Research output: Contribution to journal › Article › peer-review
Isotopic Composition of Glacier Ice and Meltwater in the Arid Parts of the Altai Mountains (Central Asia). / Bantcev, Dmitriy; Ganyushkin, Dmitriy; Terekhov, Anton; Ekaykin, Alexey; Tokarev, Igor; Chistyakov, Kirill.
In: Water (Switzerland), Vol. 14, No. 2, 252, 16.01.2022.Research output: Contribution to journal › Article › peer-review
}
TY - JOUR
T1 - Isotopic Composition of Glacier Ice and Meltwater in the Arid Parts of the Altai Mountains (Central Asia)
AU - Bantcev, Dmitriy
AU - Ganyushkin, Dmitriy
AU - Terekhov, Anton
AU - Ekaykin, Alexey
AU - Tokarev, Igor
AU - Chistyakov, Kirill
N1 - Publisher Copyright: © 2022 by the authors. Licensee MDPI, Basel, Switzerland.
PY - 2022/1/16
Y1 - 2022/1/16
N2 - The objective of this study is to reveal the isotopic composition of ice and meltwater in glaciated regions of South-Eastern Altai. The paper depicts differences between the isotopic composition of glacier ice from several types of glaciers and from various locations. Detected differences between the isotopic composition of glacier ice in diversified parts of the study region are related to local climate patterns. Isotopic composition of meltwater and isotopic separation for glacier rivers runoff showed that in the Tavan-Bogd massif, seasonal snow participates more in the formation of glacier runoff due to better conditions for snow accumulation on the surface of glaciers. In other research areas pure glacier meltwater prevails in runoff.
AB - The objective of this study is to reveal the isotopic composition of ice and meltwater in glaciated regions of South-Eastern Altai. The paper depicts differences between the isotopic composition of glacier ice from several types of glaciers and from various locations. Detected differences between the isotopic composition of glacier ice in diversified parts of the study region are related to local climate patterns. Isotopic composition of meltwater and isotopic separation for glacier rivers runoff showed that in the Tavan-Bogd massif, seasonal snow participates more in the formation of glacier runoff due to better conditions for snow accumulation on the surface of glaciers. In other research areas pure glacier meltwater prevails in runoff.
KW - Altai
KW - Glaciers
KW - Isotopic composition
KW - Isotopic separation
KW - Runoff
KW - glaciers
KW - CORE
KW - NORTHERN SLOPE
KW - runoff
KW - RIVER
KW - isotopic separation
KW - isotopic composition
KW - HYDROGRAPH SEPARATION
KW - MASSIF
KW - ORIGIN
KW - RUNOFF
UR - http://www.scopus.com/inward/record.url?scp=85123164717&partnerID=8YFLogxK
UR - https://www.mendeley.com/catalogue/b6135e9a-0763-3222-a39d-b9a27f76aabf/
U2 - 10.3390/w14020252
DO - 10.3390/w14020252
M3 - Article
AN - SCOPUS:85123164717
VL - 14
JO - Water (Switzerland)
JF - Water (Switzerland)
SN - 2073-4441
IS - 2
M1 - 252
ER -
ID: 92115204