Aurora Borealis

Auroras are produced by the collision of charged particles from Earth’s magnetosphere, mostly electrons but also protons and heavier particles, with atoms and molecules of Earth’s upper atmosphere (at altitudes above 80 km (50 miles)).

The collisions in the atmosphere electrically excite electrons to take quantum leaps (a mechanism in which the electron’s kinetic energy is converted to visible light); and molecules in the upper atmosphere. The excitation energy can be lost by light emission or collisions. Most auroras are green and red emissions from atomic oxygen. Molecular nitrogen and nitrogen ions produce some low level red (pink) and very high blue/violet auroras. 

Wiki: http://3.ly/ScX

~ by sternbo on August 25, 2009.

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