 and 22 km, and eventually, in early winter, both HCl and ClONO 2 were almost depleted. When the sun returned to Antarctica in spring, enhancement of ClO and gradual O 3 destruction were observed. During the ClO-enhanced period, a negative correlation between ClO and ClONO 2 was observed in the time series of the data at Syowa Station. This negative correlation was associated with the relative distance between Syowa Station and the edge of the polar vortex. We used MIROC3.2 chemistry–climate model (CCM) results to investigate the behavior of whole chlorine and related species inside the polar vortex and the boundary region in more detail. From CCM model results, the rapid conversion of chlorine reservoir species (HCl and ClONO 2 ) into Cl 2 , gradual conversion of Cl 2 into Cl 2 O 2 , increase in HOCl in the winter period, increase in ClO when sunlight became available, and conversion of ClO into HCl were successfully reproduced. The HCl decrease in the winter polar vortex core continued to occur due to both transport of ClONO 2 from the subpolar region to higher latitudes, providing a flux of ClONO 2 from more sunlit latitudes into the polar vortex, and the heterogeneous reaction of HCl with HOCl. The temporal variation of ...