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An ecoregion is a relatively large area of land or water sharing geographically distinct natural communities. Ecoregions have characteristic combinations of climate, topography, soil, flora and fauna. Species found within each ecoregion interact ecologically in ways that are critical for their long term persistence.
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Scroll over map for Ecoregion name Click on Ecoregion for more information |
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| ECOREGIONS WITHIN THE PORCUPINE CARIBOU RANGE | |||||||||||||||||
| Arctic Tundra | |||||||||||||||||
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The north coast of Alaska is a broad, level plain that is generally less than 300m in elevation. It is a treeless, windswept landscape characterized by lakes, wetlands, and permafrost related features. Permafrost is a thick, unbroken layer of ice that lies underneath the ecoregion to depths of 600m in some areas and is almost continuous across the region. When water melts on top of the permafrost, it collects into “thaw” lakes which cover close to 50% of the ecoregion. Due to the abundance of lakes and saturated soils, over 82% of the ecoregion is considered wetland. |
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The severe arctic climate produces short, cool summers and long, cold winters reaching temperatures of -51°C. The average annual temperature varies from -13 to -10 C. In summer, the ecoregion has sunlight 24 hours a day for up to 85 consecutive days, and in winter, it can remain dark 24 hours a day for as long as 67 consecutive days. The growing season averages only two weeks per year with a low average annual precipitation of 10-15 cm that mostly falls as snow during the winter. The entire Arctic Coastal Plain is an important breeding and calving ground for many species including many species of waterfowl that nest on the coastal plain. The ecoregion is important to shorebirds, both nationally and internationally. |
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| Brooks Range - Tundra Polar Desert | |||||||||||||||||
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The Brooks Range is
a northern extension of the Rocky Mountains with elevations ranging from
500 – 2600m. The range is characterized by steep mountains with
scattered glaciers above 1800m. Parts of the range have large lakes created
from glacial moraine dams with high energy streams and rivers cutting
through narrow ravines. Due to the harsh, mountainous terrain and climate
of this ecoregion, vegetation cover is sparse and restricted mostly to
valleys and lower slopes. Wetlands occupy at least 20% of the ecoregion. |
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The
dry polar climate has short, cool summers reaching temperatures of 38°C
and long, cold winters reaching temperatures of -60°C. The average
annual temperatures ranges from -12 to -6°C. The ecoregion gets several
days of 24-hr sunlight in June, and several sunless days in December.
Average annual precipitation averages 15- 33 cm, but drainage is rapid
due to the region’s steep slopes and the low holding capacity of
its soils. Permafrost is continuous under the entire area. |
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| Upper Yukon - Taiga Meadow | |||||||||||||||||
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The Upper Yukon
ecoregion consists of rounded low mountains with elevations ranging from
600 to 1200m, plateaus, and highlands of rolling topography. There are no
glaciers in this region. Vegetation patterns in the region are complex with
white spruce forests at lower elevations and on south facing slopes and
black spruce forests at higher elevations and on north facing slopes. Alpine
meadows are found above the black spruce forest. The extreme continental boreal climate has severely cold winters, and short, hot summers. Average temperatures range from -12°C to -4°C. Annual precipitation averages 26-38cm with precipitation being heaviest in late summer. Annual average snowfall averages 120-250cm. Discontinuous permafrost is found under the entire ecoregion. |
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| Southern Arctic | |||||||||||||||||
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The
Southern Arctic ecozone is characterized by sprawling shrublands, wet sedge
meadows, and many cold, clear lakes. The landscape is largely the result
of glaciers which left piles of bouldery moraines, long eskers up to 100
km and “glacial erratics” of rocks the size of houses that were
torn from the bedrock and carried by the glaciers. Permafrost occurs continuously
throughout the Southern Arctic Ecozone resulting in soils that are often
waterlogged or frozen. The repeated freezing and thawing of this soil creates
fascinating features on the surface. The
extreme polar climate has short (four months), cool summers with temperatures
averaging 5ºC and long, dark, cold winters with temperatures averaging
-28ºC. Average annual precipitation ranges from 25-50cm. |
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| Taiga Plains | |||||||||||||||||
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The Taiga Plains Ecozone is characterized by broad lowlands and plateaus centred on the Mackenzie River (Canada’s largest river) and its many tributaries. In some places the tributaries have cut canyons hundreds of metres deep into the ground. The lowest areas are primarily large wetlands and muskeg with soil being shallow, highly acidic, and nutrient-poor. The floodplains are covered in small lakes and meandering channels with fast eroding banks. The subarctic climate has
short, cool summers with temperatures averaging 7 to 15°C and long,
cold winters with temperatures averaging -15 to -26°C. Snow and freshwater
ice-cover persists for six to eight months a year. Average annual precipitation
ranges from 25-50cm. |
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| Taiga Cordillera | |||||||||||||||||
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The
Taiga Cordillera Ecozone is mountainous terrain (northern extension of the
Rocky Mountains) with towering peaks, rivers with shear rock walls, broad
windswept uplands dominated by alpine and arctic shrubs. This region has
some of Canada’s largest waterfalls, deepest canyons, and wildest
rivers. The ecozone also contains vast wetlands, rolling hills and valleys.
The northern region is dominated by treeless arctic tundra. The extremely cold and humid climate has short, cool summers with temperatures averaging 8 ºC and long, dark winters with temperatures averaging -22 ºC. Average annual precipitation ranges from 25-30 cm with snow and freshwater ice-cover persisting for six to eight months. |
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| Group 8 : Brandi Smithson : Anthony Jjumba : Geog 351 : Fall 06 | |||||||||||||||||