ABSTRACT
A methodology for the treatment of uncertainty using temporal disaggregation is presented in Chapter 4 (Section 4. 1 ) . This chapter presents the application of the methodology to the flood forecasting model of the Klodzko catchment in Poland. The Klodzko catchment is located on the river Nysa Klodzka. The river serves as a highland tributary of the upper Odra River. The Klodzko catchment is a small mountain basin with a very short lag time between rainfall and runoff (see
Kundzewicz at ai . , 1 999 and Szamalek, 2000). The river Nysa Klodzka and its tributaries are shown in Figure 5 . 1 .
