Flooding update
The peak of the floods in the Gwydir Valley have passed through the township of Moree and are heading west. Many describe this event as
being two floods, the one caused initially from local rainfall of between 100-200mm and then the flood from upstream water sources like the
Horton River into the Gwydir and Mehi systems, that came at least three-days later.
Local rainfall and unregulated water is therefore, now being backed up by the major floodwaters from upstream, which is likely to result in
sustained, major flooding in the lower sections of the Gwydir floodplain.
All the rivers and creeks in the lower floodplain are flowing above capacity as water spills out. There is 100% supplementary access
available. During this time, Copeton Dam has increased from 22% to 39% capacity during this event, with a resource allocation likely
in early April in response.
There is a history of flooding in the Gwydir Valley and the peak height of the flood in Moree and surrounding gauges is provided on our
page 'History of Flooding' and compared with previous large and major floods.