This Northern Light's
Phenomenon is produced by charged electrons and protons striking gas particles
in the earth's upper atmosphere. These electrons and protons are
released through sunspot activity from the sun. It takes one to two
days for them to reach earth's atmosphere, where they are pulled to the
north and south poles by earth's magnetic forces.
The color varies, depending how
hard the gas particles are being struck. Auroras can range from simple
arcs to drapery like forms in green (the most common), red, blue, and purple.
The lights occur in a pattern rather than a solid glow, because electric
current sheets flowing through the gases create a V shaped potential double
layers.
These beautiful displays take
place as low as 40 to 68 miles above the earth's surface and extend hundreds
of miles into space. The lights concentrate in two bands centered
above the Arctic Circle and Antarctic Circle, and are about 2,500 miles
in diameter. The southern lights are known as the Aurora Australis.
In the northern latitudes the greatest occurrence of aurora displays is
in the spring or fall months, owing to the tilt of the earth to the sun.
The first 1982 published photographs of the northern lights in their entirety
were taken from satellite cameras and had the appearance of a nearly perfect
circle. |