Standard

The Components of the Glacial Runoff of the Tsambagarav Massif from Stable Water Isotope Data. / Bantcev, Dmitry V. ; Ganyushkin, Dmitry A. ; Chistyakov, Kirill V. ; Volkov, Ilya V. ; Ekaykin, Alexey A. ; Veres, Arina N. ; Tokarev, Igor V. ; Shtykova , Natalya B. ; Andreeva, Tatiana A. .

в: Geosciences (Switzerland), Том 9, № 7, 297, 07.2019.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Bantcev, DV, Ganyushkin, DA, Chistyakov, KV, Volkov, IV, Ekaykin, AA, Veres, AN, Tokarev, IV, Shtykova , NB & Andreeva, TA 2019, 'The Components of the Glacial Runoff of the Tsambagarav Massif from Stable Water Isotope Data', Geosciences (Switzerland), Том. 9, № 7, 297. https://doi.org/10.3390/geosciences9070297

APA

Bantcev, D. V., Ganyushkin, D. A., Chistyakov, K. V., Volkov, I. V., Ekaykin, A. A., Veres, A. N., Tokarev, I. V., Shtykova , N. B., & Andreeva, T. A. (2019). The Components of the Glacial Runoff of the Tsambagarav Massif from Stable Water Isotope Data. Geosciences (Switzerland), 9(7), [297]. https://doi.org/10.3390/geosciences9070297

Vancouver

Bantcev DV, Ganyushkin DA, Chistyakov KV, Volkov IV, Ekaykin AA, Veres AN и пр. The Components of the Glacial Runoff of the Tsambagarav Massif from Stable Water Isotope Data. Geosciences (Switzerland). 2019 Июль;9(7). 297. https://doi.org/10.3390/geosciences9070297

Author

Bantcev, Dmitry V. ; Ganyushkin, Dmitry A. ; Chistyakov, Kirill V. ; Volkov, Ilya V. ; Ekaykin, Alexey A. ; Veres, Arina N. ; Tokarev, Igor V. ; Shtykova , Natalya B. ; Andreeva, Tatiana A. . / The Components of the Glacial Runoff of the Tsambagarav Massif from Stable Water Isotope Data. в: Geosciences (Switzerland). 2019 ; Том 9, № 7.

BibTeX

@article{b727df90f461425ebb0d3fee89a21709,
title = "The Components of the Glacial Runoff of the Tsambagarav Massif from Stable Water Isotope Data",
abstract = "The aim of this study was to determine the contribution of snow and glacial ice to the river fluxes, and to identify the type of ice formation in the Tsambagarav massif (the northwestern part of Mongolia). The main method for this study was isotopic analysis of water samples. The isotopic separation showed that the shares of the main components in the total runoff differed for different rivers of the massif. Alongside with that, glacial meltwater prevailed in all the investigated fluxes. The share of snow and firn in the meltwater coming from the surface of the large valley glaciers in the middle of the ablation season in 2017 changed by only 10%—from 20% to 30%. Thus, further reduction of glaciation caused by global climate change could significantly affect the water balance of the study area. The isotopic composition of glacial ice proves that its alimentation primarily comes from precipitation during the transitional seasons. Superimposed ice is not the basis for nourishment of the glaciers of the Tsambagarav massif.",
keywords = "Altai, Glaciers, Inner Asia, Runo, Stable isotopes, glaciers, stable isotopes, NORTH, runoff, RIVER, MOUNTAINS",
author = "Bantcev, {Dmitry V.} and Ganyushkin, {Dmitry A.} and Chistyakov, {Kirill V.} and Volkov, {Ilya V.} and Ekaykin, {Alexey A.} and Veres, {Arina N.} and Tokarev, {Igor V.} and Shtykova, {Natalya B.} and Andreeva, {Tatiana A.}",
year = "2019",
month = jul,
doi = "10.3390/geosciences9070297",
language = "English",
volume = "9",
journal = "Geosciences (Switzerland)",
issn = "2076-3263",
publisher = "MDPI AG",
number = "7",

}

RIS

TY - JOUR

T1 - The Components of the Glacial Runoff of the Tsambagarav Massif from Stable Water Isotope Data

AU - Bantcev, Dmitry V.

AU - Ganyushkin, Dmitry A.

AU - Chistyakov, Kirill V.

AU - Volkov, Ilya V.

AU - Ekaykin, Alexey A.

AU - Veres, Arina N.

AU - Tokarev, Igor V.

AU - Shtykova , Natalya B.

AU - Andreeva, Tatiana A.

PY - 2019/7

Y1 - 2019/7

N2 - The aim of this study was to determine the contribution of snow and glacial ice to the river fluxes, and to identify the type of ice formation in the Tsambagarav massif (the northwestern part of Mongolia). The main method for this study was isotopic analysis of water samples. The isotopic separation showed that the shares of the main components in the total runoff differed for different rivers of the massif. Alongside with that, glacial meltwater prevailed in all the investigated fluxes. The share of snow and firn in the meltwater coming from the surface of the large valley glaciers in the middle of the ablation season in 2017 changed by only 10%—from 20% to 30%. Thus, further reduction of glaciation caused by global climate change could significantly affect the water balance of the study area. The isotopic composition of glacial ice proves that its alimentation primarily comes from precipitation during the transitional seasons. Superimposed ice is not the basis for nourishment of the glaciers of the Tsambagarav massif.

AB - The aim of this study was to determine the contribution of snow and glacial ice to the river fluxes, and to identify the type of ice formation in the Tsambagarav massif (the northwestern part of Mongolia). The main method for this study was isotopic analysis of water samples. The isotopic separation showed that the shares of the main components in the total runoff differed for different rivers of the massif. Alongside with that, glacial meltwater prevailed in all the investigated fluxes. The share of snow and firn in the meltwater coming from the surface of the large valley glaciers in the middle of the ablation season in 2017 changed by only 10%—from 20% to 30%. Thus, further reduction of glaciation caused by global climate change could significantly affect the water balance of the study area. The isotopic composition of glacial ice proves that its alimentation primarily comes from precipitation during the transitional seasons. Superimposed ice is not the basis for nourishment of the glaciers of the Tsambagarav massif.

KW - Altai

KW - Glaciers

KW - Inner Asia

KW - Runo

KW - Stable isotopes

KW - glaciers

KW - stable isotopes

KW - NORTH

KW - runoff

KW - RIVER

KW - MOUNTAINS

UR - http://www.scopus.com/inward/record.url?scp=85069631854&partnerID=8YFLogxK

UR - http://www.mendeley.com/research/components-glacial-runoff-tsambagarav-massif-stable-water-isotope-data

U2 - 10.3390/geosciences9070297

DO - 10.3390/geosciences9070297

M3 - Article

VL - 9

JO - Geosciences (Switzerland)

JF - Geosciences (Switzerland)

SN - 2076-3263

IS - 7

M1 - 297

ER -

ID: 44994511