21-50 years
A weather bomb caused flooding in Marlborough.
A weather "bomb” developed from a wave near Lord Howe Island. Development occurred in equatorwards entrance to a 150 kt jet, and in an area of strong vorticity advection. There was deepening of the low from 998 hPa to 968 hPa in an 18-hour period - almost two bergerons. Deepening rates of this magnitude are rarely seen in New Zealand area. A period of very strong northwest winds affected northern South Island ahead of the front, with wind strength supplemented by the rapid movement of the low, and by outflow from thunderstorms accompanying the front.
Weather situation that produced high rainfall was very similar to that of the flood of 1954 which was also a major event for the Cobb Reservoir.
There was minor damage.
Cobb Dam recorded 121 mm (12.1 cm) of rain in 17 hours.
The heavy rain produced the largest ever peak flow into Cobb reservoir.
Uruwhenua recorded 198 mm (19.8 cm) of rain in 24 hours.
The heavy rain was associated with a depression which developed in the North Tasman Sea and moved southeastwards towards Fiordland. The significant contributing factor to the large rainfalls was the strong northwesterly surface wind.
Heavy rain began at 8:30am on the 1st of April and a 15 hour period of heavy rain followed.
Onamalutu recorded 157 mm (15.7 cm) of rain in 24 hours (which has a return period of 25 years).
The Branch recorded 127 mm (12.7 cm) of rain in 24 hours (which was a return period of 20 years).
153 mm The Wye recorded 153 mm (15.3 cm) of rain.
Waihopai recorded 75 mm (7.5 cm) of rain in 24 hours.
The flow of Wairau River was similar to that of the flood of 1954.
The flow was the greatest since at least the flood of 1936.
Flood control prevented damage from the flood.
The flood had an estimated return period of 50 years.
21-50 years
A weather bomb caused flooding in Marlborough.
A weather "bomb” developed from a wave near Lord Howe Island. Development occurred in equatorwards entrance to a 150 kt jet, and in an area of strong vorticity advection. There was deepening of the low from 998 hPa to 968 hPa in an 18-hour period - almost two bergerons. Deepening rates of this magnitude are rarely seen in New Zealand area. A period of very strong northwest winds affected northern South Island ahead of the front, with wind strength supplemented by the rapid movement of the low, and by outflow from thunderstorms accompanying the front.
Weather situation that produced high rainfall was very similar to that of the flood of 1954 which was also a major event for the Cobb Reservoir.
There was minor damage.
Cobb Dam recorded 121 mm (12.1 cm) of rain in 17 hours.
The heavy rain produced the largest ever peak flow into Cobb reservoir.
Uruwhenua recorded 198 mm (19.8 cm) of rain in 24 hours.
The heavy rain was associated with a depression which developed in the North Tasman Sea and moved southeastwards towards Fiordland. The significant contributing factor to the large rainfalls was the strong northwesterly surface wind.
Heavy rain began at 8:30am on the 1st of April and a 15 hour period of heavy rain followed.
Onamalutu recorded 157 mm (15.7 cm) of rain in 24 hours (which has a return period of 25 years).
The Branch recorded 127 mm (12.7 cm) of rain in 24 hours (which was a return period of 20 years).
153 mm The Wye recorded 153 mm (15.3 cm) of rain.
Waihopai recorded 75 mm (7.5 cm) of rain in 24 hours.
The flow of Wairau River was similar to that of the flood of 1954.
The flow was the greatest since at least the flood of 1936.
Flood control prevented damage from the flood.
The flood had an estimated return period of 50 years.