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By waldo.
On the nineteenth of September in the
year of two-thousand and twelve we saw, for many of us the first
time, the famed, revered, and mythical Aurora Borealis. Glowing in
streaks of green, flowing towards the North. Green because of the
highly charged particles from outer space bombarding the oxygen atoms
in the highest part of our atmosphere, the thermosphere, causing them
to release photons in order to return to a non-excited so called
“ground” state. Should one happen to see red or blue, both are
attributed to the element of nitrogen, the most abundant element on
our atmosphere, the former attributed to the loosing of an electron
and returning to its grounded state, and the latter from gaining an
electron and elevating it to a higher excited energy state. But red
may also be attributed to oxygen as well due to a higher energy level
in the excited atoms, though seeing red form oxygen can be hard to
detect. In the far reaches of this part of our atmosphere oxygen is
the primary element followed by nitrogen and lower elevations thus
one sees auroras in the following orders of colors from most common
to least common, green, pink, red, yellow, and blue. This color
gradient is due to how far down the ionizing energy can reach into
our atmosphere and thus what elements it can ionize.
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