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Winter 2003 Issue |
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50-MHz F2 Propagation Mechanisms Part 1 |
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![]() Figure 1. A typical plot of the daytime electron density as a function of height above the ground, showing the C, D, E, F1, and F2 layers. |
This seminal work on 50-MHz F2 propagation is reprinted by permission from the Proceedings of the 34th Conference of the Central States VHF Society, July 2000. By Jim Kennedy,* KH6/K6MIO |
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The possibility of worldwide F-layer
propagation is a particularly intriguing part of the challenge of 6-meter
operation. Even the casual 6-meter operator will soon notice that there
are some fairly mysterious things going on when it comes to ionospheric
propagation. The more seasoned operator will notice that there are a
number of prevalent patterns, but it is still very difficult to predict
when the band will open, especially on a day-to-day basis. Unfortunately,
there are no simple answers to this dilemma. Nevertheless, there are some
pieces to the F2 puzzle that are known and understood, and some clues to
those that remain mysterious. In order to understand (however imperfectly)
when the band will open, it is essential to have some understanding of why
the band will open.
These factors play key roles in the success or
failure of a communications path via either E or F layers. Although there
are many external things which influence the status of the three
conditions, in the end, it is the combination of these three that make or
break any path. The way in which external events affect these three
parameters determines what kind of propagation will occur. The task of predicting band openings generally involves predicting not just one event, but the coincidence of several events, and not always the same ones or in the same combinations. In truth, we do not yet know what all the factors are, much less how they interact. On the other hand, there are a number of things that are known to be significant, and most of them involve the Sun in one way or another. The Ionosphere and the Sun The Earth’s atmosphere extends from the surface to heights well in excess of 1000 km (or 620 miles). The density of the static atmosphere is highest near the surface and decreases progressively as one goes upwards. Most of the atmospheric mass is located very near the Earth’s surface, with more than half the mass contained within just the first 6 km (or 4 miles).
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