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The dew point of a given body of air is the temperature to which it must be cooled to become saturated with water vapor. This temperature depends on the pressure and water content of the air. When the air is cooled below the dew point, its moisture capacity is reduced and airborne water vapor will condense to form liquid water known as dew. [1]
These measurements reflect averages over a large region and so are lower than the maximum point surface temperature. [ 6 ] Satellite measurements of the surface temperature of Antarctica, taken between 1982 and 2013, found a coldest temperature of −93.2 °C (−135.8 °F) on 10 August 2010, at 81°48′S 59°18′E / 81.8°S 59.3°E ...
The temperature at which frost will form is called the dew point, and depends on the humidity of the air. [1] When the temperature of the air drops below its dew point, excess water vapor is forced out of solution, resulting in a phase change directly from water vapor (a gas) to ice (a solid).
Date Location Highest Temperature: 106 °F (41 °C) 23 August 1916 Torrington, CT [1] 15 July 1995 Danbury, CT: Lowest Temperature: −32 °F (−36 °C) 16 February 1943 Norfolk, CT “The Ice Box of CT” [1] 22 January 1961 Coventry, CT
Very famous books and books for children may be listed both places to help people find them. This page was last edited on 10 December 2018, at 18:38 (UTC). Text is ...
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When temperatures are low enough, the water droplets freeze into ice particles known as frost. dew point (T d) Also dewpoint or dew-point. The temperature to which an air parcel must be cooled, at constant pressure and moisture content, in order for saturation to occur. Continued cooling below the dew point will cause condensation of water ...
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