Study of the Flood Frequency Based on Normal Transformation in Arid Inland Region: A Case Study of Manas River in North-Western China

Figure 3

Results of correcting the mutation of flood serry. (a) The correction result of the annual maximum flood peak discharge mutation, (b) the correction result of the maximum 1 d flood volume mutation, (c) the correction result of the maximum 3 d flood volume mutation, and (d) the correction result of the maximum 5 d flood volume mutation.

(a)

(b)

(c)

(d)