Intracloud Lightning Flashes Can Be Similar in Detail
ORAL
Abstract
The unpredictable shape of the channel from cloud to ground in lightning is well known. However, when we mapped repeated intra-cloud (IC) lightning flashes, we in some cases see a repeatable path over 15 minutes. A storm, on 8/18/2004 near Langmuir Lab in New Mexico, spawned six flashes between 19:52:30 and 20:06:41 UTC exhibiting remarkable similarity. When corrected for winds (i.e., when shown in a coordinate system relative to their air-parcel) all flashes originated within a roughly 1~km radius. We introduce ``lightning nursery'' to describe these fecund regions of atmosphere. The first three of these flashes were the most similar. They formed branching structures roughly 30~km in size in which the branches coincided with each other over substantial lengths to a precision of a kilometer. Several conclusions can be drawn from this. 1) When the pre-flash electric field is sufficiently strong, the distribution of charge in a thunderstorm completely determines the path of the flash, over tens of kilometers. 2) Over a period of a couple of minutes, a storm recharges itself to a very similar configuration. 3) This observation validates the use of lightning mapping techniques to deduce the charge structure of storms not just as layers, but as 3-dimensional forms.
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Authors
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Richard Sonnenfeld
Physics Dept \& Langmuir Lab, New Mexico Tech, New Mexico Institute of Mining and Technology
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William Winn
Physics Dept \& Langmuir Lab, New Mexico Tech
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Gaopeng Lu
ECE Dept, Duke University
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Harald Edens
NMT, Physics Dept \& Langmuir Lab, New Mexico Tech
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Steven Hunyady
Physics Dept \& Langmuir Lab, New Mexico Tech
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Jeff Lapierre
New Mexico Institute of Mining and Technology, Physics Dept \& Langmuir Lab, New Mexico Tech