High Ozone Isotope Anomaly at Mt. Everest Linked to Stratospheric Ozone Intrusion

Abstract Atmospheric O 3 possesses a rare isotopic signal, that is, Δ 17 O(O 3 ), varying with pressure and temperature, providing a potential tracer to explore stratosphere‐to‐troposphere transport (STT) of O 3 that plays a vital role in atmospheric chemistry and climate. However, it has been proposed that the higher stratospheric Δ 17 O(O 3 ) can't be preserved en‐route to the troposphere given the rapidly re‐established isotopic equilibrium by photochemistry. Here, we reported Δ 17 O(O 3 ) data mainly from the Tibetan Plateau, and found the relatively high Δ 17 O(O 3 ) at Mt. Everest can't be explained by in situ photochemistry. Instead, the distinct diurnal cycle with elevated nighttime value at Mt. Everest is associated with the katabatic wind bringing stratosphere‐sourced O 3 with high Δ 17 O. This demonstrates that the high Δ 17 O(O 3 ) can be preserved at troposphere at some circumstances. Given the fast transfer of Δ 17 O(O 3 ) to atmospheric nitrate, it might be potential to probe past STT of O 3 using nearby ice core records of nitrate.

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Publication Details

Journal
Geophysical Research Letters
Published
2026-02-22
DOI
https://doi.org/10.1029/2025gl121239
Primary Topic
Atmospheric Ozone and Climate
Type
article
Field-Weighted Citation Impact
0.00

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article

High Ozone Isotope Anomaly at Mt. Everest Linked to Stratospheric Ozone Intrusion

C Ye, Y. C. Xu, Zhuang Jiang, Pengfei Chen et al.
Geophysical Research Letters
Atmospheric Ozone and Climate
article

High Ozone Isotope Anomaly at Mt. Everest Linked to Stratospheric Ozone Intrusion

C Ye, Y. C. Xu, Zhuang Jiang, Pengfei Chen, Joël Savarino, Chong Zhang, Lei Geng, WeiLi Lin, Shichang Kang, Zhongyi Zhang
article en

Abstract

Abstract Atmospheric O 3 possesses a rare isotopic signal, that is, Δ 17 O(O 3 ), varying with pressure and temperature, providing a potential tracer to explore stratosphere‐to‐troposphere transport (STT) of O 3 that plays a vital role in atmospheric chemistry and climate. However, it has been proposed that the higher stratospheric Δ 17 O(O 3 ) can't be preserved en‐route to the troposphere given the rapidly re‐established isotopic equilibrium by photochemistry. Here, we reported Δ 17 O(O 3 ) data mainly from the Tibetan Plateau, and found the relatively high Δ 17 O(O 3 ) at Mt. Everest can't be explained by in situ photochemistry. Instead, the distinct diurnal cycle with elevated nighttime value at Mt. Everest is associated with the katabatic wind bringing stratosphere‐sourced O 3 with high Δ 17 O. This demonstrates that the high Δ 17 O(O 3 ) can be preserved at troposphere at some circumstances. Given the fast transfer of Δ 17 O(O 3 ) to atmospheric nitrate, it might be potential to probe past STT of O 3 using nearby ice core records of nitrate.

Geophysical Research LettersVol. 53(4)
Institut polytechnique de Grenoble (FR), University of Science and Technology of China (CN), Centre National de la Recherche Scientifique (FR), Peking University (CN), State Ethnic Affairs Commission (CN), Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement (FR), Northwest Institute of Eco-Environment and Resources (CN), Institut des Géosciences de l'Environnement (FR), Institute of Mountain Hazards and Environment (CN), Geological Exploration Technology Institute of Jiangsu Province (CN), University of Chinese Academy of Sciences (CN), Institut de Recherche pour le Développement (FR), Université Grenoble Alpes (FR)
European Commission, National Natural Science Foundation of China
Climate action
Openalex Percentile: Top 60%
Atmospheric Ozone and Climate
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