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The frost line—also known as frost depth or freezing depth—is most commonly the depth to which the groundwater in soil is expected to freeze. The frost depth depends on the climatic conditions of an area, the heat transfer properties of the soil and adjacent materials, and on nearby heat sources.
Map showing the snowbelts around the Great Lakes of North America with 150 cm (60 in) accumulations or more during winter. The Snowbelt, Snow Belt, Frostbelt, or Frost Belt [1] is the region near the Great Lakes in North America where heavy snowfall in the form of lake-effect snow is particularly common. [2]
The coldest parts of Canada were the eastern prairie provinces, Ontario, Quebec, and the Northwest Territories. However, only southern Ontario set temperature records. During most of the early cold wave, Winnipeg was the coldest major city in Canada. On January 6, it reached a low of −37 °C (−35 °F), while on January 7, the low was −36 ...
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The Great Lakes Basin consists of the Great Lakes and the surrounding lands of the states of Illinois, Indiana, Michigan, Minnesota, New York, Ohio, Pennsylvania, and Wisconsin in the United States, and the province of Ontario in Canada, whose direct surface runoff and watersheds form a large drainage basin that feeds into the lakes.
At least 22 deaths in North America have been directly attributed to the cold wave, with several of these people frozen to death (hypothermia).[3]Around 2,700 flights were canceled on January 30, with 2,000 canceled the next day. [11]
Köppen climate classification types of Canada. ... First frost Last frost Frost-free Baker Lake: NU: 0.21: 13.1: ... Maps Weather Stations locations in Canada. ...
The watersheds are located in the states of Indiana, Michigan, New York, Ohio, and Pennsylvania in the United States, and in the province of Ontario in Canada. The basin is part of the Great Lakes Basin and Saint Lawrence River Watershed, which feeds into the Atlantic Ocean . 80% of the lake's water flows in from the Detroit River , with only 9 ...