Hoar frost landscape, Hertfordshire, UK, rural scene, low winter sunshine

Hoar frost landscape, Hertfordshire, UK, rural scene, low winter sunshine Stock Photo
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Contributor:

Scenics & Science / Alamy Stock Photo

Image ID:

D757A7

File size:

43.7 MB (2.4 MB Compressed download)

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Dimensions:

5616 x 2718 px | 47.5 x 23 cm | 18.7 x 9.1 inches | 300dpi

Date taken:

13 April 2013

More information:

Hoar frost (also called radiation frost or hoarfrost or pruina) refers to the white ice crystals, loosely deposited on the ground or exposed objects, that form on cold clear nights when heat is lost into the open sky causing objects to become colder than the surrounding air. A related effect is flood frost or frost pocket which occurs when air cooled by ground-level radiation losses travels downhill to form pockets of very cold air in depressions, valleys, and hollows. Hoar frost can form in these areas even when the air temperature a few feet above ground is well above freezing. Nonetheless the frost itself will be at or below the freezing temperature of water. Hoar frost may have different names depending on where it forms. For example, air hoar is a deposit of hoar frost on objects above the surface, such as tree branches, plant stems, wires; surface hoar is formed by fernlike ice crystals directly deposited on snow, ice or already frozen surfaces; crevasse hoar consists of crystals that form in glacial crevasses where water vapour can accumulate under calm weather conditions; depth hoar refers to cup shaped, faceted crystals formed within dry snow, beneath the surface. The name hoar comes from an Old English adjective for showing signs of old age, and is used in this context in reference to the frost which makes trees and bushes look like white hair. It may also have association with hawthorn when covered in its characteristic white spring blossom. Surface hoar is a cause of avalanches when it forms on top of snow. Conditions are ideal for the formation of hoarfrost on cold clear nights, with a very light wind that is able to circulate more humidified air around the snow surface. Wind that is too abrupt will destroy the crystals. When buried by subsequent snows they may remain standing for easy identification, or become laid down, but still dangerous because of the weakness of the crystals. In low temperatures surface hoar can also be broken apart and blow