Caption: A false-color ultraviolet film of an auroral oval (AKA auroral ring) over the Antarctica. The green false-color was probably chosen to mimic the actual green color of some aurora.
Features:
But the charged particles can move along the magnetic field lines , and so touch down usually in the Earth's atmosphere in the Earth's polar regions in the auroral zone in a pattern called an auroral oval such as in this film.
The air molecules de-excite by emitting light.