Figure 1-1 Atmospheric Layers

Figure 1.1—Atmospheric layers. since they have the greatest effect on your job. Daily of the ultraviolet energy that initially set them free variations in the ionosphere produce four cloud-like layers of electrically-charged gas atoms called ions, which enable radio waves to be propagated great distances around the earth. Ions are formed by a process called ionization. Ionization In ionization, high-energy ultraviolet light waves from the sun periodically enter the ionosphere, strike neutral gas atoms, and knock one or more electrons free from each atom. When the electrons are knocked free, the atoms become positively charged (positive ions) and remain in space, along with the negatively- charged free electrons. The free electrons absorb some and form an ionized layer. Since the atmosphere is bombarded by ultraviolet waves of differing frequencies, several ionized layers are formed at different altitudes. Ultraviolet waves of higher frequencies penetrate the most, so they produce ionized layers in the lower portion of the ionosphere. Conversely, ultraviolet waves of lower frequencies penetrate the least, so they form layers in the upper regions of the ionosphere. An important factor in determining the density of these ionized layers is the elevation angle of the sun. Since this angle changes frequently, the height and thickness of the ionized layers vary, depending 1-2