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Articles

Stable H and O isotope-based investigation of moisture sources and their role in river and groundwater recharge in the NE Carpathian Mountains, East-Central EuropeFootnote

, , , &
Pages 161-178 | Received 28 Sep 2018, Accepted 22 Jan 2019, Published online: 19 Mar 2019
 

ABSTRACT

The region situated between the mountain area and the lowlands in NE Romania (East-Central Europe) is experiencing increased competition for water resources triggered by a growing population, intensification of agriculture, and industrial development. To better understand hydrological cycling processes in the region, a study was conducted using stable isotopes of water and atmospheric trajectory data to characterize regional precipitation and vapour sources derived from the Atlantic Ocean, Mediterranean and Black Seas, as well as recycled continental moisture, and to assess and partition these contributions to recharge of surface and groundwater. Atmospheric moisture in the lowlands is found to be predominantly delivered along easterly trajectories, while mountainous areas appear to be dominated by North Atlantic Ocean sources, with moisture transported along mid-latitude, westerly storm tracks. Large-scale circulation patterns affect moisture delivery, the North Atlantic Oscillation being particularly influential in winter and the East Atlantic pattern in summer. Winter precipitation is the main contributor to river discharge and aquifer recharge. As winter precipitation amounts are projected to decrease over the next decades, and water abstraction is expected to steadily increase, a general reduction in water availability is projected for the region.

Acknowledgments

We thank the two reviewers and John Gibson for helpful comments that resulted in an improved article.

Disclosure statement

No potential conflict of interest was reported by the authors.

Notes

† ‘Population on 1 January by age groups and sex–functional urban areas’. Eurostat. (http://ec.europa.eu/eurostat/web/cities/data/database).

Additional information

Funding

This project was funded by grants number PN-II-RU-TE-2011-3-0235, PN-II-RU-TE-2014-4-1993, PN-III-P1-1.1-TE-2016-2210 financed by Unitatea Executivă pentru Finanțarea Învățământului Superior, a Cercetării, Dezvoltării și Inovării Romania (UEFISCDI) and RO-18452, RO-22895, financed by the International Atomic Energy Agancy (IAEA), awarded to AP. MI is funded by the Helmholtz Climate Initiative REKLIM. The EEA Financial Mechanism 2009–2014 under the project contract no CLIMFOR18SE funded C-AB and VN. This work was partially supported from contract no. 18PFE/16.10.2018 funded by the Romanian Ministry of Research and Innovation within Program 1 – Development of national research and development system, Subprogram 1.2 – Institutional Performance-RDI excellence funding projects.

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