收藏设为首页 广告服务联系我们在线留言

干旱区地理 ›› 2022, Vol. 45 ›› Issue (3): 746-753.doi: 10.12118/j.issn.1000-6060.2021.284

• 气候变化 • 上一篇    下一篇

高原复杂地理参数对雷电活动的影响分析

胡亚男1(),陶世银1(),龚梅竹2,马海玲1   

  1. 1.青海省气候中心,青海 西宁 810000
    2.青海省气象服务中心,青海 西宁 810000
  • 收稿日期:2021-06-22 修回日期:2021-08-17 出版日期:2022-05-25 发布日期:2022-05-31
  • 通讯作者: 陶世银
  • 作者简介:胡亚男(1992-),女,博士研究生,主要从事遥感在气候变化的应用研究. E-mail: iiophuhu@163.com
  • 基金资助:
    青海省应用基础研究(2019-ZJ-7098)

Influence analysis of geographic parameters on lightning in plateau

HU Yanan1(),TAO Shiyin1(),GONG Meizhu2,MA Hailing1   

  1. 1. Qinghai Climate Center, Xining 810000, Qinghai, China
    2. Qinghai Meteorological Service Center, Xining 810000, Qinghai, China
  • Received:2021-06-22 Revised:2021-08-17 Online:2022-05-25 Published:2022-05-31
  • Contact: Shiyin TAO

摘要:

雷电活动参数作为反映区域雷电活动特征的重要指标,地形对其影响不容忽视。利用2014—2018年青海省地闪数据、数字地形高程数据以及HWSD土壤数据集,定量分析海拔、坡度、坡向以及土壤电阻率对青海省地闪分布特征的影响。结果表明:(1) 青海省地闪主要集中在海拔3150~4850 m、坡度0~35°的地区,其中东北坡向地闪次数最多,东南坡向地闪次数最少,地闪对应的土壤电阻率主要集中于100 Ω·m。(2) 地闪密度随海拔的升高先增大后减小,随坡度的增大而减小;地闪平均强度随海拔的升高先减小后增大,随坡度的增大而增大。(3) 选取92°27′00″~97°44′24″E、31°40′48″~34°16′48″N地闪活跃区域,对其1 km×1 km网格内地闪数据与地理参量平均值进行相关性分析,所选区域内地闪密度与平均海拔呈正相关关系,与平均坡度呈负相关关系;而地闪强度与平均海拔呈负相关关系,与平均坡度呈正相关关系。

关键词: 雷电活动, 海拔, 坡度, 坡向, 土壤电阻率, 青海高原

Abstract:

The influence of terrain on lightning current parameters cannot be ignored as a basis for lightning theory study and engineering protection application. Thus, in this study, the impacts of altitude, slope, aspect, and soil conductivity on the characteristics of cloud-to-ground lightning distribution in Qinghai Province, China, were quantitatively analyzed using cloud-to-ground lightning data from 2014 to 2018, digital terrain altitude data, and the HWSD data set. As per the data, it was determined that (1) cloud-to-ground lightning mostly concentrated at the altitude of 3150-4850 m and a slope of 0-35°. The number of slope to the northeast had the greatest cloud-to-ground lightning, whereas the one to the southeast had the least. The electrical conductivity corresponding to cloud-to-ground lightning is primarily concentrated at a distance of 100 Ω·m. (2) For a given unit area, the cloud-to-ground lightning frequency increased first and then decreased with altitude. The number of cloud-to-ground lightning strikes increases slowly as the slope increases. In addition, the average cloud-to-ground lightning intensity decreases first and then increases as altitude increases. It showed a trend of gradual increase as the slope increased and an increasing trend as the conductivity increased. (3) A correlation analysis was performed between the cloud-to-ground lightning data and the mean value of the geographical parameters in a 1 km×1 km grid covering the active areas of 92°27′00′′-97°44′24′′E and 31°40′48′′-34°16′48′′N. The cloud-to-ground lightning density in the selected areas was positively correlated with altitude and negatively correlated with the slope. A negative correlation was noted between cloud-to-ground lightning intensity and mean altitude, but a positive correlation with slope.

Key words: lightning activity, altitude, slope, slope direction, soil conductivity, Qinghai Plateau