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Lismore Flooding - Introduction The Northern Rivers district of NSW, Australia is one of the most flood prone areas of the country outside of the tropics.
With Lismore at the junction of two major streams - Leycester Creek and Wilsons River - it is often subject to significant flooding.
Topography and the alignment of the Northern NSW coast relative to prevailing weather patterns allows for prolonged orographically enhanced rainfall events from time to time - particularly during late Summer, Autumn and early Winter.
During those months large slow-moving blocking high pressure systems are often positioned around 40 degrees south and provide a long fetch of moisture-laden southeast to easterly winds onto the North Coast.
It is not essential for a strong 'blocking' high pressure system to help cause a flood, but it is nearly always present for the major events - as it keeps the rain producing systems in the same area longer.
Some examples of flood producing weather patterns: Lismore aerial photo and location map from.
Click for larger view.
Richmond River Flood Plain casino nsw flood map Catchment Maps The Wilsons River, Leycester Creek and tributaries upstream from Lismore represent only about one-quarter of the Richmond River catchment, however the majority of flooding occurs in this area and through to Coraki.
The Nightcap Range to the north of Lismore, and hills extending through Bangalow to near Alstonville often receive much higher rainfall than the rest of the region due to orographic effects and because it is closer to the coast and the source of rain-bearing clouds.
The floodplain is also narrower due to hilly terrain.
South and west of Lismore the terrain is quite flat and the floodplain very casino nsw flood map in comparison.
Major flooding of the Richmond River upstream from Coraki requires heavy rainfall west of the Nightcap and Border Ranges and into the eastern parts of the Richmond Range.
This occurs far less frequently than Lismore flooding, with February 1954 and January 2008 the stand-out events for Casino, Kyogle and Wiangaree.
Heavy rainfall occurring over the generally flat country and eastern parts of the Richmond Range in the southwest of the catchment contributes to flooding at Coraki, Woodburn and downstream.
Heavy rainfall on the southern side of the Alstonville Plateau also affects the Lower Richmond River.
Another part of the catchment is the Teven Valley and North Creek northwest and north of Ballina.
Flooding can occur in this area during very heavy rainfall although those waters quickly enter the Richmond River.
Lismore Flood Heights The Lismore flood gauge is on the rowing club building at the western end of Magellan Street red dot on the and the figures below are all taken from that point.
Australian Height Datum AHD was introduced in the late 1990s.
AHD flood height measurements are 0.
Flood heights in other parts of Lismore vary depending on a number of factors including the volume and speed of water coming down the Wilsons River and Leycester Creeks, the amount of local flooding due to heavy rain in Lismore, whether the Browns Creek pump is operational and whether levees have or are being overtopped.
The Lismore central business district used to begin flooding when the Wilsons River reached 9.
Water would flow into the streets near the old Post Office at the corner of Molesworth and Magellan streets.
Major flows into the city would occur by 9.
A concrete wall flood levee was built over a couple of years and finished in March 2005.
It protects the CBD from floods up to about 10.
Flood waters during major events will still top the levee but will start to enter streets at the Browns Creek spillway on Molesworth Street between Woodlark and Zadoc streets.
A long established earthen levee protects South Lismore from all but major floods exceeding 10.
North Lismore has no flood protection and is the first area to be cut off.
The highest recorded Lismore flood levels were on 21st February 1954 and 11th March 1974.
Signs such as this one are displayed on power poles throughout casino nsw flood map city to mark the highest level floodwaters reached.
Daily rainfall data from all sites in the Northern Rivers have been added for each flood event.
Tropical cyclone tracking map links are listed where it is known they directly or indirectly contributed to a flood event.
Infrared satellite picture loops are available for all flood events since 1983.
Bureau of Meterology flood levels metres AHD for the Wilsons River at Lismore Major: 9.
Links to daily rainfall data are provided where available.
Floods were likely 11-12 Feb and also 16-18 Feb.
Rainfall figures suggest a moderate flood was likely.
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Browns Ck raging torrent over Spinks Bridge.
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South Lismore levee breached.
Cyclonic wind - Easterly then calm then Westerly.
Major flooding in Sydney and Hunter Valley.
Eye of tropical cyclone crossed Cape Byron - winds were calm for a short time.
Minor flooding in Lismore but moderate flooding on the Clarence River.
The casino nsw flood map of TC Ivor as an upper low, continued for two more weeks and caused the worst flooding ever for western NSW and Qld.
Moderate flooding in Lismore and Murwillumbah.
Heavy rain for only 24 hours.
Severe flooding at Nimbin with 300mm in one night caused some of the worst flooding ever there.
Rainfall figures reveal another rainfall event around 17th May but it was fairly coastal in extent.
Many locations received over 400mm of rain in 36 hours.
The entire catchment was saturated from days of rain, then further extreme rainfalls fell in the Tweed and Upper Richmond rivers during the evening of Friday 4th January.
Several intense meso-lows formed in the trough and brought very heavy rain and destructive winds - particularly to the Northern Rivers region on Thursday 21st.
Major river and flash flooding occurred between the Queensland Sunshine Coast and Port Macquarie between Wednesday 20th to Sunday 24th May.
casino grill Lismore, the new levee once again saved the main part of the central business district from inundation - but only just - another hour of heavy rainfall and it would have over-topped.
Flooding was major in the Wilsons, Richmond and Clarence rivers, with the Tweed and Brunswick Valley not as badly hit.
A strong high pressure was anchored in the Tasman Sea.
A mid level trough in the southern Coral Sea tracked westward and crossed the coast during the morning of the 11th.
This time the heaviest falls were in SE QLD however local rainfall was enough to push the Wilsons River in Lismore to minor flood levels.
Metres Date Synoptic situation and notes.
Links to daily rainfall data are provided where available.
These flood pictures were taken overlooking the Lismore basin then around the central business district.
The flood peak had dropped about 20cm by this time.
After the biggest flood since 1974 hit the region on 2nd April 1989, a second flood for the same calendar month occurred.
A few photos were taken near the Lismore rowing club and Browns Creek pump.
This CBD inundation proved to be the final straw to get the Lismore flood levee built.
The pictures on the 1st were taken near Eltham, and on the 2nd near Eltham and in the Lismore CBD.
The flood photos are taken of the Wilsons River at Eltham and along the Bangalow Road leading into Lismore.
Major flooding peaked at the low end of the major level.
It illustrated how well the levee worked in protecting the CBD from 90 per cent of floods that occur in the region.
The flood photographs are taken near Eltham and around Lismore.
The pictures are taken around Eltham and Lismore.
The river peak in Lismore was quite slow to arrive with floodwaters persisting from the 4th to the 6th.
The pictures are taken near Eltham and the Tweed Coast.
Lismore was lucky and only saw moderate flooding.
Most low lying areas along the Richmond River were inundated with some record stream rises.
The Lismore flood levee protected most of the central business district from inundation.