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Köppen climate types of New Zealand. 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.
New Zealand's forest ecosystems for example are being considered as the second most endangered of the world, with only 7% of the natural habitat remaining. [12] A male brown kiwi. Eighty per cent of New Zealand's biota is endemic. New Zealand's biodiversity exhibits high levels of endemism, both in its flora and fauna.
A report in 2017, Adapting to Climate Change in New Zealand, identifies Māori as among the most vulnerable groups to climate-change in New Zealand due to their "significant reliance on the environment as a cultural, social and economic resource". [99] Māori tend to be involved in primary industries, and many Maori communities were near the coast.
New Zealand's climate is predominantly temperate maritime (Köppen: Cfb), with mean annual temperatures ranging from 10 °C (50 °F) in the south to 16 °C (61 °F) in the north. [109] Historical maxima and minima are 42.4 °C (108.32 °F) in Rangiora, Canterbury and −25.6 °C (−14.08 °F) in Ranfurly, Otago. [110]
After a British colony was established in New Zealand in 1840, William Hobson, then Lieutenant-Governor of New Zealand, chose Auckland as its new capital. Ngāti Whātua Ōrākei made a strategic gift of land to Hobson for the new capital. Hobson named the area after George Eden, Earl of Auckland, British First Lord of the Admiralty. Māori ...
An old castaway hut on the Antipodes Islands.. The islands constituting this ecoregion share a long history of isolation, both from other landmasses and each other. The isolation, combined with harsh climates characterised by low temperatures, strong westerly winds and few hours of sunlight in winter, have resulted in the evolution of many endemic plants and animals, though species richness is ...
An analysis in 2004 of long term records from four New Zealand tide gauges indicated an average rate of increase in sea level of 1.6 mm a year for the 100 years to 2000, which was considered to be relatively consistent with other regional and global sea level rise calculations when corrected for glacial-isostatic effects. [8]
The Auckland Islands were part of the Colony of New Zealand under the Letters Patent of April 1842, which fixed the southern boundary of New Zealand at 53° south, but they were then excluded by the New Zealand Constitution Act 1846, which defined the southern boundary at 47° 10' south; however, they were again included by the New Zealand ...
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