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  • of the temperate and sub-polar latitudinal climate conditions. The data from more than 1800 catchments show that the contribution of few events represents a high proportion of the total basin suspended sediment load. The analysis suggests that the relative
  • been employed with the best available data sets on K-, C-, R- and LS-factors. Model results show that soil losses in Hesse vary between 0.5 and 15 tonnes/(ha.year). The mean loss amounts and the sediment delivery ratios for sub-catchments are also