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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
A United Nations agency confirmed today that an arctic temperature record of more than 100.4 degrees Fahrenheit was reached in a Siberian town last year.
Highest dew point temperature: A dew point of 35 °C (95 °F) — while the temperature was 42 °C (108 °F) — was observed at Dhahran, Saudi Arabia, at 3:00 p.m. on 8 July 2003. [ 202 ] Highest heat index : In the observation above at Dhahran, Saudi Arabia, the heat index ("feels like" temperature) was 81.1 °C (178.0 °F).
The same stretch of days last January brought temperatures of 11, 6 and 3.3 degrees Fahrenheit above the historical average for Minneapolis, Chicago and New York City, respectively.
Some parts of the Arctic are covered by ice (sea ice, glacial ice, or snow) year-round, especially at the most poleward parts; and nearly all parts of the Arctic experience long periods with some form of ice or snow on the surface. Average January temperatures range from about −40 to 0 °C (−40 to 32 °F), and winter temperatures can drop ...
The new record should be a wake-up call for the rest of the world, scientists say, because it means the planet is growing warmer.
The Arctic Circle, at roughly 66.5° north, is the boundary of the Arctic waters and lands. The Arctic Circle is one of the two polar circles, and the northernmost of the five major circles of latitude as shown on maps of Earth at about 66° 34' N. [1] Its southern counterpart is the Antarctic Circle.
Skin can freeze in roughly one minute when the air temperature is -22 degrees Fahrenheit and the wind speed is roughly 10 miles per hour, according to the Kentucky Transportation Cabinet.