NZ Historic Weather Events Catalogue

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May 1923 Otago Flooding ( 1923-05-13 )

Abnormally heavy rainfall over Dunedin and Taieri Plains over two days resulted in flooding.

Otago

Heavy RainHeavy Rain at Otago
Comments:

ImpactAbnormally heavy rainfall resulted in serious floods in Dunedin and Taieri Plains.

Physical CharacteristicThe rainfall had an average intensity of 0.5 in (1.27cm) per hour.

Heavy RainHeavy Rain at Middlemarch
Map Location: -45.508281 170.125395
Comments:

Physical CharacteristicMiddlemarch recorded 1.19 in (3.0cm) of rain in 24 hours.

Heavy RainHeavy Rain at Musselburgh
Map Location: -45.89644 170.51357
Comments:

Physical CharacteristicMusselburgh recorded 0.7 in (1.8cm) of rain in 24 hours ending at 8am on the 13th.

Physical CharacteristicMusselburgh recorded 1.32 in (3.4cm) of rain in 24 hours ending at 8am on the 14th.

Heavy RainHeavy Rain at Whare Flat
Map Location: -45.81165 170.43029
Comments:

Physical CharacteristicWhare Flat recorded 1.95 in (5.0cm) of rain in 24 hours ending at 8am on the 13th.

Physical CharacteristicWhare Flat recorded 2.9 in (7.4cm) of rain in 24 hours ending at 8am on the 14th.

Heavy RainHeavy Rain at Sullivans Dam
Map Location: -45.80616 170.52222
Comments:

Physical CharacteristicSullivan's Dam recorded 1.25 in (3.2cm) of rain in 24 hours ending at 8am on the 13th.

Physical CharacteristicSullivan's Dam recorded 3.19 in (8.1cm) of rain in 24 hours ending at 8am on the 14th.

Heavy RainHeavy Rain at Dunedin
Map Location: -45.87911 170.502707
Comments:

CommentRain fell on the 13th for five and a half hours and on the 8th for eight hours.

FloodingFlooding
Comments:

DamageThe Leith was in high flood and caused serious damage to the paper mills at Woodhaugh.

ImpactThe botanical gardens were inundated to a considerable depth.

ImpactThe April flood brought down large quantities of boulders and shingle which lodged in channels. The restricted waterways caused overflow and serious flooding.

Physical CharacteristicHarbour Terrace had a peak discharge of 4000 cusecs (113 cumecs).

CommentLindsay's Creek was in high flood.

ImpactMany people in the lower parts of the North East Valley and along the Leith had their houses flooded.

Affected LifelineDamage to both road and rail communication was severe.

Damage CostFor the floods of April 1923 and May 1923: the estimated cost for repairing culverts, bridges, walls, slips, washouts, scoured metal, and removing household debris totalled £20,000 ($1,736,000 2008 dollars). This included £7,670 ($665,900 2008 dollars) for cleaning out and clearing the bed and straightening the course as far as possible of the Water of Leith, and £1,385 ($120,200 2008 dollars) for similar work in Lindsay's Creek. The Drainage Board had an expenditure of £6,045 ($524,800 2008 dollars) in the Leith and £5,565 ($483,200 2008 dollars) in Lindsay's Creek.

Damage CostFor the floods of April 1923 and May 1923: The total cost of clearing and reconstruction work of the Leith and Lindsays Creek up to 31st March 1924 was £33,628 ($2,919,600 2008 dollars).

ImpactFor the floods of April 1923 and May 1923: The total quantity of material removed from the bed of the Leith was 43,000 cubic yards (33,000 cubic metres).

Affected LifelineFor the floods of April 1923 and May 1923: Bridges on the Leith Valley Road at Nicholl's Creek and Henderson's were demolished.

Affected LifelineFor the floods of April 1923 and May 1923: The foundations of the eastern pier of the bridge over the Leith at Harbour's was badly scoured.

LandslideLandslide
Comments:

Affected LifelineNorth of Dunedin extensive slips blocked the railway.

FloodingFlooding at Taieri Plain
Map Location: -45.88401 170.253762
Comments:

Physical CharacteristicTaieri Plains were extensively flooded. Tairei River broke out through breaches in the stop banks and peaked at 59,000 cusecs (1671 cumecs) at Outram Gorge.

Peak River LevelTaieri River had a peak level of 18 ft 8 in (5.7m) and a large area to the west of Tairei was inundated.

FloodingFlooding at Allanton
Map Location: -45.918208 170.25344
Comments:

Peak River LevelAt Allanton, Taieri River had a peak level of 15 ft 6 in (4.7m).

FloodingFlooding at Otokia
Map Location: -45.949801 170.189367
Comments:

Peak River LevelAt Otokia, Taieri River rose 9 ft (2.7m) and the highest peak river level was at West Tairei Bridge at 19 ft 8 in (6.0m).

FloodingFlooding at Waipori River
Map Location: -45.92281 170.0046
Comments:

Physical CharacteristicWaipori River rose 10 ft 6 in (3.2m) above normal at the Weir.

FloodingFlooding at Waitahuna
Map Location: -45.986063 169.747236
Comments:

ImpactFlooding occurred in the Waitahuna township.

References

Cowie, C.A; Attwood, A.K.(1957) FLOODS in NEW ZEALAND 1920 -53, The Soil Conservation and Rivers Control Council, Wellington, New Zealand,239p.
MacLean, M., McGregor Wilke, J., and Alexander, J.G. (n.d.) Water of Leith and Lindsay's Creek, Dunedin.
Municipality of Dunedin. City of Dunedin (New Zealand), Departmental Reports For the Year 1922-1923.
Municipality of Dunedin. City of Dunedin (New Zealand), Departmental Reports For the Year 1923-1924.

May 1923 Otago Flooding ( 1923-05-13 )

Abnormally heavy rainfall over Dunedin and Taieri Plains over two days resulted in flooding.

Otago

Heavy RainHeavy Rain at Otago
Comments:

ImpactAbnormally heavy rainfall resulted in serious floods in Dunedin and Taieri Plains.

Physical CharacteristicThe rainfall had an average intensity of 0.5 in (1.27cm) per hour.

Heavy RainHeavy Rain at Middlemarch
Map Location: -45.508281 170.125395
Comments:

Physical CharacteristicMiddlemarch recorded 1.19 in (3.0cm) of rain in 24 hours.

Heavy RainHeavy Rain at Musselburgh
Map Location: -45.89644 170.51357
Comments:

Physical CharacteristicMusselburgh recorded 0.7 in (1.8cm) of rain in 24 hours ending at 8am on the 13th.

Physical CharacteristicMusselburgh recorded 1.32 in (3.4cm) of rain in 24 hours ending at 8am on the 14th.

Heavy RainHeavy Rain at Whare Flat
Map Location: -45.81165 170.43029
Comments:

Physical CharacteristicWhare Flat recorded 1.95 in (5.0cm) of rain in 24 hours ending at 8am on the 13th.

Physical CharacteristicWhare Flat recorded 2.9 in (7.4cm) of rain in 24 hours ending at 8am on the 14th.

Heavy RainHeavy Rain at Sullivans Dam
Map Location: -45.80616 170.52222
Comments:

Physical CharacteristicSullivan's Dam recorded 1.25 in (3.2cm) of rain in 24 hours ending at 8am on the 13th.

Physical CharacteristicSullivan's Dam recorded 3.19 in (8.1cm) of rain in 24 hours ending at 8am on the 14th.

Heavy RainHeavy Rain at Dunedin
Map Location: -45.87911 170.502707
Comments:

CommentRain fell on the 13th for five and a half hours and on the 8th for eight hours.

FloodingFlooding
Comments:

DamageThe Leith was in high flood and caused serious damage to the paper mills at Woodhaugh.

ImpactThe botanical gardens were inundated to a considerable depth.

ImpactThe April flood brought down large quantities of boulders and shingle which lodged in channels. The restricted waterways caused overflow and serious flooding.

Physical CharacteristicHarbour Terrace had a peak discharge of 4000 cusecs (113 cumecs).

CommentLindsay's Creek was in high flood.

ImpactMany people in the lower parts of the North East Valley and along the Leith had their houses flooded.

Affected LifelineDamage to both road and rail communication was severe.

Damage CostFor the floods of April 1923 and May 1923: the estimated cost for repairing culverts, bridges, walls, slips, washouts, scoured metal, and removing household debris totalled £20,000 ($1,736,000 2008 dollars). This included £7,670 ($665,900 2008 dollars) for cleaning out and clearing the bed and straightening the course as far as possible of the Water of Leith, and £1,385 ($120,200 2008 dollars) for similar work in Lindsay's Creek. The Drainage Board had an expenditure of £6,045 ($524,800 2008 dollars) in the Leith and £5,565 ($483,200 2008 dollars) in Lindsay's Creek.

Damage CostFor the floods of April 1923 and May 1923: The total cost of clearing and reconstruction work of the Leith and Lindsays Creek up to 31st March 1924 was £33,628 ($2,919,600 2008 dollars).

ImpactFor the floods of April 1923 and May 1923: The total quantity of material removed from the bed of the Leith was 43,000 cubic yards (33,000 cubic metres).

Affected LifelineFor the floods of April 1923 and May 1923: Bridges on the Leith Valley Road at Nicholl's Creek and Henderson's were demolished.

Affected LifelineFor the floods of April 1923 and May 1923: The foundations of the eastern pier of the bridge over the Leith at Harbour's was badly scoured.

LandslideLandslide
Comments:

Affected LifelineNorth of Dunedin extensive slips blocked the railway.

FloodingFlooding at Taieri Plain
Map Location: -45.88401 170.253762
Comments:

Physical CharacteristicTaieri Plains were extensively flooded. Tairei River broke out through breaches in the stop banks and peaked at 59,000 cusecs (1671 cumecs) at Outram Gorge.

Peak River LevelTaieri River had a peak level of 18 ft 8 in (5.7m) and a large area to the west of Tairei was inundated.

FloodingFlooding at Allanton
Map Location: -45.918208 170.25344
Comments:

Peak River LevelAt Allanton, Taieri River had a peak level of 15 ft 6 in (4.7m).

FloodingFlooding at Otokia
Map Location: -45.949801 170.189367
Comments:

Peak River LevelAt Otokia, Taieri River rose 9 ft (2.7m) and the highest peak river level was at West Tairei Bridge at 19 ft 8 in (6.0m).

FloodingFlooding at Waipori River
Map Location: -45.92281 170.0046
Comments:

Physical CharacteristicWaipori River rose 10 ft 6 in (3.2m) above normal at the Weir.

FloodingFlooding at Waitahuna
Map Location: -45.986063 169.747236
Comments:

ImpactFlooding occurred in the Waitahuna township.

References

Cowie, C.A; Attwood, A.K.(1957) FLOODS in NEW ZEALAND 1920 -53, The Soil Conservation and Rivers Control Council, Wellington, New Zealand,239p.
MacLean, M., McGregor Wilke, J., and Alexander, J.G. (n.d.) Water of Leith and Lindsay's Creek, Dunedin.
Municipality of Dunedin. City of Dunedin (New Zealand), Departmental Reports For the Year 1922-1923.
Municipality of Dunedin. City of Dunedin (New Zealand), Departmental Reports For the Year 1923-1924.