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The lowest air temperature record, the lowest reliably measured temperature on Antarctica was set on 21 July 1983, when a temperature of −89.2 °C (−128.6 °F) was observed at Vostok Station. [2] [5] For comparison, this is 10.7 °C (19.3 °F) colder than subliming dry ice (at sea level pressure). The elevation of the location is 3,488 ...
Average yearly temperature is 22.4 °C, ranging from an average minimum of 12.2 °C to a maximum of 29.9 °C. The average temperature range is 11.4 °C. [6] Variability throughout the year is small (standard deviation of 2.31 °C for the maximum monthly average and 4.11 °C for the minimum). The graph also shows the typical phenomenon of ...
To accommodate the lowest points on Earth, the model starts at a base geopotential altitude of 610 meters (2,000 ft) below sea level, with standard temperature set at 19 °C. With a temperature lapse rate of −6.5 °C (-11.7 °F) per km (roughly −2 °C (-3.6 °F) per 1,000 ft), the table interpolates to the standard mean sea level values of ...
July is the warmest month, with an average temperature of 77 °F (25.0 °C). Salt Lake City's record high minimum temperature is 81 °F (27.2 °C), set on July 18, 2016, and its record high temperature is 107 °F (42 °C), first set on July 26, 1960 and again on July 13, 2002 (although the temperature in 2002 was slightly higher). [5]
Much of the year's 61.9 inches (1,570 mm) of rainfall occurs during this period. Extreme temperatures range from 27 F [3] on February 3, 1917, [4] to 100 °F on July 21, 1942, (−2.8 to 38 °C), the only triple-digit (°F) reading on record; [5] the more recent freezing temperature seen at Miami International Airport was on December 25, 1989. [6]
The Adirondacks typically experience pleasant dry weather in the summer, with average daily maximum temperatures in the range of 66 °F–73 °F (18–22 °C). Evenings in the Adirondacks are chilly, with average daily minimum temperatures ranging on average between 45 °F–54 °F (7–12 °C).
This is a list of cities by average temperature (monthly and yearly). The temperatures listed are averages of the daily highs and lows. Thus, the actual daytime temperature in a given month may be considerably higher than the temperature listed here, depending on how large the difference between daily highs and lows is.
The potential temperature of a parcel of fluid at pressure is the temperature that the parcel would attain if adiabatically brought to a standard reference pressure , usually 1,000 hPa (1,000 mb). The potential temperature is denoted θ {\displaystyle \theta } and, for a gas well-approximated as ideal , is given by