Regional characteristics of atmospheric sulfate formation in East Antarctica imprinted on 17 O-excess signature

• Published in: Journal of Geophysical Research: Atmospheres
• Main Authors: Ishino, Sakiko, Hattori, Shohei, Legrand, Michel, Chen, Q., Alexander, Becky, Shao, J., Huang, J., Jaeglé, L., Jourdain, Bruno, Preunkert, Suzanne, Yamada, A., Yoshida, Naohiro, Savarino, Joël
• Other Authors: Tokyo Institute of Technology Tokyo (TITECH), Institut des Géosciences de l’Environnement (IGE), Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ), Université Grenoble Alpes (UGA), University of Washington Seattle
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2021
• Subjects: [SDU.OCEAN]Sciences of the Universe [physics]/Ocean; Atmosphere; [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology; [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry; Antarctic; Austral; Dumont d'Urville; Dumont-d'Urville; East Antarctica; Antarc*; Antarctica
• Online Access: https://hal.science/hal-03402190; https://hal.science/hal-03402190/document; https://hal.science/hal-03402190/file/885769_1_merged_1606359882.pdf; https://doi.org/10.1029/2020JD033583

International audience 17O-excess (Δ17O = δ17O − 0.52 × δ18O) of sulfate trapped in Antarctic ice cores has been proposed as a potential tool for assessing past oxidant chemistry, while insufficient understanding of atmospheric sulfate formation around Antarctica hampers its interpretation. To probe...