GSTDTAP  > 气候变化
DOI10.1002/2016JD026189
Expanding on the relationship between continuing current and in-cloud leader growth
Lapierre, Jeff L.1,2,3; Sonnenfeld, Richard G.2,3; Stock, Michael4,5; Krehbiel, Paul R.2,3; Edens, Harald E.2,3; Jensen, Daniel2,3
2017-04-27
发表期刊JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
ISSN2169-897X
EISSN2169-8996
出版年2017
卷号122期号:8
文章类型Article
语种英语
国家USA; Japan
英文摘要

When lightning connects to the ground, there is a large surge of current, called the return stroke, which is occasionally followed by a longer-lasting steady current, called continuing current (CC). In a previous study of negative cloud-to-ground (-CG) flashes, we observed the growth rate of in-cloud positive leaders in an attempt to identify occurrences of CC. However, there was no observed change in positive leader growth rate during CC of negative CG flashes. In this study, we use the Langmuir Electric Field Array, Lightning Mapping Array, and Flash-Continuous Broadband Digital Interferometer data to extend the previous study to the growth of the negative leader during positive CG flashes. We have found that in contrast with previous results, negative leader growth during positive CG flashes does show increases in growth rates coincident with CC. Finally, we find that the growth rate magnitudes for positive and negative leaders are typically approximate to 2-4km/10ms and approximate to 25-40km/10ms, respectively. These contrasting results highlight the differences between positive and negative leaders and provide strong evidence as to why -CC and +CC behave differently. Negative leaders inject higher amounts of current and allow the channel to remain conductive throughout the duration of CC. Whereas for positive leaders, the channel becomes nonconductive relatively quickly. It is therefore disconnected from the channel to the ground, and, due to the positive leader's continued growth, an electric potential is built up until a K event is produced that re-ionizes the channel.


Plain Language Summary Cloud-to-ground (CG) discharges are bipolar events consisting of a downward leader to ground fed by an opposite polarity leader within the cloud. For negative CG discharges (-CGs), the downward leader lowers negative charge toward ground, while the associated in-cloud breakdown is positive. The opposite is true of positive CG discharges (+CGs). When the descending leader contacts the ground, ground potential propagates rapidly back up the channel as a high-current return stroke, which can occasionally initiate a long-lasting continuous current (CC). Generally, -CG flashes consist of three to five return strokes, whereas +CG flashes consist of one. In this study, we analyze the growth of negative leaders of +CG flashes during CC to determine whether there is any observable change. We have found that in contrast with -CG flashes, negative leader growth during +CG flashes does show increases in growth rates coincident with CC. Furthermore, we find that negative leaders inject higher amounts of current and allow the channel to remain conductive throughout the duration of CC. Whereas for positive leaders, which inject smaller amounts of current, the channel becomes nonconductive relatively quickly, which leads to multiple return strokes.


英文关键词lightning continuing current physics atmospheric electricity
领域气候变化
收录类别SCI-E
WOS记录号WOS:000401180800002
WOS关键词ELECTRIFICATION ; THUNDERSTORMS ; NORMALITY
WOS类目Meteorology & Atmospheric Sciences
WOS研究方向Meteorology & Atmospheric Sciences
引用统计
被引频次:10[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/33967
专题气候变化
作者单位1.Univ Virginia, Dept Environm Sci, Clark Hall, Charlottesville, VA 22903 USA;
2.New Mexico Inst Min & Technol, Dept Phys, Socorro, NM 87801 USA;
3.New Mexico Inst Min & Technol, Langmuir Lab, Socorro, NM 87801 USA;
4.Rairan Pte Ltd, Osaka, Japan;
5.Osaka Univ, Osaka, Japan
推荐引用方式
GB/T 7714
Lapierre, Jeff L.,Sonnenfeld, Richard G.,Stock, Michael,et al. Expanding on the relationship between continuing current and in-cloud leader growth[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2017,122(8).
APA Lapierre, Jeff L.,Sonnenfeld, Richard G.,Stock, Michael,Krehbiel, Paul R.,Edens, Harald E.,&Jensen, Daniel.(2017).Expanding on the relationship between continuing current and in-cloud leader growth.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,122(8).
MLA Lapierre, Jeff L.,et al."Expanding on the relationship between continuing current and in-cloud leader growth".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 122.8(2017).
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