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Analysis of lightning field changes produced by Florida thunderstorms.

机译:分析佛罗里达雷暴产生的闪电场变化。

摘要

An interactive computer program .has been developed to compute accurate values of lightning-caused changes in the cloud electric field (ΔE). The ΔE' s for individual discharges in eight Florida thunderstorms have been analyzed using a nonlinear, least-squares minimization procedure and point charge (Q) and point dipole (P) models of the change in cloud charge. The results indicate that the temporal and spatial behavior of the Q- and P- model parameters are similar to those reported previously by Koshak and Krider [1989]. In all storms, the high altitude P-vectors tend to point downward toward a narrow altitude band of Q-solutions that is centered at about 8 km; low altitude P-vectors tend to point upward toward the Q-region: and the P-vectors that are at the same altitude as the Q-solutions tend to be horizontal. Because there are inherent limitations in the above least-squares analysis method and models, a new, fundamentally different approach for analyzing lightning field changes has been developed. This method finds an optimum volume charge distribution on a grid of finite dimensions and resolution. with this linear approach, we now have the ability to describe complex field change patterns subject to a variety of external constraints. We also have a framework in which a standard eigenanalysis can be used to access the general information content of data and the effects of measurement errors. Tests of the linear method with simulated lightning sources show that a centroid of the lightning charge distribution can be retrieved to within the grid resolution (2 km) when a Landweber iterative algorithm is used. Tests on three natural lightning events show that there is good agreement with previous Q- and P- model solutions and a resonable result for one event that could not be described with either a Q- or a Pmodel.
机译:已经开发了交互式计算机程序以计算云电场(ΔE)中由雷电引起的变化的准确值。已经使用非线性最小二乘最小化程序以及云电荷变化的点电荷(Q)和点偶极(P)模型分析了八次佛罗里达雷暴中单个放电的ΔE。结果表明,Q和P模型参数的时空行为与Koshak和Krider [1989]先前报道的相似。在所有风暴中,高海拔P向量都倾向于朝着以8 km为中心的Q解的狭窄高度带向下指向;低海拔的P向量趋向于指向Q区域:与Q解处于同一高度的P向量趋向于水平。由于上述最小二乘分析方法和模型存在固有的局限性,因此已经开发出一种新的,根本不同的方法来分析雷电场变化。该方法在有限尺寸和分辨率的网格上找到最佳的体积电荷分布。通过这种线性方法,我们现在能够描述受各种外部约束的复杂场变化模式。我们还有一个框架,可以使用标准特征分析来访问数据的一般信息内容以及测量误差的影响。使用模拟雷电的线性方法的测试表明,当使用Landweber迭代算法时,雷电分布的质心可以恢复到网格分辨率(2 km)之内。对三个自然雷电事件的测试表明,它与以前的Q模型和P模型解决方案有很好的一致性,并且对于一个事件,无论是Q模型还是P模型都无法描述,因此得出了合理的结果。

著录项

  • 作者

    Koshak William John.;

  • 作者单位
  • 年度 1990
  • 总页数
  • 原文格式 PDF
  • 正文语种 en
  • 中图分类

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