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A map of the Arctic. The red line is the 10 °C isotherm in July, commonly used to define the Arctic region; also shown is the Arctic Circle. The white area shows the average minimum extent of sea ice in summer as of 1975. [1] The climate of the Arctic is characterized by long, cold winters
The 24-hour daylight of the Arctic summer attracts visitors from afar, including huge flocks of seabirds like the crested auklet. A male must use both his song and a secret tangerine perfume if he is to attract a mate. For the resident walrus, the summer heat can be unbearable. After hauling himself to the beach to moult, an old male uses an ...
The Arctic sea ice minimum is the day in a given year when Arctic sea ice reaches its smallest extent, occurring at the end of the summer melting season, normally during September. Arctic Sea ice maximum is the day of a year when Arctic sea ice reaches its largest extent near the end of the Arctic cold season, normally during March. [14]
NEW YORK (Reuters) -Millions of Americans awoke on Tuesday to snow, freezing rain and frigid temperatures as an Arctic blast gripped much of the United States, ending a nearly two-year "snow ...
Shockingly cold air funneled directly from the Arctic will be making an unwelcome appearance across nearly the entire eastern half of the country this weekend and into early next week, forecasters ...
In winter, this relatively warm water, even though covered by the polar ice pack, keeps the North Pole from being the coldest place in the Northern Hemisphere, and it is also part of the reason that Antarctica is so much colder than the Arctic. In summer, the presence of the nearby water keeps coastal areas from warming as much as they might ...
The weeklong Arctic cold that's blanketed much of the nation has taken more than 50 lives, officials said, as 95 million people in the United States are under winter weather warnings Friday.
The Arctic's indigenous people have a long relationship with its icy conditions, and face the loss of their cultural heritage. Further, there are numerous implications which go beyond the Arctic region. Sea ice loss not only enhances warming in the Arctic but also adds to global temperature increase through the ice-albedo feedback.
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