首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Determination of the Global-Average Charge Moment of a Lightning Flash Using Schumann Resonances and the LIS/OTD Lightning Data
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Determination of the Global-Average Charge Moment of a Lightning Flash Using Schumann Resonances and the LIS/OTD Lightning Data

机译:使用舒曼共振和LIS / OTD闪电数据确定闪电闪光的全局平均电荷时刻

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In this paper, we use (1) the 20 year record of Schumann resonance (SR) signals measured at West Greenwich Rhode Island, USA, (2) the 19 year Lightning Imaging Sensor (LIS)/Optical Transient Detector (OTD) lightning data, and (3) the normal mode equations for a uniform cavity model to quantify the relationship between the observed Schumann resonance modal intensity and the global-average vertical charge moment change M (C km) per lightning flash. This work, by integrating SR measurements with satellite-based optical measurements of global flash rate, accomplishes this quantification for the first time. To do this, we first fit the intensity spectra of the observed SR signals to an eight-mode, three parameter per mode, (symmetric) Lorentzian line shape model. Next, using the LIS/OTD lightning data and the normal mode equations for a uniform cavity model, we computed the expected climatological-daily-average intensity spectra. We then regressed the observed modal intensity values against the expected modal intensity values to find the best fit value of the global-average vertical charge moment change of a lightning flash (M) to be 41 C km per flash with a 99% confidence interval of ±3.9 C km per flash, independent of mode. Mode independence argues that the model adequately captured the modal intensity, the most important fit parameter herein considered. We also tested this relationship for the presence of residual modal intensity at zero lightning flashes per second and found no evidence that modal intensity is significantly different than zero at zero lightning flashes per second, setting an upper limit to the amount of nonlightning contributions to the observed modal intensity.
机译:在本文中,我们使用(1)在西格林威治美国罗德岛,测量舒曼共振(SR)信号的20年纪录(2)年仅19闪电成像传感器(LIS)/光学瞬间探测器(OTD)闪电数据,和(3)的正常模式的均匀腔模型方程以定量观察到的舒曼共振模态强度和每闪电全球均垂直电荷力矩将M(C公里)之间的关系。这项工作,通过整合SR测量与全球闪存率的基于卫星的光学测量,完成这个量化的第一次。要做到这一点,我们首先观察到的SR信号的强度光谱适合每个模式的八模式,三个参数,(对称)洛伦兹线形状模型。接下来,使用LIS / OTD闪电数据和用于均匀空腔模型正常模式方程,我们计算了预期气候每日平均强度光谱。然后,我们回归与预期模态强度值观测到的模态强度值找到一个闪电(M)的全球平均水平垂直电荷的时候,变革的最合适的值,为每闪存41Ç公里,99%的置信区间每个闪存±3.9ç公里,独立的模式。模式独立认为该模型充分地捕获的模态强度,本文考虑的最重要的拟合参数。我们还以每秒零个闪电测试残留的模态强度的存在此关系,并发现,没有证据表明模态强度是在每秒零个闪电大于零显著不同,设定上限,以nonlightning贡献所观察到的量模态强度。

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