Middle Arctic tundra explained

Canadian Middle Arctic Tundra
Map:Middle Arctic tundra map.svg
Map Size:300
Map Alt:Ecoregion territory (in green)
Ecozone:Nearctic
Biome:Tundra
Border1:Arctic coastal tundra
Border2:Davis Highlands tundra
Border3:High Arctic tundra
Border4:Low Arctic tundra
Area:1034340
Country:Canada
State1:Northwest Territories
State2:Nunavut
State3:Quebec
Region Type:Province/Territory
Coordinates:67.25°N -91.75°W
Climate:Polar

The Canadian Middle Arctic Tundra ecoregion 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] [5] 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]

Location and description

The ecoregion stretches over 2500km (1,600miles) 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 176m (577feet)).

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 10C.[6] [7] In this ecoregion, the mean summer month temperature ranges from 0.5C in the north to 4.5C 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

Notes and References

  1. Web site: Middle Arctic tundra. World Wildlife Federation. en. March 21, 2020.
  2. Web site: Map of Ecoregions 2017. Resolve, using WWF data. en. September 14, 2019.
  3. Web site: Middle Arctic tundra. Digital Observatory for Protected Areas. en. August 1, 2020.
  4. Web site: Middle Arctic tundra. The Encyclopedia of Earth. en. August 28, 2020.
  5. https://www.oneearth.org/ecoregions/canadian-middle-arctic-tundra/
  6. Web site: M. . Kottek . J. . Grieser . C. . Beck . B. . Rudolf . F. . Rubel . 2006 . World Map of Koppen-Geiger Climate Classification Updated. Gebrüder Borntraeger 2006. en. September 14, 2019.
  7. Web site: Dataset - Koppen climate classifications. World Bank. en. September 14, 2019.