Interrelation Between Glacier Summer Mass Balance And Runoff In Mountain River Basins

Measurements of summer mass balance Bs, made over the period 1946-2016, on 56 continental glaciers, located in the basins of mountain rivers in 14 countries, were analysed for the purpose of resolving several tasks: (a) constructing physically based interrelations between river flow Wbas and Bs; (b)...

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Bibliographic Details
Published in:GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY
Main Authors: V. Konovalov, E. Rets, N. Pimankina
Other Authors: Institute of Geography RAS, in framework of scientific themes № 01482018-0008 and № 0148-2019-0004, RFBR № 16-35-60042, grants, MON RK, № АР05133077
Format: Article in Journal/Newspaper
Language:English
Published: Russian Geographical Society 2019
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Online Access:https://ges.rgo.ru/jour/article/view/661
https://doi.org/10.24057/2071-9388-2018-26
Description
Summary:Measurements of summer mass balance Bs, made over the period 1946-2016, on 56 continental glaciers, located in the basins of mountain rivers in 14 countries, were analysed for the purpose of resolving several tasks: (a) constructing physically based interrelations between river flow Wbas and Bs; (b) estimating the representativeness of local measurement of Bs for enhancement of hydrological computations and for control of modelled values Wbas; and (c) use of time series of Bs for the evaluation of norms and extrema of Wbas. Results of the study of the outlined problem serve as the basis for making the transition of local glaciological characteristics to the basin-wide level by using the relationship between runoff and summer balance of glaciers. It includes also analysis and conclusions on the spatial and temporal homogeneity of averaging glaciological mass balance data by the sampling method.