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Spring 2004 Issue |
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The Sporadic-E Files |
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No matter how you look at it, sporadic-E is
the major VHF propagation mode for much of the world. However, while it is
extremely important for hams on 6 and 2 meters and occasionally on 220
MHz, it is probably the most misunderstood mode and the one about which
many myths are circulated. Before we discuss the transport theory of sporadic-E in this initial article, we will provide a simple overview of the basic behavior of the phenomenon as observed by hams on the VHF bands. For the temperate zones of the Earth, sporadic-E has two seasons, a major summer season and a minor winter season. They are separated by significant absence of the phenomenon during the spring and fall equinox. For stations in the northern temperate zone, the summer season starts around May 1st and ends more or less around mid-August. During some parts of June and July, sporadic-E may appear as a daily event, usually lasting for several hours. The winter season is less distinct as far as specific start and end dates, but generally it appears on an occasional basis in late October and lasts through mid-January. It is the major propagation mode for 6 meters during these time periods and also sometimes for 2 meters. The mode makes for lots of fun on these VHF bands during the summer months, as has been documented in CQ VHF over the past several years!
Sporadic-E has been of intense interest to the
scientific community as well as hams. In 1962 Ernest K. Smith and
Matsushita published the book Ionospheric Sporadic-E (Pergamon Press),
which was dedicated entirely to the phenomenon. Dr. Smith had previous
experience with this phenomenon; his doctoral thesis, published during the
late 1950s, was entitled “World Occurrence of Sporadic-E.” Both works
remain a valuable starting point for someone first studying the
phenomenon. However, it is important to realize that much of the data at
that time was collected by ionosondes (or sounding stations) and radio
observations, the best that could be accomplished at the time. Since then
significant data has been collected through the use of rocket probes sent
into the ionosphere, as well as EISCAT radar plots. Figure 1 is an example
of an EISCAT plot. Click here to return to this month's highlights Click here to subscribe to VHF and read more about The Sporadic-E-Files
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