Rodriguez & Sons Pty Ltd v Queensland Bulk Water Supply Authority trading as Seqwater
[2019] NSWSC 1657
At a glance
Source factsCourt
Supreme Court of NSW
Decision date
2017-12-15
Before
Beech-Jones J
Source
Original judgment source is linked above.
Judgment (16 paragraphs)
Background
- Like the situation at present, from 2001 to 2008 severe drought was experienced in eastern Australia, including South East Queensland. By 2009 the drought had broken. Towards the end of calendar year 2010 significant rainfall was expected and fell in South East Queensland as the effect of a "La Niña" climate phase took hold. The rainfall caused the declaration of a number of so-called "flood events" and the conduct of flood operations at Wivenhoe Dam and Somerset Dam in the last three months of 2010.
- By early January 2011, the catchment area of the Brisbane River [3] was saturated. Despite significant flood releases having been made during December 2010, as at early January 2011, each dam was above its so-called "Full Supply Level" ("FSL"). [4]
- Although the period from 2 January 2011 was referred to as the "January 2011 Flood Event", releases for flood mitigation from Wivenhoe Dam and Somerset Dam ceased on that day. They would not resume again until the afternoon of 7 January 2011. From 3 January 2011, various weather forecasts began to predict significant rainfall over the Brisbane River basin, including the catchments above the dams. These forecasts steadily increased and became ominous over the following days. Significant amounts of rain fell in the Brisbane River basin, including in the catchments above the dams, on 5 January 2011. It continued for the next two days, although it eased on Saturday 8 January 2011.
- On Sunday 9 January 2011, the heavens opened. Over that day and the following two days rainfall totals approximating 350mm to 400mm in depth were experienced in the catchment areas above the dams. [5] The rainfall on 11 January 2011 in the area of Wivenhoe Dam was of biblical proportions. [6] Extreme rainfall was also experienced during this period in the catchments downstream of the dams, especially in the Lockyer Valley which caused a significant increase in the flow of water in Lockyer Creek. Lockyer Creek flows into the Brisbane River just downstream of Wivenhoe Dam. [7] Extreme rain also fell in the catchment area for the Bremer River. The Bremer River flows through Ipswich and into the Brisbane River at a point 16 hours flow time downstream of Wivenhoe Dam and just above Moggill, a suburb of Brisbane. [8] The central business district of Brisbane is a further 10 hours flow time downstream of Moggill. [9]