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Water Stable Isotopes in the Central Altai Mountainous Rivers as Indicator of Glacier Meltwater Fraction in Runoff. / Банцев, Дмитрий Вадимович; Распутина, Валерия Алексеевна; Овсепян, Анайит Арамовна; Грига, Семен Алексеевич; Козачек, Анна Владимировна; Чихачев, Кирилл Борисович; Ганюшкин, Дмитрий Анатольевич.

In: Water (Switzerland), Vol. 16, No. 9, 1288, 30.04.2024.

Research output: Contribution to journal › Article › peer-review

Harvard

Банцев, ДВ, Распутина, ВА, Овсепян, АА, Грига, СА, Козачек, АВ, Чихачев, КБ & Ганюшкин, ДА 2024, 'Water Stable Isotopes in the Central Altai Mountainous Rivers as Indicator of Glacier Meltwater Fraction in Runoff', Water (Switzerland), vol. 16, no. 9, 1288. https://doi.org/10.3390/w16091288

APA

Банцев, Д. В., Распутина, В. А., Овсепян, А. А., Грига, С. А., Козачек, А. В., Чихачев, К. Б., & Ганюшкин, Д. А. (2024). Water Stable Isotopes in the Central Altai Mountainous Rivers as Indicator of Glacier Meltwater Fraction in Runoff. Water (Switzerland), 16(9), [1288]. https://doi.org/10.3390/w16091288

Vancouver

Банцев ДВ, Распутина ВА, Овсепян АА, Грига СА, Козачек АВ, Чихачев КБ et al. Water Stable Isotopes in the Central Altai Mountainous Rivers as Indicator of Glacier Meltwater Fraction in Runoff. Water (Switzerland). 2024 Apr 30;16(9). 1288. https://doi.org/10.3390/w16091288

Author

Банцев, Дмитрий Вадимович ; Распутина, Валерия Алексеевна ; Овсепян, Анайит Арамовна ; Грига, Семен Алексеевич ; Козачек, Анна Владимировна ; Чихачев, Кирилл Борисович ; Ганюшкин, Дмитрий Анатольевич. / Water Stable Isotopes in the Central Altai Mountainous Rivers as Indicator of Glacier Meltwater Fraction in Runoff. In: Water (Switzerland). 2024 ; Vol. 16, No. 9.

BibTeX

@article{d507021523c94c178e434022024cbce2,
title = "Water Stable Isotopes in the Central Altai Mountainous Rivers as Indicator of Glacier Meltwater Fraction in Runoff",
abstract = "We used stable water isotopes (δ18O and δ2H) to identify the fractions of glacier meltwater and summer precipitation in the runoff in the Taldura River in the Altai mountains. The mean isotopic characteristics of glacier ice, snow, summer precipitation and river water were obtained. Using isotopic separation of hydrographs, we determined that glacier feeding completely prevails throughout the Taldura River in the middle of the ablation season. In general, the fraction of glacier meltwater in the Taldura River{\textquoteright}s runoff in the ablation season varies from 80% to 95% depending on local weather conditions.",
keywords = "glacier meltwater, glacier rivers, hydrograph separation, stable isotopes",
author = "Банцев, {Дмитрий Вадимович} and Распутина, {Валерия Алексеевна} and Овсепян, {Анайит Арамовна} and Грига, {Семен Алексеевич} and Козачек, {Анна Владимировна} and Чихачев, {Кирилл Борисович} and Ганюшкин, {Дмитрий Анатольевич}",
year = "2024",
month = apr,
day = "30",
doi = "10.3390/w16091288",
language = "English",
volume = "16",
journal = "Water (Switzerland)",
issn = "2073-4441",
publisher = "MDPI AG",
number = "9",

}

RIS

TY - JOUR

T1 - Water Stable Isotopes in the Central Altai Mountainous Rivers as Indicator of Glacier Meltwater Fraction in Runoff

AU - Банцев, Дмитрий Вадимович

AU - Распутина, Валерия Алексеевна

AU - Овсепян, Анайит Арамовна

AU - Грига, Семен Алексеевич

AU - Козачек, Анна Владимировна

AU - Чихачев, Кирилл Борисович

AU - Ганюшкин, Дмитрий Анатольевич

PY - 2024/4/30

Y1 - 2024/4/30

N2 - We used stable water isotopes (δ18O and δ2H) to identify the fractions of glacier meltwater and summer precipitation in the runoff in the Taldura River in the Altai mountains. The mean isotopic characteristics of glacier ice, snow, summer precipitation and river water were obtained. Using isotopic separation of hydrographs, we determined that glacier feeding completely prevails throughout the Taldura River in the middle of the ablation season. In general, the fraction of glacier meltwater in the Taldura River’s runoff in the ablation season varies from 80% to 95% depending on local weather conditions.

AB - We used stable water isotopes (δ18O and δ2H) to identify the fractions of glacier meltwater and summer precipitation in the runoff in the Taldura River in the Altai mountains. The mean isotopic characteristics of glacier ice, snow, summer precipitation and river water were obtained. Using isotopic separation of hydrographs, we determined that glacier feeding completely prevails throughout the Taldura River in the middle of the ablation season. In general, the fraction of glacier meltwater in the Taldura River’s runoff in the ablation season varies from 80% to 95% depending on local weather conditions.

KW - glacier meltwater

KW - glacier rivers

KW - hydrograph separation

KW - stable isotopes

UR - https://www.mendeley.com/catalogue/96cad6ae-2d66-30c2-921e-84f097d68003/

U2 - 10.3390/w16091288

DO - 10.3390/w16091288

M3 - Article

VL - 16

JO - Water (Switzerland)

JF - Water (Switzerland)

SN - 2073-4441

IS - 9

M1 - 1288

ER -

ID: 119488506