The meteorology of negative cloud‐to‐ground lightning strokes with large charge moment changes: Implications for negative sprites. Issue 14 (26th July 2013)

• Record Type: Journal Article
• Authors: Lang, Timothy J.; Cummer, Steven A.; Rutledge, Steven A.; Lyons, Walter A.
• Is Part Of: Journal of geophysical research. Volume 118:Issue 14(2013)
• Page Start: 7886
• Page End: 7896
• Publication Date: 2013-07-26
• Subjects: negative sprites -- charge moment change -- negative lightning; Atmospheric physics -- Periodicals; Geophysics -- Periodicals; 551.5
• DOI: 10.1002/jgrd.50595
• Languages: English
• ISSNs: 2169-897X

Abstract

Abstract: [1] 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. Key Points: Negative sprite lightning mainly occurred near intense, deep convection The systems producing these discharges were frequently large Systems producing these discharges mainly produced negative CG lightning