Characteristics of maximum discharges on torrential watersheds in Serbia
Abstract
Torrential floods are the most frequent phenomenon in the arsenal of 'natural risks' in Serbia (droughts, avalanches, landslides, rockslides, hail, forest fires, storm wind and earthquakes). Regime of occurrence of floods was studied on the basis of investigations carried out on 128 control profiles, on all important river systems in Serbia, south from Sava and Danube. Frequency of event of maximum discharge Q(max), over determined threshold, defined as average maximum discharge Q(max av),was analysed. The primary maximum of frequencies was noticed in the period May-June, and the secondary maximum of frequencies in the period February-March. The absolute maximum discharges Q(max ab) on certain profiles follow the periods with the most expressed frequencies, but there are also significant exceptions. A few equations have been derived, which point out close relations between average maximum discharge Q(max av), magnitude of the catchment area A, average annual discharge Q(av) and the abs...olute maximum discharge Q(max ab) [Q(max av) = f(A); Q(max av) = f(Q(av)); Q(max av) = f(A, Q(av)); Q(max ab) =f(Q(max av))]. Historical cases of maximum discharges, reconstructed on the basis of 'hydraulics flood traces', are presented.
Keywords:
specific discharge of maximum ordinate of unit hydrograph / reconstructed discharge / mean maximum discharge / frequency / absolute maximum dischargeSource:
Journal of Environmental Protection and Ecology, 2011, 12, 2, 471-487Collections
Institution/Community
Šumarski fakultetTY - JOUR AU - Ristić, Ratko AU - Radić, Boris AU - Vasiljević, Nevena PY - 2011 UR - https://omorika.sfb.bg.ac.rs/handle/123456789/358 AB - Torrential floods are the most frequent phenomenon in the arsenal of 'natural risks' in Serbia (droughts, avalanches, landslides, rockslides, hail, forest fires, storm wind and earthquakes). Regime of occurrence of floods was studied on the basis of investigations carried out on 128 control profiles, on all important river systems in Serbia, south from Sava and Danube. Frequency of event of maximum discharge Q(max), over determined threshold, defined as average maximum discharge Q(max av),was analysed. The primary maximum of frequencies was noticed in the period May-June, and the secondary maximum of frequencies in the period February-March. The absolute maximum discharges Q(max ab) on certain profiles follow the periods with the most expressed frequencies, but there are also significant exceptions. A few equations have been derived, which point out close relations between average maximum discharge Q(max av), magnitude of the catchment area A, average annual discharge Q(av) and the absolute maximum discharge Q(max ab) [Q(max av) = f(A); Q(max av) = f(Q(av)); Q(max av) = f(A, Q(av)); Q(max ab) =f(Q(max av))]. Historical cases of maximum discharges, reconstructed on the basis of 'hydraulics flood traces', are presented. T2 - Journal of Environmental Protection and Ecology T1 - Characteristics of maximum discharges on torrential watersheds in Serbia EP - 487 IS - 2 SP - 471 VL - 12 UR - conv_2184 ER -
@article{ author = "Ristić, Ratko and Radić, Boris and Vasiljević, Nevena", year = "2011", abstract = "Torrential floods are the most frequent phenomenon in the arsenal of 'natural risks' in Serbia (droughts, avalanches, landslides, rockslides, hail, forest fires, storm wind and earthquakes). Regime of occurrence of floods was studied on the basis of investigations carried out on 128 control profiles, on all important river systems in Serbia, south from Sava and Danube. Frequency of event of maximum discharge Q(max), over determined threshold, defined as average maximum discharge Q(max av),was analysed. The primary maximum of frequencies was noticed in the period May-June, and the secondary maximum of frequencies in the period February-March. The absolute maximum discharges Q(max ab) on certain profiles follow the periods with the most expressed frequencies, but there are also significant exceptions. A few equations have been derived, which point out close relations between average maximum discharge Q(max av), magnitude of the catchment area A, average annual discharge Q(av) and the absolute maximum discharge Q(max ab) [Q(max av) = f(A); Q(max av) = f(Q(av)); Q(max av) = f(A, Q(av)); Q(max ab) =f(Q(max av))]. Historical cases of maximum discharges, reconstructed on the basis of 'hydraulics flood traces', are presented.", journal = "Journal of Environmental Protection and Ecology", title = "Characteristics of maximum discharges on torrential watersheds in Serbia", pages = "487-471", number = "2", volume = "12", url = "conv_2184" }
Ristić, R., Radić, B.,& Vasiljević, N.. (2011). Characteristics of maximum discharges on torrential watersheds in Serbia. in Journal of Environmental Protection and Ecology, 12(2), 471-487. conv_2184
Ristić R, Radić B, Vasiljević N. Characteristics of maximum discharges on torrential watersheds in Serbia. in Journal of Environmental Protection and Ecology. 2011;12(2):471-487. conv_2184 .
Ristić, Ratko, Radić, Boris, Vasiljević, Nevena, "Characteristics of maximum discharges on torrential watersheds in Serbia" in Journal of Environmental Protection and Ecology, 12, no. 2 (2011):471-487, conv_2184 .
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