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Country / region Average male height Average female height Stature ratio (male to female) Sample population / age range Share of pop. over 18 covered [9] [10] [b] Method
Generally there are relatively small variations between summer and winter temperatures. An example of this is Auckland which has a variation of just 9 °C or 16 °F between the average mid-winter high temperature (14.7 °C or 58.5 °F) and average mid-summer high temperature (23.7 °C or 74.7 °F).
The Auckland Region is New Zealand's most populous territorial authority and Auckland its most populous city. In the 2018 census, 1,571,718 persons declared themselves as residents of the region – an increase of 156,178 people or 11.0% since the 2013 census. The Auckland Region accounts for about one-third (33.4%) of New Zealand's population.
The average annual precipitation for New Zealand as a whole is 2.1 m (6 ft 11 in). In mountain portions of the West Coast, it exceeds 10 m per year. The distribution of precipitation across the country is determined by its location with the mid-southern latitudes and its topography.
Climate charts provide an overview of the climate in a particular place. The letters in the top row stand for months: January, February, etc. The bars and numbers convey the following information: The blue bars represent the average amount of precipitation (rain, snow etc.) that falls in each month. The blue numbers are the amount of ...
New Zealand’s largest city experiences 2.5 times an entire summer’s rain in just a month Skip to main content. 24/7 Help. For premium support please call: 800-290 ...
Men earn more than women on average, with the median income for men in 2011 being $31,500, $12,400 more than women. [124] The highest median personal income were for people identifying with the European or "other" ethnic group, while the lowest was from the Asian ethnic group. The median income for people identifying as Māori was $20,900. [125]
These landscapes can affect the local climate, such as the 2.5 °C temperature rise in Christchurch from the urban heat island effect [33] or the decreased transpiration from farmland. [34] This increase in soil water content and reduction in the stabilising effects of roots leaves deforested areas prone to soil loss and landslides.