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Probable fogbow in Utqiagvik Homes along the Arctic Ocean in Utqiagvik Utqiagvik sea ice, July 2006, 2007. Owing to its location 330 mi (530 km) north of the Arctic Circle, Utqiagvik's climate is cold and dry, classified as a tundra climate (Köppen ET). Winter weather can be hazardous because of the combination of cold and wind, while summers ...
Following the Chukchi Sea coast, the Chukchi Corridor stretches from Point Hope, Alaska to Utqiagvik, Alaska. From winter through early summer, the area is covered in sea ice with recurring openings in the ice that allow wildlife to migrate north from the Bering Sea to areas of the Chukchi or Beaufort seas during spring and early summer [2]
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 ...
The town of Utqiagvik, Alaska won't see the sun again until January as it enters a polar night. Here's what to know about the phenomenon. The town of Utqiagvik, Alaska won't see the sun again ...
This visual shows the Arctic sea ice change and the corresponding absorbed solar radiation change during June, July, and August from 2000 through 2014. The Arctic ice pack is the sea ice cover of the Arctic Ocean and its vicinity. The Arctic ice pack undergoes a regular seasonal cycle in which ice melts in spring and summer, reaches a minimum ...
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]
DMSP satellite. Useful satellite data concerning sea ice began in December 1972 with the Electrically Scanning Microwave Radiometer (ESMR) instrument. However, this was not directly comparable with the later SMMR/SSMI, and so the practical record begins in late 1978 with the launch of NASA's Scanning Multichannel Microwave Radiometer (SMMR) satellite., [5] and continues with the Special Sensor ...
Unlike polynyas, which tend to occur, and remain, at a given location, leads are transient features that can form anywhere in an ice-covered ocean. [6] Moreover, while the origin of polynyas is linked with either warm air current circulation from the coastline or a warm water upwelling, the driving force behind lead formation is a state of stress, either wind- or current-induced, within the ...