Search results
Results From The WOW.Com Content Network
The two major Canadian cities that fall outside the continental climate schema are Vancouver and Victoria. Vancouver experiences an oceanic climate, bordering warm-summer mediterranean with a marked summer dry season. Victoria, BC is the only major Canadian city entirely in a warm-summer mediterranean climate.
In 2014, the Canadian Council on Ecological Areas (CCEA) released an update to the first digital version of the Canadian Ecological Framework (CEF). The new spatial framework was designed to replace the 1995 ecological framework as well as the Ecozone+ framework used in the Canadian Biodiversity: Ecosystem Status and Trends 2010 Report.
Climate is a major barrier to life; the growing season is extremely short. Mean average temperature usually ranges from 0 °C (32 °F) to 4 °C (39 °F), and even in summer the average temperature does not exceed 10 °C (50 °F). The zone sees heavy precipitation, usually in the form of snow. [3]
The Canadian Prairies (usually referred to as simply the Prairies in Canada) is a region in Western Canada. It includes the Canadian portion of the Great Plains and the Prairie provinces, namely Alberta, Saskatchewan, and Manitoba. [2] These provinces are partially covered by grasslands, plains, and lowlands, mostly in the southern regions.
Boreal forest covers much of the shield, with a mix of conifers that provide valuable timber resources in areas such as the Central Canadian Shield forests ecoregion that covers much of Northern Ontario. The Canadian Shield is known for its vast mineral reserves such as emeralds, diamonds and copper, and is there also called the "mineral house ...
Because of its location east of the Rocky Mountains, the Prairies ecozone can be semi-arid in some areas, annual precipitation generally increases farther east in the ecozone from 250 millimetres (9.8 in) in southern Alberta and Saskatchewan to 700 millimetres (28 in) in parts of Manitoba, as well humidity increases eastward through this zone. [5]
Additionally, Yukon glaciers have lost 22% of their surface area (a total loss of 2,541 ± 189 km 2) over the last 50 years, corresponding to a total mass loss of 406 ± 177 Gigatonnes (equivalent to 1.13 ± 0.49 millimeter of global sea level rise). Rainfall in the Canadian Arctic has increased by more than 20% in the last decades.
The climate and ecology of different locations on the globe naturally separate into life zones, depending on elevation, location, and latitude. The generally strong dependency on elevation is known as altitudinal zonation : the average temperature of a location decreases as the elevation increases.