Table of Contents
Introduction: Start with Definition
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- Auroras are stunning natural light displays that occur in polar regions.
- Aurora Borealis: Also known as the Northern Lights, visible in the northern hemisphere, primarily near the Arctic Circle. (e.g., Alaska, Norway, Canada).
- Aurora Australis: Also known as the Southern Lights, visible in the southern hemisphere (e.g., Antarctica, parts of Australia, New Zealand).
- Auroras are stunning natural light displays that occur in polar regions.
- Can add recent examples: In Ladakh, an auroral red arc was seen in the Dark Sky Reserve in Hanle.
- Shape
- Auroras constantly change shape and pattern due to the changing magnetic fields and flow of charged particles.
How are Auroras Triggered?
- Solar Wind Interaction: Auroras are caused by the interaction between solar winds (streams of charged particles from the sun) and the Earth’s magnetic field.
- Geomagnetic Storms: When solar winds carry highly charged particles, they disturb the Earth’s magnetosphere, leading to geomagnetic storms.
- Excitation of Atmospheric Particles:Solar wind particles collide with atoms (mostly oxygen and nitrogen) in the Earth’s upper atmosphere (ionosphere), transferring energy and exciting these atoms.
- Light Emission: As excited particles return to their normal state, they release energy in the form of visible light, creating the auroras’ characteristic colorful glow.
- For example, when solar wind particles collide with oxygen, a green colour light is produced. Interaction with nitrogen produces shades of blue and purple.
Conclusion:
Auroras are not just spectacular light shows but are also the result of complex space weather phenomena, revealing the dynamic interaction between Earth and solar activity.
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