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Climatic characteristics of Canada
Climate characteristics of Canada: Canada has abundant sunshine and distinct seasons.

Most areas belong to continental temperate coniferous forest climate. It is spring from mid-March to late June. It is summer from late June to mid-September, autumn from mid-September to late June in 65438+February, and winter from late June to mid-March in 65438+February.

Most plants in southern Canada begin to germinate in March and bloom in April and May. But in Vancouver and Victoria on the west coast, spring is about two months ahead of schedule, which is the shortest and mildest winter in Canada.

The eastern part of Canada is the low Labrador Plateau, and the southeastern part is Lake Superior, Lake Huron, Lake Erie and Lake Ontario, which are connected with Lake Michigan in the United States to form the St. Lawrence River, sandwiched between the St. Lawrence Mountains and the Appalachian Mountains, forming a valley with flat terrain and many basins.

In the west is the Rocky Mountains of the Cordillera Mountains, with many peaks over 4000 meters above sea level. The highest peak, Logan Peak, is located in the Loki Mountains in the west, with an altitude of 595 1 meter. Arctic islands are mostly hills and low mountains, which are covered with snow and ice due to the polar climate. The central part is the Great Plains and the Lauren Qin Low Plateau, accounting for about half of the country.