To ascertain the trends of the sediments runoff changes in the Upper Dnister River basin systems the data sets for 23 gauging stations for two periods have been analyzed. The first period is 1958 – 1990 and the second one – 1991 – 2019. The second period is taken as the conditional start of the intensive climatic changes. The investigation is also based on the own semi-stationary observations which were carried out during the 2004 – 2014. The analysis has testified that denudation intensity is considerably different in time and space aspects. The Carpathian basin systems are characterized by the high sediments runoff in the period 1958 – 1990. During the next period 1991 – 2019 the trend of decreasing of the sediments runoff is observed in all the basin systems of the Upper Dnister.
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