Frost Cracks
Frost cracks appear as shallow to deep, longitudinal cracks in the trunk of trees. Frost cracks often, but not always, occur on the south or southwest sides of trees because this area experiences the greatest temperature fluctuations between day and night.
On a bitterly cold day, with full sun, the trunk of a tree is warmed by the sun and expands. A sudden drop in temperature, due to development of cloud cover or the setting of the sun, causes the outer layer of wood to contract more rapidly than the inner layer, which results in a long vertical crack at weak points in the trunk.
Once a frost crack occurs on a tree, it is likely to appear annually.
Young trees with thinner bark are more susceptible to this. Trees most susceptible to frost cracks include London plane, maple species, crabapples, fruit trees, lindens, poplars, birches, and willows.
Sunscald and Frost Cracks
Sunscald can occur under the same conditions that cause frost cracks. Frost cracks and sunscald can occur together or separately.
Sunscald often appears as an elongated canker or damaged areas on the trunks of thin-barked trees. Sunscald often develops on the south or southwest side of trees following a sudden exposure to direct sun.
In winter, the temperatures on the sun side of the trunk may exceed air temperatures by as much as 20°F. This is thought to trigger the de-acclimation of trunk tissue. The bark slowly darkens, turns reddish-brown, and becomes rough. After a time, the callus tissue eventually cracks and falls away. Sometimes only the outermost cambium layer is damaged and a sunken area appears on the trunk.
Affected trees often have sparse foliage, stem dieback, and stunted growth.