Extreme weather - winds and tornadoes

Due to its position in the 'Roaring Forties', a belt of strong winds in the Southern Hemisphere which generally occur between the latitudes of 40 and 49 degrees, as well as its small size, New Zealand is a windy country.

Extreme winds – There is no widely accepted definition for 'extreme wind'. In New Zealand, in the context of building design, an extreme wind is a wind gust which is strong enough to be dangerous for people, or cause significant damage to buildings and property. Winds this strong are expected to happen every 500 years or so. Wind events with return periods of more than 2 years usually cause some problems and might be regarded as extreme in contexts such as transmission line damage.

Find out more about return periods

Tornadoes – A tornado is a large rotating column of air (or vortex) that occurs in association with a thunderstorm. It has winds that travel at very high speeds around a central area of very low atmospheric pressure. The parent thunderstorms typically have very strong updrafts with speeds of 36 km/h and which are developed in a wind-shear environment which causes the updraft to rotate, in turn potentially causing a tornado.

Very strong updraft speeds of over 150km/hr or more have been reported in the United States, but not here in New Zealand. 

Causes of extreme winds and tornadoes

Extreme wind gusts are the result of intense turbulence within vigorous storms systems such as ex-tropical cyclones or mid-latitude storms. These systems contain bands of generally strong winds associated with areas of large pressure gradients and these are usually near the centre of low-pressure. Organised convection, wind-shear, and steep terrain within these bands can all generate the turbulence that gives rise to the extreme wind gusts. Extreme winds can on occasion also be caused by tornadoes and convective downbursts from isolated thunderstorms not associated with a large storm systems.

Potential consequences of extreme winds and tornadoes

Extreme winds and tornadoes can cause deaths and property damage, with the damage being highly unpredictable.

Typical damage experienced in New Zealand includes:

  • destruction of buildings, including roofing being blown off, broken windows, and other flying debris
  • large scale forest damage and fallen trees or branches falling onto power-lines
  • high-sided vehicles and outdoor equipment such as centre-pivot irrigators being blown over
  • very tall buildings, suspension bridges and transmission lines can suffer structural failures.

Worst case examples of extreme winds and tornadoes around New Zealand

Some of the worst storms in living memory are:

  • Ex-tropical cyclone Bola, in March 1988, when very heavy rains and hurricane-force winds struck the east coast of the North Island causing extensive severe damage and flooding
  • The Wahine storm (ex-cyclone Gisele), in April 1968, when an ex-tropical cyclone hit the Wellington region. Fifty three people lost their lives when the Wahine ferry sank in Wellington Harbour.

Some of the worst recent tornadoes have been:

  • in Dec 2012, a tornado in Auckland killed three people, injured seven others and was responsible for an estimated $13 million in cleanup costs, and $6.5 million in insurance claims
  • in May 2011, a tornado in Auckland, killed one person, injured several others, as well as causing several million dollars' worth of damage
  • in August 2004, a tornado near Waitara, Taranaki destroyed a farmhouse and killed two people: in July 2007, several tornados on the same evening caused damage to homes and other property worth seven million dollars in Oakura and New Plymouth.

Extreme winds and tornado research at NIWA

NIWA carries out a variety of research projects measuring and computer modelling of winds in co-operation with GNS, BRANZ, OPUS and the University of Auckland. In addition, NIWA is building a searchable database of storms and hazards, including tornadoes and strong winds, in New Zealand.

Current NIWA research projects

Winds

  • Topographic multipliers. NIWA is currently undertaking the second phase of a field campaign measuring the speed up of winds over the complex terrain of the Belmont Hills near Wellington. The experiment also involves high resolution numerical modelling of the observed flows with the GERRIS CFD (computational Fluid Dynamics model) and also comparing these with results obtained by the OPUS wind tunnel.
  • RiskScape. Extreme wind fields experienced in strong wind storms over various towns and cities within New Zealand are being estimated/mapped with high resolution numerical models. These wind fields are overlaid with building databases within the RiskScape model and likely damage and probable losses can then be estimated.
  • Participation in the GeoScience Australia damage survey following Tropical Cyclone Yasi in North Queensland. Also, in association with the Samoan Ministry of Natural Resources and Environment, we conducted a damage survey in Samoa following Tropical Cyclone Evan. 
  • Strong winds also cause damaging storm surge and hazardous wave conditions, so the research into strong winds also assists other NIWA projects that study ocean and coastal hazards.

More information about RiskScape 

Read our media release 'Preparing New Zealand for storms: lessons from Yasi'

Tornadoes

  • Modelling and forecasting of Taranaki tornadoes (Natural Hazards Update 2009) and the Albany and Hobsonville tornadoes, using the NZLAM and NZ Convective Scale numerical weather models.
  • Idealised very high-resolution simulations of a tornadic vortex with the GERRIS model
  • Damage survey's following tornadoes are occasionally done, e.g., Oakura and New Plymouth, 2007,Albany 2011, and Hobsonville 2012.
    Turner, R., M. Revell, S. Reese, S. Moore, and S. Reid, 2011: Some recent extreme wind events in New Zealand. Winds and Structures.

Contact

Dr Richard Turner
richard.turner@niwa.co.nz

Dr Mike Revell
mike.revell@niwa.co.nz
Tel 04 386 0328

Tornado in Oklahoma, USA

Tornado in Oklahoma, USA (Wikimedia Commons/NOAA)

wind - vertical motion field.jpg

700 hPa (3 km altitude) vertical motion field at 5:30 pm NZST July 5, 2007. Dark red areas indicate strong updrafts, dark blue areas indicate strong downdrafts.

tornadic thunderstorm schematic.jpg

Idealized schematic plan view of a tornadic thunderstorm at low levels. Dark red shaded area shows the position of the main thunderstorm updraft (UD) Light blue shaded areas show the Rear Flank Downdraft (RFD) and Forward Flank Downdraft (FFD). Light-green line shows the probable extent of a radar echo. Black arrows shows the storm-relative flow (i.e. wind vectors with the mean northwesterly storm-motion subtracted). Frontal symbols mark the boundary between the warm inflow and cold outflow - areas of rising motion along the frontal boundary are shaded light-red. The likely location of tornadoes is indicated by the circled Ts.