The Components of the Glacial Runoff of the Tsambagarav Massif from Stable Water Isotope Data
AbstractThe 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. View Full-Text
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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. The Components of the Glacial Runoff of the Tsambagarav Massif from Stable Water Isotope Data. Geosciences 2019, 9, 297.
Bantcev DV, Ganyushkin DA, Chistyakov KV, Volkov IV, Ekaykin AA, Veres AN, Tokarev IV, Shtykova NB, Andreeva TA. The Components of the Glacial Runoff of the Tsambagarav Massif from Stable Water Isotope Data. Geosciences. 2019; 9(7):297.Chicago/Turabian Style
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. 2019. "The Components of the Glacial Runoff of the Tsambagarav Massif from Stable Water Isotope Data." Geosciences 9, no. 7: 297.
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