Institute for Marine and Atmospheric research Utrecht (IMAU), Physics Department, Science Faculty, Utrecht University, Princetonplein 5, 3584 CC Utrecht, the Netherlands
now at: The Terrestrial Ecosystem Analysis Group, Institute of Geography, People and Processes, Department of Geosciences and Natural Resource Management, Science Faculty, University of Copenhagen, Øster Voldgade 10, 1350 Copenhagen K, Copenhagen, Denmark
Copernicus Institute of Sustainable Development, Utrecht University, Princetonlaan 8a, 3584 CB Utrecht, the Netherlands
Neha Mehendale
Institute for Marine and Atmospheric research Utrecht (IMAU), Physics Department, Science Faculty, Utrecht University, Princetonplein 5, 3584 CC Utrecht, the Netherlands
now at: Institute for Environmental Physics, University of Bremen, Otto-Hahn-Allee 1, 28359 Bremen, Germany
Institute for Marine and Atmospheric research Utrecht (IMAU), Physics Department, Science Faculty, Utrecht University, Princetonplein 5, 3584 CC Utrecht, the Netherlands
Meteorology and Air Quality, Wageningen University, Wageningen, the Netherlands
Institute for Marine and Atmospheric research Utrecht (IMAU), Physics Department, Science Faculty, Utrecht University, Princetonplein 5, 3584 CC Utrecht, the Netherlands
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1,943
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2,142
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Supplement: 74
BibTeX: 41
EndNote: 54
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293
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HTML: 293
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Total article views: 2,594 (including HTML, PDF, and XML)
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Total article views: 2,142 (including HTML, PDF, and XML)
Thereof 2,103 with geography defined
and 39 with unknown origin.
Total article views: 452 (including HTML, PDF, and XML)
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This study presents high-precision measurements of ∆′17O(CO2). Key findings include the extension of the N2O–∆′17O correlation to the upper troposphere and the identification of significant differences in the N2O–∆′17O slope in StratoClim samples. Additionally, the ∆′17O measurements are used to estimate global stratospheric production and surface removal of ∆′17O, providing an independent estimate of global vegetation CO2 exchange.
This study presents high-precision measurements of ∆′17O(CO2). Key findings include the...