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Earth’s atmosphere is divided into several layers, including the troposphere, stratosphere, mesosphere, thermosphere, and exosphere. Each layer has unique properties and plays a role in weather, climate, and communication. When it comes to long-distance radio communication, the most important layer is the ionosphere.
The ionosphere is a region of the upper atmosphere, roughly between 60 km and 1,000 km above Earth's surface, that is filled with charged particles, or ions. These ions are created when solar radiation from the Sun strikes gas molecules, knocking out electrons and forming electrically charged particles. This process makes the ionosphere capable of reflecting certain types of radio waves back toward Earth.
When a radio signal is transmitted upward, it can hit the ionosphere and bounce back to another location far away from the original source. This allows radio communication over hundreds or even thousands of kilometers, far beyond the line of sight of the transmitter. Without the ionosphere, radio signals would travel straight into space and would not reach distant receivers.Looking at the other options:
Exosphere: The outermost layer where particles are very sparse, not useful for radio wave reflection.
Troposphere: Closest to Earth, where weather occurs, but it does not reflect radio waves effectively.
Stratosphere: Contains the ozone layer but is not responsible for radio communication.
Ozone layer: Protects from harmful UV rays but does not reflect radio waves.
Thus, the correct answer is Ionosphere, as it is the atmospheric layer that enables long-range radio communication by reflecting and refracting radio signals.
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