From 240 miles above Earth's surface, lightning is visible as bright blotches, and city lights appear as yellow streaks; the atmosphere glows in bands of yellow, green, and red as energetic air molecules interact and emit light, a process (called airglow) that is difficult to see from the gro
From 240 miles above Earth's surface, lightning is visible as bright blotches, and city lights appear as yellow streaks; the atmosphere glows in bands of yellow, green, and red as energetic air molecules interact and emit light, a process (called
airglow) that is difficult to see
from the gro
from the ground.
Fundamental experimental data were derived
from the observations of
airglows by the Spectroscopy for Investigation of Characteristics of the Atmosphere of Mars (SPICAM) instrument on - board Mars Express: while NO is useful to constrain dynamics around the 100 km level (Gagné et al. 2013), CO and CO2 + UV emissions allow the direct monitoring of the efficiency of ionization processes (Stiepen et al. 2015).
There's still some debate though as to whether Steve is a true aurora, or perhaps a form of
airglow, which results
from the upper atmosphere releasing a tiny amount of light as it is warmed by the sun and the Earth's surface.