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The meteorology of negative cloud‐to‐ground lightning strokes with large charge moment changes: Implications for negative sprites
Author(s) -
Lang Timothy J.,
Cummer Steven A.,
Rutledge Steven A.,
Lyons Walter A.
Publication year - 2013
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/jgrd.50595
Subject(s) - sprite (computer graphics) , meteorology , mesoscale meteorology , lightning detection , radar , atmospheric sciences , atmospheric electricity , convection , environmental science , precipitation , mesoscale convective system , thunderstorm , geology , physics , electric field , telecommunications , quantum mechanics , computer science , computer vision
Abstract This study examined the meteorological characteristics of precipitation systems that produced 38 “sprite‐class” negative cloud‐to‐ground (CG) strokes (i.e., peak currents in excess of 100 kA and charge moment changes in excess of 800 C km) as well as those that produced three confirmed negative sprites on 23 different days during 2009–2011. Within 15 km of the negative sprite‐parent/class stroke, the median characteristics for these systems were to produce negative CGs as 69.2% of all CGs, and for the 30 dBZ radar reflectivity contour to reach on average 14.2 km above mean sea level (MSL), during a 25 min period encompassing the occurrence of the stroke. The median contiguous area of 30 dBZ composite radar echo (i.e., maximum value in the vertical column) for these systems was 6.73 × 10 3 km 2 . All but three of the discharges occurred in intense multicellular convection, with 30 dBZ exceeding 10 km MSL in altitude, while the others occurred in the stratiform regions of mesoscale convective systems. All but six of the systems produced greater than 50% negative CG lightning, though flash rates tended to be low near the stroke (1–2 min −1 on average). The results suggest that negative sprite‐parent/class lightning typically occurs in precipitation systems of similar size and intensity as those that produce positive sprites, but not necessarily the same systems, and the negative lightning normally strikes ground in the convection rather than the stratiform precipitation. However, upper‐level positive charge in the convection may play an important role in sprite‐class/parent lightning of either polarity.