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The former name Barrow was derived from Point Barrow and was originally a general designation because non-native Alaskan residents found it easier to pronounce than the Inupiat name. Point Barrow was named after Sir John Barrow of the British Admiralty by explorer Frederick William Beechey in 1825. A U.S. post office was established in 1901 ...
After getting 30 minutes of daylight, the town of Utqiaġvik, Alaska – formerly known as Barrow – saw its final sunset of the year on Monday as it enters a "polar night." The sun won't return ...
The Barrow Area Information Database (BAID) is designed to support Arctic science with a special focus on the research hubs of Barrow, Atqasuk, and Ivotuk on the North Slope of Alaska. The BAID Internet Map Server (BAID-IMS) is freely available to scientists, land managers, educators and the local community.
Sunshine hours for selected cities in North America and Central America Country City Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year Ref. Canada Calgary: 119.5 144.6 177.2 220.2 249.4 269.9 314.1 284.0 207.0 175.4 121.1 114.0 2,396.3 [191] Canada Churchill: 79.7 117.7 177.8 198.2 197.0 243.0 281.7 225.9 112.0 58.1 55.3 53.1 1,799.5 [192 ...
Ennis, Alaska is modeled on real towns like Utqiaġvik, formerly known as Barrow. Ennis isn't a real town, but the show was based on a real area in the northernmost state: North Slope Borough, Alaska.
For instance, in Fairbanks, Alaska, which is south of the Arctic Circle, the Sun sets at 12:47 a.m. at the summer solstice. This is because Fairbanks is 51 minutes (1 hour and 51 minutes at Daylight Savings Time) ahead of its idealized time zone (as most of the state is in one time zone) and Alaska observes daylight saving time.
Point Barrow or Nuvuk is a headland on the Arctic coast in the U.S. state of Alaska, 9 miles (14 km) northeast of Utqiagvik (formerly Barrow). It is the northernmost point of all the territory of the United States, at 71°23′20″N 156°28′45″W / 71.38889°N 156.47917°W / 71.38889; -156.47917 ( Point Barrow ) , 1,122 ...
Relationship of Earth's axial tilt (ε) to the tropical and polar circles. The Arctic Circle is the southernmost latitude in the Northern Hemisphere at which the centre of the Sun can remain continuously above or below the horizon for twenty-four hours; as a result, at least once each year at any location within the Arctic Circle the centre of the Sun is visible at local midnight, and at least ...