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• W1981587942 abstract "Multi-isotope (δ17O and δ18O) measurements of stratospheric CO2 and 14CO are reported. Samples were acquired from altitudes in excess of 11.5 km from Christchurch, New Zealand to the South Pole. A mass independent isotopic variation is observed in CO2, the magnitude of which correlates well with 14CO concentration, indicating a stratospheric source of the effect. The component arises from isotopic exchange between the product of O3 photolysis, O(¹D) and CO2 thus providing a unique measure of ozone photolysis and turnover. A similar process may occur in the Martian atmosphere, as suggested by water isotopic measurements from SNC meteorites." @default.
• W1981587942 created "2016-06-24" @default.
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• W1981587942 date "1995-02-01" @default.
• W1981587942 modified "2023-09-23" @default.
• W1981587942 title "Observation of a mass independent oxygen isotopic composition in terrestrial stratospheric CO₂, the link to ozone chemistry, and the possible occurrence in the Martian atmosphere" @default.
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• W1981587942 doi "https://doi.org/10.1029/94gl02996" @default.
• W1981587942 hasPublicationYear "1995" @default.
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