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).
Based on the team's analyses, they estimate that the 10 - fold - or - more magnification
of airglow occurs somewhere on Earth on 7 % of nights, with observers at any one spot able to see a bright night only once per year — and only then if conditions are just right.
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.
Not exact matches
Trapped beneath Earth's ocean
of air, ground - based observatories will be stymied by starlight - warping turbulence, and by
airglow — faint light emitted by atmospheric chemical reactions that can corrupt delicate observations.
Trapped below Earth's ocean
of air, even the largest ground - based observatories will be stymied by starlight - warping turbulence and by
airglow, faint light emitted by atmospheric chemical reactions that can corrupt delicate observations.
Processes in the ionosphere also create bright swaths
of color in the sky, known as
airglow.
Still, at altitudes above roughly 80 kilometers (50 miles) lunar tides have been detected in winds, temperature,
airglow emissions and a number
of ionospheric parameters.
Two upcoming NASA missions will study
airglow and other properties
of the ionosphere.
Analyzing measurements
of high - altitude
airglow gathered by a satellite in 1992 and 1996 (years
of maximum and minimum solar flare activity, respectively), the scientists found 11 cases where
airglow, in theory, brightened enough to be seen by observers on the ground, they report in Geophysical Research Letters.
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 ground.
This enormous reservoir
of charged particles plays a still - unexplained role as middleman in the interaction
of Earth and sun which is reflected in magnetic storms, in the
airglow and in the beautiful displays
of the aurora.
As evidenced in previous sections,
airglow is a manifestation
of planetary space weather.
A similar scheme applies to the NO
airglow UV emission, ultimately generated after the UV dissociation
of CO2 and N2 at the dayside (Stiepen et al. 2013).
In his early stage
of research, he was involved in the field
of the earth's upper atmosphere like observations
of terrestrial
airglow and aurora, as well as the ozone layer.
I'm open for new ideas and do not write off the idea
of electrical phenomena playing a role in climate — hence a discussion on the subject together with various curiosities such as Aurora, Elves,
airglow, Sprites, the Van Allen belts, and Lightening in my book «Solar Activity and Earth's Climate» (2002; Praxis / Springer).