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Journal ArticleDOI

A review of positive and bipolar lightning discharges

Vladimir A. Rakov
- 01 Jun 2003 - 
- Vol. 84, Iss: 6, pp 767-776
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TLDR
In this article, the characteristics of positive and bipolar lightning discharges are reviewed and five situations that appear to be conducive to the more frequent occurrence of positive lightning are discussed, including dissipating stage of an individual thunderstorm, winter thunderstorms, trailing stratiform regions of mesoscale convective systems, some severe storms, and 5) thunderclouds formed over forest fires or contaminated by smoke.
Abstract
Characteristics of lightning discharges that transport either positive charge or both positive and negative charges to the ground are reviewed. These are termed positive and bipolar lightning discharges, respectively. Different types of positive and bipolar lightning are discussed. Although positive lightning discharges account for 10% or less of global cloud-to-ground lightning activity, there are five situations that appear to be conducive to the more frequent occurrence of positive lightning. These situations include 1) the dissipating stage of an individual thunderstorm, 2) winter thunderstorms, 3) trailing stratiform regions of mesoscale convective systems, 4) some severe storms, and 5) thunderclouds formed over forest fires or contaminated by smoke. The highest directly measured lightning currents (near 300 kA) and the largest charge transfers (hundreds of coulombs or more) are thought to be associated with positive lightning. Two types of impulsive positive current waveforms have been obse...

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Citations
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Cloud-to-ground lightning in Austria : a 10-year study using data from a lightning location system

TL;DR: In this paper, the authors presented lightning statistics for more than three million cloud-to-ground (CG) flashes located during the 10-year operation period 1992-2001 of the Austrian lightning location system (LLS) called ALDIS (Austrian Lightning Detection and Information System).
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A ground level gamma-ray burst observed in association with rocket-triggered lightning

TL;DR: In this paper, the authors reported an unusual event that occurred during the last rocket-triggered flash of the 2003 season for this flash, an intense burst of MeV gamma-rays was observed from a distance of 650 m from the lightning channel, not in association with the dart leader or return stroke, but in combination with a large current pulse (11 kA) occurring during the initial-stage (during the initial continuous current), about 20 ms after the vaporization of the triggering wire.
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Photonuclear reactions triggered by lightning discharge

TL;DR: Ground-based observations of neutron and positron signals after lightning provide conclusive evidence of positrons being produced after the lightning, and the centre energy of the prolonged line emission corresponds to electron–positron annihilation.
Journal ArticleDOI

Characteristics of cloud-to-ground lightning in warm-season thunderstorms in the Central Great Plains

TL;DR: In this article, a field campaign was conducted in the Central Great Plains to obtain 60-field/s video imagery of lightning in correlation with reports from the U.S. National Lightning Detection Network and broadband electric field waveforms from the Los Alamos Sferic Array.
Journal ArticleDOI

Positive lightning: An overview, new observations, and inferences

TL;DR: The U.S. National Lightning Detection Network (NLDN) located 51 (96%) of the positive strokes at distances of 7.8 to 157 km from the field-measuring station as mentioned in this paper.
References
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Journal ArticleDOI

A Combined TOA/MDF Technology Upgrade of the U.S. National Lightning Detection Network

TL;DR: The U.S. National Lightning Detection Network (NLDN) has provided real-time and historical lightning data to the electric utility industry, the National Weather Service, and other government and commercial users.
Journal ArticleDOI

The electrical structure of the Hokuriku winter thunderstorms

TL;DR: In this paper, a strong correlation exists between the fraction of positive ground strokes and the vertical wind shear in the cloud layer, which helps to ensure that an initiating positive streamer will continue down to ground rather than into the negatively charged region that would normally be located directly below it.
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