Ground frost
Ground frost refers to the various coverings of ice produced by the direct deposition of water vapor on objects and trees, whose surfaces have a temperature below the freezing point of water (0 °C, 32 °F).[1]
Types[]
The three main types of ground frost are radiation frost (hoar frost), advection frost (advection hoar frost) and evaporation frost. The latter is a rare type which occurs when surface moisture evaporates into drier air causing its temperature at the surface to fall at or under the freezing point of water.[1] Rime (both soft and hard) is technically not a type of ground frost.
Alternative definition[]
Ground frost may also refer to the condition when the temperature of the upper layer of the soil falls below the freezing point of water.[1]
In England[]
From 1906 to 1960 the Met Office practice was to base the number of days of ground frost on this criterion: a day with a minimum temperature reaching 30 °F (−1 °C), probably because 32 °F (0 °C) was not considered enough cold to cause damage to growing plants. Since 1961 the statistics have referred to the number of days with grass minimum temperature below 0°C. Occasionally, the term ground frost can still be seen, but it means simply a minimum temperature below 0 °C.[2]
See also[]
- Frost
- Frost (temperature)
References[]
- ^ Jump up to: a b c International Meteorological Vocabulary. Geneva: Secretariat of the World Meteorological Organization. 1992.
- ^ D.H. McIntosh, ed. (1972). Meteorological Glossary. London: Her Majesty's Stationery Office.
- Snow or ice weather phenomena