Гідрологія, гідрохімія і гідроекологія

Hydrology, hydrochemistry and hydroecology

GOPTSIY M.V., POZDNYAKOV YU.O. ASSESSMENT OF SEASONAL RUNOFF IN THE TISZA RIVER SUB-BASIN

DOI: https://doi.org/10.17721/2306-5680.2024.4.4

Hydrology, Hydrochemistry and Hydroecology. 2024. № 4(74)
Publication language: Ukrainian
Authors:
Goptsiy M.V., Taras Shevchenko National University of Kyiv
Pozdnyakov Yu.O., Odesa Mechnikov National University

The article is devoted to the study of the water regime of the rivers of the Tisza sub-basin within Ukraine, which is critically important in the context of modern climate change, which is characterized by the growth of extreme weather events. Global warming leads to changes in the distribution of precipitation, melting of snow and glaciers, which directly affects the water regime of rivers, increasing the frequency and intensity of floods, floods and droughts, which requires the development of a strategy for adapting to changes in the water regime based on its reliable assessment. The purpose of the study is to estimate the value of the annual runoff, analyze the phases of water content and fluctuations in water content within the seasons, which allows to determine periods with a surplus or deficit of water resources.
The study is based on the analysis of observation data on daily water flows at 22 hydrological stations located on the rivers of the Tisza sub-basin for the period up to 2020. Statistical methods of time series analysis were used, in particular, determining the average values, coefficients of variation and asymmetry, and the runoff rate was determined.
The results of the study showed that the average multi-year average annual runoff module in the catchments of the rivers of the Tysa sub-basin varies from 9.71 l/(c·km²) of the Stara River – the village of Znyatsovo (F = 224 km²) in the western part of the sub-basin to 36.6 l/(c·km²) of the Kosivska River – the village of Kosivska Polyana (F = 122 km²) in the southeastern part of the sub-basin. It was established that over the past 30 years, low-water years have prevailed in most catchments, but years with high floods are also noted.
A detailed analysis of the intra-annual distribution of runoff was conducted, which showed that the largest percentage of runoff is formed in March-April (central and western parts of the sub-basin) and April-May (eastern part of the sub-basin). Summarizing the observation data, it was found that spring runoff is 38 %, summer-autumn – 40 %, and winter – 22 % of the annual runoff.
Special attention is paid to identifying differences in the distribution of runoff between the eastern and central-western parts of the sub-basin. It was found that in the eastern part of the sub-basin the share of the summer-autumn season is 46 %, and winter – only 15 %, which indicates the specific conditions for runoff formation in this region.
The results of the study are of important practical importance for water use planning, water resources management and prevention of natural disasters such as floods and droughts. They can also be used to develop strategies for adapting to climate change and ensuring sustainable development of the region.

Key words: Tisza sub-basin, annual and seasonal runoff, runoff variability, statistical characteristics.

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Goptsiy, M.V., Pozdnyakov, Yu.O. (2024). Assessment of Seasonal Runoff in the Tisza River Sub-Basin. Hidrolohiia, hidrokhimiia i hidroekolohiia [Hydrology, Hydrochemistry and Hydroecology], 4(74), 44-53 (in Ukrainian, abstr. in English). https://doi.org/10.17721/2306-5680.2024.4.4