Articles | Volume 30, issue 9
https://doi.org/10.5194/hess-30-2859-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-30-2859-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Moisture origins affecting sub-daily precipitation δ18O and d-excess values mapped in Western Europe
CATchment and ecohydrology research group, Environmental sensing and modelling research unit (ENVISION), Luxembourg Institute of Science and Technology, 4422 Belvaux, Luxembourg
Faculty of Science, Technology and Medicine, University of Luxembourg, 4365 Esch/Alzette, Luxembourg
Christoph J. Gey
Institute of Geosciences, University of Mainz, 55122 Mainz, Germany
Bernd R. Schöne
Institute of Geosciences, University of Mainz, 55122 Mainz, Germany
CATchment and ecohydrology research group, Environmental sensing and modelling research unit (ENVISION), Luxembourg Institute of Science and Technology, 4422 Belvaux, Luxembourg
Faculty of Science, Technology and Medicine, University of Luxembourg, 4365 Esch/Alzette, Luxembourg
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Short summary
Stable isotopes of oxygen (O16/O18) are powerful tools in eco-hydrology. Yet, a limitation is that the influence of atmospheric circulation on precipitation isotope signals is not well known. Here, we mapped isotope signals from different moisture origins with an air mass trajectory model, revealing contrasted contributions to precipitation isotope signals in Western Europe. These insights are key for interpreting isotope signals to assess changes in the water cycle.
Stable isotopes of oxygen (O16/O18) are powerful tools in eco-hydrology. Yet, a limitation is...