Definition
The D region is the same as the D-layer of the ionosphere, which is the lowest part of the ionosphere, about 60 to 90 kilometers above the Earth's surface. It primarily absorbs radio waves during the day, affecting long-distance communication. It's created by ionization from solar X-rays and ultraviolet radiation. At night, ionization decreases, and the D region mostly disappears. This disappearance allows radio signals to travel further distances. It is important for understanding how radio waves propagate.