sdu faculty of forestry journal special edition 2009 - Orman Fakültesi
sdu faculty of forestry journal special edition 2009 - Orman Fakültesi
sdu faculty of forestry journal special edition 2009 - Orman Fakültesi
You also want an ePaper? Increase the reach of your titles
YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.
SDU Faculty <strong>of</strong> Forestry Journal<br />
Serial: A, Number: Special Issue, Year: <strong>2009</strong>, ISSN: 1302-7085, Page: 238-240<br />
HAIL DAMAGE OF FOREST TREES IN WESTERN CANADA<br />
ABSTRACT<br />
Yasuyuki HIRATSUKA 1*<br />
1 Northern Forestry Centre, Canadian Forest Service<br />
Edmonton, Alberta CANADA<br />
* yahirats@nrcan.gc.ca<br />
Hail and hail storms damage agricultural and horticultural crops, as well as vehicles,<br />
houses and other buildings; these weather events also cause various degrees <strong>of</strong> damages to<br />
forest trees. Western Canada, with its diverse topography and varied weather systems, is<br />
known to have frequent hail storms. In the Canadian Rockies in the fall <strong>of</strong> 2008, a severe<br />
discoloration <strong>of</strong> foliage and many dead branches were observed over several hectares <strong>of</strong> a<br />
subalpine fir (Abies laciocarpa (Hook.)Nutt.) stand. After examining the symptoms and<br />
topographical features <strong>of</strong> the affected area, it was concluded that the damage was caused by<br />
a hail storm. Hail damage as well as other weather-related damage to forest trees, such as<br />
frost damage and drought damage, are <strong>of</strong>ten predisposing factors <strong>of</strong> branch and foliage<br />
symptoms associated with pathogenic fungi belonging to such genera as Nectria,<br />
Cytospora, and Sphaeropsis, and this weather-related damage should be considered when<br />
diagnosing forest tree health problems.<br />
Keywords: hail damage, western Canada, non-biotic tree diseases, predisposition<br />
1. INTRODUCTION<br />
Hail or hail storms usually occur at the front <strong>of</strong> storm systems from spring to<br />
fall but rarely during cold winter weather. Hail is formed when updrafts in<br />
thunderclouds carry rain drops upward into extremely cold areas <strong>of</strong> the cloud and<br />
form ice particles; updrafts carry the ice particles to the cold region <strong>of</strong> the storm<br />
clouds, where the size <strong>of</strong> the ice particles increases. When the ice particles become<br />
too heavy to be supported by the updraft, they fall to the ground at speeds <strong>of</strong> up to<br />
100 km/h. Hail storms can cause damage to crops, houses, and vehicles as well as<br />
injuries to people and animals. Hail damages to forest trees have <strong>of</strong>ten been<br />
reported (Benjamin, 1957; Grayburn, 1957; Hiratsuka and Zalasky, 1993; Laut and<br />
Elliott, 1966; Nelson, <strong>2009</strong>; Riley, 1953).<br />
Hail storms occur more frequently along mountain ranges because winds<br />
(moving in a horizontal direction) react to the change in topography, shifting<br />
upwards within thunderstorms and creating favorable conditions for the creation <strong>of</strong><br />
hail and hail storms. Hail storms are known to occur throughout many parts <strong>of</strong> the<br />
238