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	Evaluation of Changes in Water Regime Caused by Long-term Development of Vegetation Cover Chlumecký, M. ; Tesař, Miroslav ; Buchtele, Josef Long monitoring of air temperature and precipitation for three catchments with up to 100 years series has been used as the input for the modelling of rainfall-runoff process and for the re-assessments of the evapotranspiration demand (ET.sub.demand./sub.). The resulting oscillations and the random changes of vegetation cover have been pursued as the indication of fluctuations also in the evapotranspiration. The intention is to appraise this complicated time series as the long-term process. The modified implementation of the conceptual model SAC-SMA enables the quicker simulation and facilitates also the conditions for automatic calibration of parameters in the used model; separately for individual, i.e. partial time intervals, namely with the diverse expected evapotranspiration. That process is to be identified simultaneously with the optimal parameters of the mode; the resulting actual evapotranspiration (ET.sub.act./sub.) is then represented as the modelling outputs, as such values could be hardly gained as measured or computed values, e. g. from other meteo-observations. Detailed record
	Using of the soil arametrisation based on soil samples database in rainfall-runoff modelling Němečková, Soňa ; Košková, Romana ; Hesse, C. The soil data processing and the simulations of the hydrological cycle in the Malse river basin using a distributed hydrological model SWIM are described. The Malse basin is situated in the southern Bohemia and it is a part of the Elbe river basin. Two sets of soil parameters were derived, the first one according to the soil samples (of the soil types) in the Malse watershed and the second according to samples from the whole Elbe river basin. The runoff simulations were completed based on both sets of parameters as the sensitivity test of the SWIM model to the soil data. Detailed record
	The effect of geology on extreme flows Jelínková, Hana Evaluation of the effect of geology on extreme flows. Comparison of sedimentary basin and crystalinic massif. Detailed record

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