ANWENDUNG VON IRRFAHRTPROBLEMEN IN DER BESCHREIBUNG DER HYDROLOGISCHEN VORGÄNGE

Abstract

The connection of the storage and continuation equations, the average delay time and the outflow probability of the water particle are described on the basis of the random walk of water particies. Its comparison to the linear reservoir model. The second part contains lhe different cases of the linear cascade models: dis- crete and continuous, homogenous cascade (Nash) model, superposition oflinear cascades (Dooge model), discrete cascades with feedback, continuous generalized linear cascades, discrete diffuse wave model and its comparison to the cascades having feedback. Finally the time and space discretising conditions coming from the theory of the random walk are demonstrated, which are identical to the criterium of stability of a discretising scherne.