Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics
ACP
Articles | Volume 25, issue 3
Articles | Volume 25, issue 3
https://doi.org/10.5194/acp-25-1965-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-25-1965-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 25, issue 3
Research article
 | 
14 Feb 2025
Research article |  | 14 Feb 2025

Diurnal, seasonal, and interannual variations in δ(18O) of atmospheric O2 and its application to evaluate natural and anthropogenic changes in oxygen, carbon, and water cycles

Shigeyuki Ishidoya, Satoshi Sugawara, and Atsushi Okazaki

Viewed

Total article views: 2,226 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,584 246 396 2,226 71 84
  • HTML: 1,584
  • PDF: 246
  • XML: 396
  • Total: 2,226
  • BibTeX: 71
  • EndNote: 84
Views and downloads (calculated since 03 Apr 2024)
Cumulative views and downloads (calculated since 03 Apr 2024)

Viewed (geographical distribution)

Total article views: 2,226 (including HTML, PDF, and XML) Thereof 2,149 with geography defined and 77 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 31 Dec 2025
Download
Short summary
The 18O/16O ratio of atmospheric oxygen, δatm(18O), is higher than that of ocean water due to isotopic effects during biospheric activities. This is known as the Dole–Morita effect, and its millennial-scale variations are recorded in ice cores. However, small variations of δatm(18O) in the present day have never been detected so far. This paper presents the first observations of diurnal, seasonal, and secular variations in δatm(18O) and applies them to evaluate oxygen, carbon, and water cycles.
Read more
Share
Altmetrics
Final-revised paper
Preprint