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

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Gulomjon Umirzakov
Sarkorbek Suvankulov
Halimjon Mamirov
Fahriddin Akbarov
Maxim Petrov

Abstract

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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Author Biographies

Gulomjon Umirzakov, National University of Uzbekistan named after Mirzo Ulugbek

PhD, Associate professor, lecturer at the department of meteorology and climatology

Sarkorbek Suvankulov, Institute of Geology and Geophysics named after H. M. Abdullayev

Junior scientist, Centre of glacial geology

Halimjon Mamirov, Institute of Geology and Geophysics named after H. M. Abdullayev

Junior scientist, Centre of glacial geology

Fahriddin Akbarov, Institute of Geology and Geophysics named after H. M. Abdullayev

Junior scientist, Centre of glacial geology

Maxim Petrov, Institute of Geology and Geophysics named after H. M. Abdullayev

Candidate of geological and mineralogical sciences, Head of the center of glacial geology