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Yellowknife experiences very cold winters and mild to warm summers. The average temperature in January is around −26 °C (−15 °F) and 17 °C (63 °F) in July. [44] According to Environment and Climate Change Canada, Yellowknife has the sunniest summer in the country, averaging 1,034 hours from June to August. [46]
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The climate of the ecoregion is Subarctic climate, without dry season (Köppen climate classification Subarctic climate (Dfc)). This climate is characterized by mild summers (only 1-3 months above 10 °C (50.0 °F)) and cold, snowy winters (coldest month below −3 °C (26.6 °F)). [5] [6] Precipitation averages 200 - 400 mm/year. [1]
Köppen climate types in the Northwest Territories. The Northwest Territories extends for more than 1,300,000 km 2 (500,000 sq mi) and has a large climate variant from south to north. The southern part of the territory (most of the mainland portion) has a subarctic climate, while the islands and northern coast have a polar climate.
With government funding, the Dene village of NdilĒ« was developed in the mid 1950s on the tip of Latham Island (the northern point of Yellowknife's Old Town). The Yellowknives Dene First Nation was formed in 1991 (formerly known as Yellowknife B Band) following the collapse of a territorial-wide comprehensive land claim negotiation. They ...
Primarily wilderness, the Taiga Shield is sparsely populated, with approximately 340,000 inhabitants, over 60% of which is First Nations. [6] Most settled areas developed around mining or hydroelectric activity, for example in Yellowknife and Uranium City in the west and Labrador City in the east, but are isolated from other communities.
Map of the world using hexagons of the same area, with landmasses and oceans categorized as different Lifezones, also arranged hexagonally. The Holdridge life zones system is a global bioclimatic scheme for the classification of land areas. It was first published by Leslie Holdridge in 1947, and updated in 1967.
The Köppen climate classification divides climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are A (tropical), B (arid), C (temperate), D (continental), and E (polar).