Abstract:Hydrological variables of a catchment and their corresponding extreme
characteristics have a possibility of switching regimes, particularly
when a catchment undergoes protracted dry periods. This can result in a
catchment experiencing a flow anomaly that is even more extreme than
what was historically considered an extreme low flow event for the
catchment. Catchments in southeast Australia have been shown to exhibit
multiple states of mean annual flows. Given this and studies that
suggest that extreme events m… Show more
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