Identification of changes in the regime of small mountain streams with glacial feeding (on the example of the Barkraksay river)

Based on the data of field observations, the regime of the Barkraksay runoff, formed from the melting of Barkrak glaciers located in the Pskem basin, and its hydrological indicators were studied. The indicators of water levels observed at the temporarily installed upper and lower hydrological gauges in Barkraksay were determined. As a result, fluctuations of water level of Barkraksay depending on air and water temperature were determined and statistically analyzed.

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