On the potential fingerprint of the Antarctic ozone hole in ice-core nitrate isotopes: a case study based on a South Pole ice core

• Published in: Atmospheric Chemistry and Physics
• Main Authors: Cao, Yanzhi, Jiang, Zhuang, Alexander, Becky, Cole-Dai, Jihong, Savarino, Joel, Erbland, Joseph, Geng, Lei
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2022
• Subjects: article; Verlagsveröffentlichung; Antarctic; South Pole; The Antarctic; Antarc*; ice core; South pole
• Online Access: https://doi.org/10.5194/acp-22-13407-2022; https://noa.gwlb.de/receive/cop_mods_00062884; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00062045/acp-22-13407-2022.pdf; https://acp.copernicus.org/articles/22/13407/2022/acp-22-13407-2022.pdf

Column ozone variability has important implications for surface photochemistry and the climate. Ice-core nitrate isotopes are suspected to be influenced by column ozone variability and δ15N(NO 3-) has been sought to serve as a proxy of column ozone variability. In this study, we examined the ability of ice-core nitrate isotopes to reflect column ozone variability by measuring δ15N(NO 3-) and Δ17O(NO 3-) in a shallow ice core drilled at the South Pole. The ice core covers the period 1944–2005, and during this period δ15N(NO 3-) showed large annual variability ((59.2 ± 29.3) ‰ ), but with no apparent response to the Antarctic ozone hole. Utilizing a snow photochemical model, we estimated 6.9 ‰ additional enrichments in δ15N(NO 3-) could be caused by the development of the ozone hole. Nevertheless, this enrichment is small and masked by the effects of the snow accumulation rate at the South Pole over the same period of the ozone hole. The Δ17O(NO 3-) record has displayed a decreasing trend by ∼ 3.4 ‰ since 1976. This magnitude of change cannot be caused by enhanced post-depositional processing related to the ozone hole. Instead, the Δ17O(NO 3-) decrease was more likely due to the proposed decreases in the O3 / HOx ratio in the extratropical Southern Hemisphere. Our results suggest ice-core δ15N(NO 3-) is more sensitive to snow accumulation rate than to column ozone, but at sites with a relatively constant snow accumulation rate, information of column ozone variability embedded in δ15N(NO 3-) should be retrievable.