The
salinity in the lake increases as the salt crust dissolves over a period of six months of a major flood, resulting in a massive
fish kill. When over deep, the lake is no saltier than the
sea, but salinity increases as the water evaporates, with
saturation occurring at about a depth. The lake takes on a pink hue when saturated, due to the presence of
beta-carotene pigment caused by the
alga Dunaliella salina.
Flooding proposals Since 1883, proposals have been made to flood Lake Eyre with seawater brought to the basin via a canal or pipeline (such as the
Bradfield Scheme). The purpose was, in part, to increase evaporation and thereby increase rainfall in the region downwind of an enlarged Lake Eyre. The added rainfall has been modelled as small. Due to the basin's low elevation below sea level and the region's high annual evaporation rate (between ), such schemes have generally been considered impractical, as it is likely that accumulation of salt deposits would rapidly block the engineered channel. At a rate of evaporation per day, a viaduct flowing a would supply enough water to create a sea. If brine water were not sent back to the ocean, it would precipitate of salt every year.
Natural floods Typically a flood occurs every three years, a flood every decade, and a fill or near fill a few times a century. The water in the lake soon evaporates, with a minor or medium flood drying by the end of the following summer. Most of the water entering the lakes arrives via
Warburton River. and 1999–2001, with the highest flood of in 1974.
1974 In 1974, the largest recorded historical lake filling in nearly 200 years occurred.
2009 to 2011 The 2009 Lake Eyre flood peaked at deep in late May, which is a quarter of its maximum recorded depth of . of water crossed the Queensland–South Australian border with most of it coming from massive floods in the
Georgina River. However, owing to the very low rainfall in the lower reaches of these rivers (contrasting with heavy rainfall in the upper catchments), the greater proportion soaked into the desert or evaporated en route to the lake, leaving less than in the lake, which covered an area of , or 12% of the total. As the flood did not start filling the lake's deepest point (Belt Bay) until late March, little bird life appeared, preferring instead to nest in the upper reaches of the Lake Eyre Basin, north of
Birdsville, where large lakes appeared in January as a result of monsoonal rain. The high rainfall in summer 2010 sent flood water into the
Diamantina,
Georgina, and
Cooper Creek catchments of the Lake Eyre basin, with the Cooper Creek reaching the lake for the first time since 1990. The higher rainfall prompted many different birds to migrate back to the area for breeding. Heavy local rain in early March 2011 in the Stuart Creek and Warriner catchments filled Lake Eyre South, with Lake Eyre North about 75 per cent covered with water firstly from the
Neales and
Macumba Rivers, and later from the
Warburton River.
2015 to 2016 In late 2015, water began flowing into Lake Eyre following heavy rain in the north-east of the state.
2019 ) of the lake, 2020 In late March 2019, floodwaters began arriving as a result of torrential rains in
northern Queensland in January. In the past, the water had taken anywhere from three to 10 months to reach the lake, but this time it arrived in two. The first flooding would be closely followed by another surge, following rains produced by
Cyclone Trevor.
Traditional owners and graziers agree that it is essential that the river run its course and should not be harvested during floods, as any interference in the natural systems could damage the
ecosystem.
2025 In April 2025 it was predicted that floodwaters from Queensland in late March, combined with local rainfall pre-filling parts of the lake, would result in the lake reaching its deepest levels in 15 years some time around late May to June. Upstream river levels have been higher than in previous flood events, with
Birdsville reaching on Wednesday 9 April (higher than the 8.15 m in 2019), and
Windorah recording flood levels approaching 1974's heights, that being Australia's wettest year on record. On 30 May 2025, the floodwaters were said to be the highest seen in
Channel Country, and making their way into Kati Thanda. However, South Australia has had severe drought since 2024, and locals think that the lake is unlikely to reach the peak reached in 1974. ==Flora and fauna==