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  1. en.wikipedia.org › wiki › AucklandAuckland - Wikipedia

    Auckland ( / ˈɔːklənd / AWK-lənd; [6] Māori: Tāmaki Makaurau) is a large metropolitan city in the North Island of New Zealand. It has an urban population of about 1,478,800 (June 2023). [4]

  2. 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.

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  4. 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. Summers are becoming longer and hotter, and some glaciers have melted completely and others have shrunk.

  5. The hottest months in New Zealand are January and February, and the coldest month of the year is July. The average temperature in New Zealand decreases as you travel south. Rain, snow and sun . New Zealand is lush and green for a reason! Our average rainfall is high and spread evenly throughout the year.

  6. The average temperature ranges from 11.3 °C (52.3 °F) in July to 20.5 °C (69 °F) in February. Here are the average temperatures. Rainfall is fairly abundant, since it amounts to 1,200 millimeters (47 inches) per year, and it's well distributed over the months. However, the rainiest season is winter. Here is the average precipitation.

  7. Resources. Climate of New Zealand. Temperature records. The highest temperature ever recorded in New Zealand was 42.4 °C (108.3 °F) on 7 February 1973 in Rangiora. [1] The lowest temperature ever recorded in New Zealand was −25.6 °C (−14.1 °F) on 18 July 1903 in Ranfurly. Highest & lowest temperatures measured in New Zealand. Lowest.

  8. Figure 6b. Tropical cyclones which made landfall in New Zealand during January, 1970-2010. Source: SPEArTC (Diamond et al., 2012). 10 Southwesterly wind flows in winter Due to the tendency for anticyclones to form over Australia in winter, and for a major trough of low pressure to lie to the east of New Zealand, southwest

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