Physics
Scientific paper
Sep 2011
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011jgra..11609313b&link_type=abstract
Journal of Geophysical Research, Volume 116, Issue A9, CiteID A09313
Physics
Atmospheric Processes: Atmospheric Electricity, Atmospheric Processes: Theoretical Modeling (4316)
Scientific paper
We demonstrate that positive cloud-to-ground lightning flash (most often responsible for sprites) from stratiform tropospheric thundercloud leading to charge moment change iΔMq high above the sprite “threshold” 500 C km really triggers the high-altitude discharge exciting the air luminescence at sprite altitudes with brightness close to the observed brightness. Specifically, we present results for three configurations with the same charges Qcl = 200 C located at altitudes 6 and 8 km (iΔMq = 1200 C km for +Qcl at 6 km and iΔMq = 1600 C km for +Qcl at 8 km) differing by a magnitude of charge density, namely, σ = 1.86, 2.88, and 4.41 C km-2. All three configurations produce luminescence at sprite altitudes with brightness close to the observed one. In addition, the configuration with σ = 2.88 C km-2 produces observable γ emission, which can be detected in near space as terrestrial gamma-ray flashes (TGFs). The configuration with σ = 4.41 C km-2, provided it really could develop, would produce a blue fluorescence directly near the cloud top and extremely intensive γ emission not observed till now. The results obtained for smaller σ prove that too small-charge density in stratiform thunderclouds and consequently too weak electric field above them could account for the lack of Reuven Ramaty High Energy Solar Spectroscopic Imager TGFs correlated with large-charge moment change.
Babich Leonid
Haldoupis Christos
Kudryavtsev Andrei
Kutsyk Igor
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