Story: Wellington region

Page 3 – Climate

Windy Wellington

New Zealand lies in the path of the roaring forties – the prevailing westerly winds. The central ranges deflect these winds through Cook Strait, the narrow gap between the North and South islands. Funnelled through this passage, they become faster and stronger. Wellington is in the teeth of these winds.

Gusty north-westerlies alternate with southerlies. North-westerly winds predominate in spring and summer, while southerlies dominate in winter. Records show that in one year, northerlies and north-westerlies blew for 61% of the time and southerlies for 28%. Only 11% of days were calm. Winds of more than 60 kilometres per hour blew on 173 days a year, compared to 30 days for Rotorua and 35 for Nelson.

Worst winds

On rare occasions, tropical cyclones stray south and become severe storms in Wellington. In February 1936 a storm drove ships aground in the harbour and flattened forest in the Tararua Range. In April 1968 a hurricane-force southerly drove the ferry Wahine onto rocks at the harbour’s entrance. Fifty-one lives were lost. The same day, Ōteranga Bay (on the shore of Cook Strait) was hit by a 267 kilometre-per-hour blast – the highest wind gust ever recorded in the region.

Chill southerlies

Wellington’s most severe winds usually come from the south, dragging cold air up from the Southern Ocean, blasting the region and sometimes leaving snow on the higher hills.

Temperature and sunshine

The region’s average daily temperature is 12.8º C (slightly above the national average) and the city has more than 2,000 hours of sunshine a year – similar to Auckland and Christchurch.

The changing climate

In the past, the climate was more severe. The ice ages (the most recent ending 10,000 years ago) caused the sea level to drop more than 100 metres as water was absorbed by extensive polar ice caps. During the coldest phase (about 25,000–15,000 years ago), the sea retreated and much of Cook Strait became a plain stretching far to the west. In the mountains, glaciers formed, and traces can still be seen in the Tararuas today. Elsewhere the rise and fall of the sea level is evident in coastal terraces such as Tongue Point, on the south coast.

Rainfall

The Wellington region receives 1,250 millimetres of rain each year – slightly less than the national average of 1,400 millimetres.

How to cite this page:

Chris Maclean. 'Wellington region - Climate', Te Ara - the Encyclopedia of New Zealand, updated 12-Apr-13
URL: http://www.TeAra.govt.nz/en/wellington-region/page-3