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The results showed that the response of source contributions to SOM displayed difference significantly during different rainfall processes, showing fluctuation with flow.
Also, for a given rain gauge, different return periods are estimated for different rainfall durations and important differences can be found between the obtained values.
The reasons for the differences depend on the catchment characteristics and different rainfall inputs that were applied.
Different rainfall regimes vary between these extremes.
Different rainfall scenarios are considered to test its robustness.
Different rainfall simulation systems produce different erosivity relationships.
Eight cities in Brazil with different rainfall patterns were analysed.
Such different rainfall and temperature regimes engendered varied vegetation and soil forms (Aniya 1985).
Mpala is the only other patch with significantly different rainfall than Tiamamut.
Figure 3 Height of overland flow versus rainfall duration for different rainfall intensities.
Figure 5 shows the variability of the safety factor F s at different rainfall intensities.
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