The ionosphere is a region in the upper-atmosphere that meets space (exosphere). ![]() Figure 1: Ionosphere (Thermosphere) is part Earth's Atmosphere When solar energy ionizes gases 48 to 800 kilometers above the earth's surface, it produces a mixture of free electrons and ions (known as "plasma"). The high densities of free electrons significantly affect radio communication. Scientists divide the ionosphere into regions, D, E and F:
The largest part of the HF absorption takes place in the D-region, in particular frequencies lower than 10 MHz. The typical (noon time) free electron density ~1010 electrons/m3 at 60-90 km, consists NO+ Nitric Oxide ionized by solar light at 1216Å UVC. What are the differences among ionospheric region D, E, and F? a summary
The ionosphere ↗ is divided into regions, D, E, and F from about 48 up to about 800 km above the earth`s surface, characterized by different free electron densities, and ion compositions.
During the day the F-region splits into two region called F1 and F2, while the D-region vanishes completely at night. These regions do not have sharp boundaries, and the altitudes at which they occur vary during the course of a day and from season to season. What makes the ionospheric regions distinct? See graph of plasma density vs altitude. ![]() Figure 3: Typical Ionospheric electron density profiles The above graph is based on a review from U.C.Berkeley by Bob Brown Ph.D, NM7M (SK)↗
As the ionosphere changes, numerous natural and man made systems are affected:
Read more about the impact of the ionosphere on radio communication.
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