Flow characteristics of rivers in northern Australia: Implications for development

• Published in: Journal of hydrology (Amsterdam) Vol. 357; no. 1; pp. 93 - 111
• Main Authors: Petheram, Cuan, McMahon, Thomas A, Peel, Murray C
• Format: Journal Article
• Language: English
• Published: Amsterdam Elsevier B.V 30.07.2008; [Amsterdam; New York]: Elsevier; Elsevier Science
• Subjects: annual stream flow; daily stream flow; drought; Earth sciences; Earth, ocean, space; Exact sciences and technology; hydrologic data; Hydrology; Hydrology. Hydrogeology; Irrigation; monthly stream flow; Northern Australia; rivers; runoff; stream flow; Streamflow; surface water; Tropical; water harvesting; Water resources; Water storage; watershed hydrology; watersheds; Australia; Queensland; Hydrology; Irrigation; Water storage; Tropical; Northern Australia; Streamflow; base flow; rivers; rainfall; Australasia; tropical zone; runoff; rain water; hydrodynamics; autocorrelation; surface water; irrigation; water resources; water storage; drought; discharge; water resource management; correlation coefficient; hydrographs; standard deviation; streamflow
• ISSN: 0022-1694; 1879-2707
• DOI: 10.1016/j.jhydrol.2008.05.008

Annual, monthly and daily streamflows from 99 unregulated rivers across northern Australia were analysed to assess the general surface water resources of the region and their implications for development. The potential for carry-over storages was assessed using the Gould-Dincer Gamma method, which utilises the mean, standard deviation, skewness and lag-one serial correlation coefficient of annual flows. Runs Analysis was used to describe the characteristics of drought in northern Australia and the potential for ‘active’ water harvesting was evaluated by Base Flow Separation, Flow Duration Curves and Spells Analysis. These parameters for northern Australia were compared with data from southern Australia and data for similar Köppen class from around the world. Notably, the variability and seasonality of annual streamflow across northern Australia were observed to be high compared with that of similar Köppen classes from the rest of the world (RoW). The high inter-annual variability of runoff means that carry-over storages in northern Australia will need to be considerably larger than for rivers from the RoW (assuming similar mean annual runoff, yield and reliability). For example, in the three major Köppen zones across the North, it was possible (theoretically) to only exploit approximately 33% (Köppen Aw; n = 6), 25% (Köppen BSh; n = 12) and 13% (Köppen BWh; n = 11) of mean annual streamflow (assuming a hypothetical storage size equal to the mean annual flow). Over 90% of north Australian rivers had a Base Flow Index of less than 0.4, 72% had negative annual lag-one autocorrelation values and in half the rivers sampled greater than 80% of the total flow occurred during the 3-month peak period. These data confirm that flow in the rivers of northern Australia is largely event driven and that the north Australian environment has limited natural storage capacity. Hence, there is relatively little opportunity in many northern rivers to actively harvest water for on-farm storage, particularly under environmental flow rules that stipulate that water can only be extracted during the falling limb of a hydrograph. Streamflow drought severity, the product of drought length and magnitude, was found to be greater in northern Australia than in similar climatic regions of the RoW, due to higher inter-annual variability increasing the drought magnitude over the course of normal drought lengths. The high likelihood of severe drought means that agriculturalists seeking to irrigate from rivers in northern Australia should have especially well developed drought contingency plans.