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1 E layer: The next layer beyond the D layer is called the E layer. 2  This exists at an altitude of between 100 and 125 km. 3  Instead of acting chiefly as an attenuator, this layer reflects radio signals although they still undergo some attenuation.
UV-B radiation is uniquely absorbed by the ozone layer. Most of the more energetic solar radiation has been absorbed by other atmospheric constituents before the ozone layer. â¦ The atmosphere stops the classical alpha, beta and gamma radiations. Neutrons decay with time, and are also slowed a bit.