The Aurora, often visible on Arctic nights, is a natural light display in the Earth's sky.
Origins
Solar Roots: The phenomenon begins with the Sun, a star of average size among billions in the Milky Way.
Energy Production: Inside the Sun, temperatures exceed 14 million degrees, allowing nuclear reactions where hydrogen atoms fuse into helium, releasing energy.
Convection Cells: This energy moves outward through convection cells, creating electrical currents of charged gas and generating magnetic fields.
Formation of Solar Storms
Magnetic Fields: Strong magnetic fields on the Sun slow down convection, creating sunspots.
Plasma: This electrically charged gas stretches and eventually breaks the magnetic field.
Eruption: Billions of tons of plasma are expelled from the Sun, forming a solar storm traveling at speeds over 8 million km/hr.
Interaction with Earth
Impact on Planets: The solar storm reaches Mercury in 6 hours and Venus in 12 hours before arriving at Earth in 18 hours.
Earth's Magnetic Shield: The Earth's magnetic field acts as a shield, deflecting the storm and creating funnel-like structures.
Daylight and Nighttime Aurora:
Daylight Aurora: Occurs when solar gas streams down on the daylight side of the pole.
Nighttime Aurora: Arises when the magnetic fields on the night side couple, break, and direct the charged gas towards the poles.
The Aurora is a profound display resulting from the interaction between solar storms and the Earth's magnetic shield, offering a dazzling spectacle in the Arctic skies.