Upper-atmospheric lightning: Revision history


For any version listed below, click on its date to view it. For more help, see Help:Page history and Help:Edit summary. (cur) = difference from current version, (prev) = difference from preceding version, m = minor edit, → = section edit, ← = automatic edit summary

(newest | oldest) View (newer 500 | ) (20 | 50 | 100 | 250 | 500)

24 April 2024

18 April 2024

14 April 2024

  • curprev 08:0208:02, 14 April 2024Marikillarl talk contribs 31,689 bytes +222 The main contributors related to the slow decay of the glow were atomic iron and nickel, molecular nitrogen and ionic molecular oxygen. Besides, we found weak traces of atomic oxygen, so this is not the main contributor to the greenish hue color, at least in the reported event. Tags: Visual edit Mobile edit Mobile web edit
(newest | oldest) View (newer 500 | ) (20 | 50 | 100 | 250 | 500)