马来西亚半岛陆地及海洋上空云对地闪电活动

M.S. Azaman, D. Johari, F. A. Haris, A. F. Abidin, N. H. Nik Ali, N. Hatta
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摘要

本文研究了马来西亚半岛陆地和海洋上空云对地闪电的特征。该研究旨在调查马来西亚半岛的负CG和正CG的特征,特别是在西海岸地区的陆地和海洋以及马六甲海峡上空。利用TNBR的闪电定位系统(LLS)记录的2020年雷电数据,从发生次数、行程密度和峰值电流等方面分析了正、负CG。选择了6个半径为15公里的圆形区域:3个在陆地上,3个在海洋上,每个区域都有不同的特征。我们发现,大部分CG闪电发生在陆地上,而不是海洋上,但两者之间只有2.4%的细微差异。我们还发现,负CG的平均峰值电流在海洋上更高,几何平均值为25.7 kA,而在陆地上,平均值为21.9 kA。对于正CG,我们发现海洋上的平均峰值电流也更高,几何平均值为32.3 kA,而陆地的平均值为28.7 kA。陆地上空CG闪电的高发可能是由于陆地上空发展增加所引起的热效应所致。海洋上空的峰值洋流强度较高可能是由于该地区气溶胶排放量较大和海水电导率较高所致。
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Cloud-to-Ground Lightning Activity over Land and Ocean in Peninsular Malaysia
This paper presents an investigation on the characteristics of cloud-to-ground (CG) lightning over land and ocean in Peninsular Malaysia. The study aims to investigate the characteristics of negative and positive CG in Peninsular Malaysia, particularly over land and ocean on the west coast region and over the Malacca Straits. By analyzing 2020 lightning data recorded by the lightning locating system (LLS) operated by TNB Research (TNBR), we analyzed the negative and positive CG in terms of their occurrences, stroke density, and the peak currents. Six circular regions with a 15 km radius were selected: three (3) over the land and three (3) over the ocean, each having distinct characteristics from the others. We found that most of the CG lightning occurred over land than ocean but there is only a slight difference of 2.4% between the two. We also found that the average peak current for negative CG is higher over the ocean with a geometric mean of 25.7 kA whereas for land, the average value is 21.9 kA. For positive CG, we found that the average peak current is also higher over the ocean with a geometric mean of 32.3 kA whereas for land, the average value is 28.7 kA. The higher occurrence of the CG lightning over land could be due to the heat effect caused by the increase in the development over the land region. The higher intensity of the CG peak currents over the ocean could be due to larger aerosol emission in the area and the higher conductivity of the seawater.
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