Meteoric water δ18O across the Dinarides: Role of topography, air-mass mixing, and precipitation seasonality

Gabriela Sanchez Ortiz; Marlene Löberbauer; Nevena Andrić‐Tomašević; OLEG MANDIC; Davor Pavelić; Vedad Demir; Patrick Keys; Maud J.M. Meijers; Jeremy K.C. Rugenstein

doi:10.1016/j.ejrh.2026.103214

February 4, 2026SHILAP Revista de lepidopterologíaOpen Access

Meteoric water δ18O across the Dinarides: Role of topography, air-mass mixing, and precipitation seasonality

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Key Points

Variations in meteoric water δ18O are significantly influenced by topographic features, with higher elevations showing distinct isotopic signatures.
The study observes seasonal changes in precipitation δ18O, highlighting the role of air-mass mixing across different climatic zones.
Observed data indicates that isotopic measurements can be robust indicators of meteorological patterns within mountainous regions.
Understanding these isotopic variations enhances our knowledge of regional hydrology and climate systems.

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Implication

Analysis of meteorological conditions reveals how air-mass mixing and topography influence precipitation isotopes in the Dinarides, indicating seasonal variations.

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Ortiz et al. (2026) studied this question.

synapsesocial.com/papers/69a76025c6e9836116a2c9b4 https://doi.org/10.1016/j.ejrh.2026.103214

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Meteoric water δ18O across the Dinarides: Role of topography, air-mass mixing, and precipitation seasonality

Key Points

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Meteoric water δ18O across the Dinarides: Role of topography, air-mass mixing, and precipitation seasonality

Key Points

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