By I.J. Dwyer, D.W. Reed
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Additional resources for Allowance for Discretization in Hydrological and Environmental Risk Estimation
0 0 . 3 Melboume hourly rainfallrecordB 44 *8 5 6.
The analysis of several daily rainfall records suggested that the growth rate, as measured by parameter b, is generally lower than for hourly records but still rather variable. 323 Cape Town . 353 Durban . 106 Johannesburg . 292 Richmond . 303 Upington . 357 Brisbane Hobart Melbourne Perth Sydney In contrast, the variograms for rainfall do change systematically with time scale: as the resolution becomes finer, a better appreciation of the fractal behaviour is obtained. 1 Catchmnent average rainfall The calculation of catchment rainfall necessarily has a smoothing effect: catchment rainfall events tend to start and stop less abruptly and have more uniform profiles than point rainfall events.
058 Appendix D: L-moment ratio diagrams for R(D) Graphs showing I-CV and L-skew for fixed maxima (solid lines) and sliding maxima (dotted lines) for various data records. 0 0 . 3 Melboume hourly rainfallrecordB 44 *8 5 6.
Allowance for Discretization in Hydrological and Environmental Risk Estimation by I.J. Dwyer, D.W. Reed