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As at 1 August 2008, NIWA had 1339 operational stations in its climate and water monitoring networks, spread throughout New Zealand, including the Chatham Islands. [12] NIWA also holds data from more than 3000 closed stations, many of which have long usable records. [ 12 ]
The climate of New Zealand is varied due to the country's diverse landscape. Most regions of New Zealand belong to the temperate zone with a maritime climate (Köppen climate classification: Cfb) characterised by four distinct seasons. Winters are relatively mild and summers comparatively cool.
Raoul Island (Sunday Island; Māori: Rangitāhua [1]) is the largest and northernmost of the main Kermadec Islands, 900 km (560 mi) south south-west of 'Ata Island of Tonga and 1,100 km (680 mi) north north-east of New Zealand's North Island.
It is the most populous city of New Zealand and the fifth largest city in Oceania. While Europeans continue to make up the plurality of Auckland's population, the city became multicultural and cosmopolitan in the late-20th century, with Asians accounting for 31% of the city's population in 2018. [7]
www.metservice.com. Meteorological Service of New Zealand Limited (MetService) (Māori: Te Ratonga Tirorangi, lit. 'Satellite Service') is the national meteorological service of New Zealand. MetService was established as a state-owned enterprise in 1992. It employs about 300 staff, and its headquarters are in Wellington, New Zealand.
Climate change in New Zealand. Atmospheric carbon dioxide record from Baring Head, Wellington from 1977 to present. [1] Climate change in New Zealand involves historical, current and future changes in the climate of New Zealand; and New Zealand's contribution and response to global climate change. [2][3] Summers are becoming longer and hotter ...
The environment of New Zealand is characterised by an endemic flora and fauna which has evolved in near isolation from the rest of the world. [1] The main islands of New Zealand span two biomes, temperate and subtropical, complicated by large mountainous areas above the tree line. [2] There are also numerous smaller islands which extend into ...
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, [1][2] with several later modifications by Köppen, notably in 1918 and 1936. [3][4] Later, German climatologist Rudolf Geiger (1894–1981) introduced ...