林业科学 ›› 2024, Vol. 60 ›› Issue (4): 136-146.doi: 10.11707/j.1001-7488.LYKX20230259
李伟克,舒立福,王明玉*(),李威,司莉青,赵凤君,李笑笑,周暖阳
收稿日期:
2023-06-19
出版日期:
2024-04-25
发布日期:
2024-05-23
通讯作者:
王明玉
E-mail:oldchoff@163.com
基金资助:
Weike Li,Lifu Shu,Mingyu Wang*(),Wei Li,Liqing Si,Fengjun Zhao,Xiaoxiao Li,Nuanyang Zhou
Received:
2023-06-19
Online:
2024-04-25
Published:
2024-05-23
Contact:
Mingyu Wang
E-mail:oldchoff@163.com
摘要:
目的: 对比分析黑龙江大兴安岭林区雷击火与人为火发生规律的差异性变化,为研究区针对性的开展火源管理及合理制定火灾防控政策提供科学依据和参考。方法: 基于研究区1966—2021年间发生的森林火灾数据,按火因归类筛选出雷击火和人为火,通过方差分析、线性拟合等方法对比分析雷击火与人为火在不同时间尺度上的发生差异、规律变化及火灾季的变化趋势。结果: 1966—2021年间研究区共发生森林火灾1 887起,其中雷击火932起,人为火503起,占比分别为49.39%和26.66%。雷击火与人为火在发生年份、月份和时段等不同时间尺度上均有显著差异。研究区雷击火数量呈波动增加,而人为火数量呈波动减少的趋势,尤其是1987年之后研究区雷击火数量逐渐高于人为火,但从整体看研究区森林火灾总数变化并不显著。从火灾面积来看,研究区雷击火面积整体呈增加趋势,而人为火和总森林火灾面积呈减少趋势。研究区雷击火集中发生在6、7月份,人为火多发生于4、5月份,且呈现夏季防火期雷击火数量显著增多,但雷击火面积变化并不显著,春季防火期人为火数量和面积显著减少的变化趋势。从发生时段上看,研究区人为火高发时段为10:00—15:00,而雷击火高发期在12:00—17:00。雷击火和人为火在不同时间尺度上的变化差异造成了研究区火灾季节的变动,其中雷击火灾季呈延后扩张的趋势,人为火灾季呈逐渐缩短的趋势,总森林火灾季呈收缩变短的趋势。结论: 受气候变化及防火政策的影响,黑龙江大兴安岭雷击火与人为火之间的发生规律具有明显的差异性,根据不同火灾类型的发生特点和变化趋势,开展针对性的火灾防控工作是有效降低研究区森林火灾风险的必要前提。
中图分类号:
李伟克,舒立福,王明玉,李威,司莉青,赵凤君,李笑笑,周暖阳. 黑龙江大兴安岭林区雷击火与人为火发生规律及变化趋势[J]. 林业科学, 2024, 60(4): 136-146.
Weike Li,Lifu Shu,Mingyu Wang,Wei Li,Liqing Si,Fengjun Zhao,Xiaoxiao Li,Nuanyang Zhou. Occurrence Pattern and Changing Trend of Lightning Induced Fires and Human-caused Fires in Daxing’anling Forest Region of Heilongjiang Province[J]. Scientia Silvae Sinicae, 2024, 60(4): 136-146.
表1
研究区不同时期间森林火灾次数和火灾面积的差异性分析①"
时期 Period | 火灾次数 Number of fires | 火灾面积 Fire area /hm2 | |||||
雷击火 Lightning fire | 人为火 Human-caused fire | 总森林火灾 Total forest fire | 雷击火 Lightning fire | 人为火 Human-caused fire | 总森林火灾 Total forest fire | ||
I (1966—1976) | 6±6b | 12±9a | 32±17a | 1 738±2 351ab | 98 109±267 699a | 221 686±316 205a | |
II (1977—1987) | 12±14ab | 16±9a | 48±24a | 5 086±10 750ab | 49 648±102 798a | 254 555±368 265a | |
III (1988—1998) | 10±9ab | 7±7a | 20±14b | 123±160b | 1 815±4 168ab | 7 286±11 775bc | |
IV (1999—2009) | 25±21a | 10±11a | 38±24a | 25 541±63 611a | 74 061±196 924a | 102 850±204 653ab | |
V (2010—2021) | 29±24a | 1±2b | 30±24a | 952±2 480ab | 569±1 277b | 1 608±3 650c |
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