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Pollack Periodica
Authors:
Andrej Šoltész
,
Dana Baroková
,
Zinaw Dingetu Shenga
, and
Michaela Červeňanská

in the Little Danube (h20, h35, h50 and h69) corresponds to the scenarios for flow rate Q = 20, 35, 50 and 69 m 3 •s -1 (see Table I ) and then the scenarios h VH (water level at the beginning of the flood wave) and h MAX (culminated water

Open access