Summer convection and lightning over the Mackenzie River basin and their impacts during 1994 and 1995

被引:20
作者
Kochtubajda, B [1 ]
Stewart, RE
Gyakum, JR
Flannigan, MD
机构
[1] Meteorol Serv Canada, Prairie & No Reg, Edmonton, AB, Canada
[2] Meteorol Serv Canada, Climate Res Branch, Downsview, ON, Canada
[3] McGill Univ, Dept Atmospher & Oceanog Sci, Montreal, PQ, Canada
[4] Canadian Forestry Serv, No Forestry Ctr, Edmonton, AB, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
D O I
10.3137/ao.400208
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Lightning activity over the Mackenzie basin has been examined for the summers of 1994 and 1995. In recent years, the lightning network operating in the Northwest Territories has detected an average of 118 K strikes per season. Positive lightning strikes (defined as lightning discharges lowering positive charge to the earth) typically comprise 12% of the total. The lightning activity during 1994 was approximately 20% below normal, while in 1995, it was 53% below normal. However, the fraction of positive lightning strikes was 25.6% during 1995. The lightning was linked to synoptic conditions favouring severe storm development, especially those tied to the diurnal cycle. As a consequence of the lightning, as well as the very dry surface conditions, record forest areas were burned. In the Northwest Territories alone, forest fires burned 3 Mha in 1994 and 2.8 Mha in 1995.
引用
收藏
页码:199 / 220
页数:22
相关论文
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