“…On the north-eastern part of the Tisza river basin, the Carpathian Mountains form the curve, which changes the south-east direction in the area of the greatest altitude for the south direction towards Romania. Due to such a location of the mountain ranges, favourable conditions for the intensification of atmospheric precipitation are created here more frequently than in other areas (Lukianets et al, 2015;Susidko et al, 2010). The areas of the permanent orographic maxima and minima of precipitation are typical for the Ukrainian Carpathians.…”