Hail injury

Hail injury - Holes in leaves caused by hailstone
  • Latin name: Ruptio grandinis Nature
  • French name: Bris de grêle
  • Division: Intemperiae
  • Class: Pluviatilae
Description

Micro-habitat(s)

Trunk, Leaf, Branch

Distribution

Canada

Damage, symptoms and biology

Evaporation caused by the sun's heat increases the level of humidity in the air. The warmed air, which is less dense, rises and as it rises, the humid air condenses and cools, eventually reaching a saturation point. That is when the droplets of water form clouds. If a thunderstorm cell forms, it is cooled more and more by the air, reaching temperatures of - 40°C to - 55°C. These low temperatures exist in the upper part of the cloud at altitudes ranging from 8 000 m (25 000 ft) to 12 000 m (40 000 ft). The resulting ice falls to the ground as hail. Minor damage to trees may include lacerations and perforations of foliage. Deep lacerations of the bark of twigs in the upper part of the tree are a more serious type of damage. These injuries can reduce sap flow in the distal portion of the wound and cause wilting of the foliage.

Other information

A hailstone normally has a diameter varying between 1 and 2 cm. In 1986, hailstones the size of tennis balls (8 cm in diameter) fell in Montreal. But the largest hailstones on record fell in Nebraska in 1928; they were 44 cm in diameter and weighed 744 grams.

Canadian Forest Service Publications

Hail injury

Information on host(s)

Main host(s)

Conifer, deciduous

Photos
  • Hail injury Holes in leaves caused by hailstone
  • Hail injury Bark laceration
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