The Interior Yukon–Alaska alpine tundraecoregion (WWF ID: NA1111) covers alpine, sub-alpine, and boreal forest areas along the cordillera (chain of mountain ranges) of Interior Alaska and south-central Yukon Territory. Geologically, they are the disjunct uplands of the Yukon–Tanana terrane plus a southern extension of the Brooks Range. The cover is extensive 'dark taiga' of closed spruce forest, open forest of other species (aspen, willow, pine, fir), and alpine vegetation at higher altitudes.[1][2][3][4] The region is mostly wilderness and relatively untouched by human development.
The valleys below these ridges are of the 'Interior Alaska-Yukon lowland taiga' ecoregion, with the Yukon River on the north and the Tanana River on the south. The mean elevation is 837 metres (2,746 ft), the highest is 2,745 metres (9,006 ft).[3]
Climate
The climate of the ecoregion is Tundra climate (Köppen climate classification ET), a local climate in which at least one month has an average temperature high enough to melt snow (0 °C (32 °F)), but no month with an average temperature in excess of 10 °C (50 °F).[5][6] The area is affected by a rain shadow effect caused by the Alaska Range to the south screening storms from the Gulf of Alaska. Average annual precipitation at Fairbanks is 287 mm/year; precipitation may reach 600 mm/year in the higher elevations. Permafrost is found at the higher elevations and more northerly extents of the ecoregion.[4]
Flora and fauna
The most common trees are white spruce (Picea glauca) and black spruce (Picea mariana). 32% of the region is closed needle-leaf evergreen forest, 26% is other types of open and closed forest, 20% shrub, 16% herbaceous vegetation, and rest bare ground or water.[3]