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Aurora is a phenomenon as brightness or luminescence that appears in the night sky, now in polar areas, but may occur in other parts of the world for short periods of time. In the northern hemisphere is known as aurora borealis, and in the southern hemisphere and aurora australis, named
The Northern Lights are visible from September to March, though at times makes its appearance during the
A polar aurora occurs when charged particles (protons and electrons) are guided by the Earth's magnetic field and affect the atmosphere near the poles. When these particles collide with atoms and molecules of oxygen and nitrogen, which are the most abundant components of the air, part of the collision energy to excite those atoms such energy levels (excited state) than when the energy is dissipated deenergized in visible light of various colors.
The colors we see in the aurora depend on the atomic or molecular species that excite solar wind particles and energy level reach those atoms or molecules: i) Oxygen is responsible for two primary colors of the aurora, green / yellow, ii) Nitrogen, at a collision can start some of their outermost electrons produces blue light, iii) while helium molecules are often responsible for the color red / purple lower edge of auroras and the curved outer parts.
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