Major Outcomes

  • Small storms can have a high impact on receiving waters because they are more frequent and can still generate significant washoff concentrations.
  • The resulting averages are shown in Table 2.8 for the case of the 0.19 in. storm. The point being made here is that even though the pollutographs produced by the two models can look very different, with the proper choice of coefficients it is possible to get event average concentrations that look similar.