南京林业大学学报(自然科学版) ›› 2024, Vol. 48 ›› Issue (3): 219-228.doi: 10.12302/j.issn.1000-2006.202206039
李岩松1(), 杨艳蓉1,*(), 张文艺1, 张乐英1, 黄傲1, 张贻荣2
收稿日期:
2022-06-22
修回日期:
2022-11-01
出版日期:
2024-05-30
发布日期:
2024-06-14
通讯作者:
*杨艳蓉(yangyanrong@njfu.edu.cn),教授。
作者简介:
李岩松(liyansonglyj1997@163.com)。
基金资助:
LI Yansong1(), YANG Yanrong1,*(), ZHANG Wenyi1, ZHANG Leying1, HUANG Ao1, ZHANG Yirong2
Received:
2022-06-22
Revised:
2022-11-01
Online:
2024-05-30
Published:
2024-06-14
摘要:
【目的】 西南地区是我国第二大天然林区,该地生态系统脆弱,森林雷击火灾频发。通过遥感、探测资料分析不同地表覆盖类型、不同海拔下垫面的雷电活动特征,探究雷电活动对森林雷击火的影响。【方法】 根据2005—2017年全球闪电定位系统(WWLLN)闪电数据、MCD12Q1土地覆盖数据、SRTM(shuttle radar topography mission)海拔数据以及相应森林雷击火个例,结合Theil-Sen趋势分析、Mann-Kendall趋势检验、相对密度差分析,对我国西南地区雷电活动随下垫面类型、海拔的变化特征及其与森林雷击火的关系进行研究。【结果】 ① 2005—2017年西南地区云地闪频次以每年8.75%的速率增加。四川和云南交界的攀枝花附近区域是最高值核心区。② 海拔500~1 000 m、稀树草原类下垫面年均云地闪频次最多。以相对密度差表征雷电活跃程度,从季节上看,春季最活跃;从昼夜变化尺度上看,昼间最活跃。表现活跃的下垫面集中在海拔0~1 000 m段,以及农用地/自然植被拼接、稀树草原类和城区为主的地表类型。③ 云地闪在不同下垫面均呈增长趋势,其增长面积占比为西南地区的93.48%。其中,海拔3 500 m以上和草地类型下垫面的增长趋势最显著,从海拔和地表类型来看,显著的面积占比均超过80%。④ 年云地闪频次越高,发生森林雷击火的概率越大。海拔0~1 000 m森林雷击火发生与云地闪活动的下垫面特点一致,海拔1 000 m以上雷击火主要受高云地闪频次影响。【结论】 西南地区雷电活动与下垫面的海拔、地表类型关系密切,且这一关系随不同时间尺度而变化。作为森林雷击火的起因,结合下垫面特征分析雷电活动,探究森林雷击火,可以为西南山地天然林保护提供科学支撑。
中图分类号:
李岩松,杨艳蓉,张文艺,等. 西南地区不同下垫面雷电活动特征与森林雷击火的关系[J]. 南京林业大学学报(自然科学版), 2024, 48(3): 219-228.
LI Yansong, YANG Yanrong, ZHANG Wenyi, ZHANG Leying, HUANG Ao, ZHANG Yirong. Relationship between characteristics of lightning activity on different underlying surface and forest lightning fire in southwest China[J].Journal of Nanjing Forestry University (Natural Science Edition), 2024, 48(3): 219-228.DOI: 10.12302/j.issn.1000-2006.202206039.
表1
Seasonal and diurnal Dr of cloud-to-ground lightning at different altitudes in southwest China from 2005 to 2017单位:%"
海拔/m altitude section | 春 spring | 夏 summer | 秋 autumn | 昼 day | 夜 night |
---|---|---|---|---|---|
[0,200) | 38.01* | -37.97 | -45.49 | 32.44* | -35.69 |
[200,500) | 10.64* | 39.14* | -21.54 | 98.10* | -24.72 |
[500,1 000) | 43.05* | 12.99* | -1.65 | 29.18* | 8.48* |
[1 000,3 500) | -22.34 | -9.17 | 16.77* | -25.05 | 4.37* |
≥3 500 | -63.63 | -34.23 | -9.46 | -81.78 | -10.98 |
表2
Seasonal and diurnal Dr of cloud-to-ground lightning at different land cover in southwest China from 2005 to 2017 单位:%"
土地覆盖类型 land cover type | 春 spring | 夏 summer | 秋 autumn | 昼 day | 夜 night |
---|---|---|---|---|---|
森林 forest | -4.57 | -10.62 | 3.91* | -10.84 | -4.11 |
多树型稀树草原 multi-tree savanna | 8.53* | 1.33* | -6.14 | 4.83* | 0.31* |
稀树草原 savanna | 27.05* | 20.93* | 15.67* | 27.18* | 16.57* |
草地 grass | -60.42 | -36.83 | -15.97 | -77.76 | -16.90 |
农用地 agricultural land | -5.49 | 2.38* | 12.24* | -8.07 | 7.66* |
城市和建筑区 urban and built areas | 10.41* | 39.15* | -0.09 | 64.48* | -2.99 |
水体 waters | -30.11 | 21.22* | -6.05 | -28.66 | -2.55 |
农用地/自然植被拼接 agricultural land/natural vegetation mosaic | 33.03* | 31.13* | -6.73 | 85.57* | -5.67 |
表3
西南地区各地表类型云地闪变化趋势"
下垫面类型 underlying surface type | 变化面积占比/% proportion of change area | |||
---|---|---|---|---|
显著增加 significant increase | 不显著 增加 insignificant increase | 不显著 减少 insignificant reduction | ||
按海拔 分类 classification by altitude | [0, 200)m | 7.69 | 84.62 | 7.69 |
[200, 500)m | 8.38 | 65.24 | 26.38 | |
[500, 1 000)m | 35.98 | 57.13 | 6.89 | |
[1 000, 3 500)m | 44.63 | 51.72 | 3.61 | |
≥3 500 m | 85.21* | 14.64 | 0.15 | |
按土地 类型分类 classification by land type | 森林 forest | 57.21* | 37.46 | 5.28 |
多树型稀树草原 multi-tree savanna | 42.21 | 52.03 | 5.76 | |
稀树草原 savanna | 34.49 | 57.97 | 7.55 | |
草地 grass | 80.61* | 18.62 | 0.77 | |
农用地 agricultural land | 28.43 | 62.88 | 8.70 | |
城市和建筑区 urban and built areas | 33.33 | 40.40 | 26.26 | |
水体 waters | 60.00* | 30.00 | 10.00 | |
农用地/自然植被拼接 agricultural land/natural vegetation mosaic | 8.92 | 1.96 | 19.12 |
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