The Use of Isotope Indicators in Hydrological Studies in the Taldura River Basin, Central Altai
The article presents the results of isotope studies in the Taldura River valley. Isotope characteristics of the ice of the Nekrasov Glacier and the water of rivers and streams in the middle of the ablation season are determined. The glacial feeding is shown to dominate along the entire length of the Taldura River. It is established that the meltwater of the smaller Nekrasov Glacier has a smaller effect on the feeding of the moraine lake Tamozhennoe compared to the effect of the meltwater of the Bolshaya Taldura Glacier on the runoff of the Taldura River.
Authors
- Anna Kozachek (ORCID: https://orcid.org/0000-0002-9704-8064)
- D. V. Bantcev (ORCID: https://orcid.org/0000-0002-4411-1998)
- A. A. Ovsepyan
- K. B. Tchikhatchev
- V. A. Rasputina (ORCID: https://orcid.org/0000-0001-9562-2950)
- D. A. Ganyushkin (ORCID: https://orcid.org/0000-0001-6109-8652)
Institutions
- St Petersburg University (RU)
- Arctic and Antarctic Research Institute (RU)
Publication Details
- Journal
- Water Resources
- Published
- 2024-12-01
- DOI
- https://doi.org/10.1134/s0097807824701252
- Primary Topic
- Hydrology and Watershed Management Studies
- Type
- article
- Field-Weighted Citation Impact
- 0.00