Volume 23, Issue 16 p. 2153-2156

Blue starters∷ Brief upward discharges from an intense Arkansas thunderstorm

E. M. Wescott

E. M. Wescott

Geophysical Institute, University of Alaska, Fairbanks, AK

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D. D. Sentman

D. D. Sentman

Geophysical Institute, University of Alaska, Fairbanks, AK

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M. J. Heavner

M. J. Heavner

Geophysical Institute, University of Alaska, Fairbanks, AK

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D. L. Hampton

D. L. Hampton

NASA Marshall Space Flight Center, Huntsville, AL

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D. L. Osborne

D. L. Osborne

Geophysical Institute, University of Alaska, Fairbanks, AK

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O. H. Vaughan Jr.

O. H. Vaughan Jr.

NASA Marshall Space Flight Center, Huntsville, AL

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First published: 01 August 1996
Citations: 86

Abstract

This paper documents the first observations of a new stratospheric electrical phenomenon associated with thunderstorms. On the night of 30 June (UT 1 July) 1994, 30 examples of these events, which we have called “blue starters,” were observed in a 6 m 44 s interval above the very energetic Arkansas thunderstorm where blue jets were first observed. The blue starters are distinguished from blue jets by a much lower terminal altitude. They are bright and blue in color, and protrude upward from the cloud top (17–18 km) to a maximum 25.5 km (83,655 ft.) in altitude. All blue starters events were recorded from two small areas near Texarkana, Texas/Arkansas where hail 7.0 cm in diameter was falling. Comparison to cloud-to-ground (CG) lightning flashes revealed: 1. Blue starters were not observed to be coincident with either positive or negative CG flashes, but they do occur in the same general area as negative CG flashes; 2. Cumulative distributions of the negative CG flashes in ±5 s before and after the starter and within a radius of 50 km shows a significant reduction for about 3 s following the event in the two cells where starters and jets were observed. The energy deficit is approximately 109 J. It is possible that blue starters are a short-lived streamer phenomenon.