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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.
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. This new ecozone map includes 18 terrestrial, 12 marine and 1 freshwater ecozone, the latter two of which were derived from the marine bioregions outlined ...
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 regional climate has long, cold winters and short summers, conditions which are moderated in coastal regions. [2] Summers in the east are warmer than those in the west of the region. [2] The mean annual temperature ranges from -4 °C in northern Saskatchewan to 5.5 °C in Newfoundland. [2] Precipitation increases from west to east. [2]
Rainfall in the Canadian Arctic has increased by more than 20% in the last decades. However, the degree of rainfall increase is subject to variation from one location to the next. For example, in Resolute, Nunavut in the period of 1948 to 2007, there was a 48% increase in rainfall recorded with an average of 13.6 mm (0.54 in) of rain per decade.
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.
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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]