Middle Arctic tundra

The Middle Arctic tundra ecoregion (WWF ID: NA1115) covers a broad stretch of northern Canada - the southern islands of the Arctic Archipelago, plus the northern mainland of Nunavut and, across Hudson Bay to the east, a portion of northern Quebec.[1][2][3][4] This is the coldest and driest ecoregion in Canada, and can be referred to as a 'polar desert'. It is an important region for breeding and migratory birds, and supports 80% of the world's muskox.[1]

Middle Arctic tundra
Muskoxen on Victoria Island (Canada)
Ecoregion territory (in green)
Ecoregion territory (in green)
Ecology
RealmNearctic
BiomeTundra
Borders
Geography
Area1,034,340 km2 (399,360 sq mi)
CountryCanada
Province/Territory
Coordinates67.25°N 91.75°W / 67.25; -91.75
Climate typePolar

Location and description

The ecoregion stretches over 2,500 kilometres (1,600 mi) from west to east: Banks Island, Victoria Island, King William Island, northeast Nunavut, and the southern portions of Prince of Wales Island and Baffin Island. Most of the territory rolling lowlands (mean elevation is 176 metres (577 ft)).

The ecoregion to the north is the 'High Arctic tundra' (colder and wetter), to the south is the Low Arctic tundra (warmer and wetter).[2] The bedrock under the western extent is Paleozoic and Mesozoic sedimentary rock with a relatively flat cover of glacial moraines and marine deposits. The eastern bedrock is older Precambrian granite, with rockier topography. Permafrost is continuous under the whole region, with depths up to hundreds of meters.[1] The northern islands are surrounded by pack ice most of the year.

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] In this ecoregion, the mean summer month temperature ranges from 0.5 °C (32.9 °F) in the north to 4.5 °C (40.1 °F) in the south. Average annual precipitation is low, from 100-200 mm/year. Snow covers the ground for 10 months each year.[1]

Flora and fauna

The middle arctic tundra is north of the treeline. 56% of the ground cover is moss and lichen, 30% is low herbaceous vegetation tolerant of the cold and dry environment, 1% is herbaceous wetlands, and up to 1% supports shrubs in protected areas.[1] Because of the harsh conditions—the cold, aridity, wind and poor, thin soils—vegetation is sparse and stunted. The rare protected area for shrubs is characterized by arctic willow (Salix arctica) and dwarf birch (Betula) and alder (Alnus); the herb cover by Saxifraga species and Dryas).[4]

Characteristic mammals include barren-ground caribou (Rangifer tarandus ssp. arcticus), muskox (Ovibos moschatus), wolf (Canis lupus), arctic fox (Alopex lagopus), polar bear (Ursus maritimus, arctic hare (Lepus arcticus, brown lemming (Lemmus sibiricus) and collared lemming (Dicrostonyx groenlandicus). The region supports up to 80% of the world's musk ox (Ovibos moschatus).[4]

The region supports important breeding and migratory grounds for birds, including snow goose (Chen caerulescens), brant (Branta bernicla), Canada goose (Branta canadensis), eider (Somateria spp.) and oldsquaw duck (Clangula hyemalis).[4]

Protected areas

Over 5% of the ecoregion is officially protected.[3] These protected areas include:

See also

References
  1. "Middle Arctic tundra". World Wildlife Federation. Retrieved March 21, 2020.
  2. "Map of Ecoregions 2017". Resolve, using WWF data. Retrieved September 14, 2019.
  3. "Middle Arctic tundra". Digital Observatory for Protected Areas. Retrieved August 1, 2020.
  4. "Middle Arctic tundra". The Encyclopedia of Earth. Retrieved August 28, 2020.
  5. Kottek, M., J. Grieser, C. Beck, B. Rudolf, and F. Rubel, 2006. "World Map of Koppen-Geiger Climate Classification Updated" (PDF). Gebrüder Borntraeger 2006. Retrieved September 14, 2019.{{cite web}}: CS1 maint: multiple names: authors list (link)
  6. "Dataset - Koppen climate classifications". World Bank. Retrieved September 14, 2019.
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