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European Pirates and Private Stations / UNID 6270 AM 0945 UTC 23 December 2018
« on: December 23, 2018, 0959 UTC »
Close down show of Sunshine 101 in Dublin.
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This is something that I could never figure out when looking at those reports. The MUFs listed at the bottom for 100, 200, 400 km are usually > foF2.
The lunar far side always faces away from Earth, so it's is free from interference from our planet's ionosphere, human-made radio frequencies and auroral radiation noise. Solar radio emission is also blocked during the lunar night.
You can see the effect of fxI in the suggested MUFs for 100, 200, 400 km distances (typical of NVIS), displayed in text at the bottom of most of the Lowell Digisonde ionograms.
You will notice that the furthest right hand green fish hook scattering (fxI frequency) often tends to correspond with the 100 km or 200 km MUF in the Lowell Digisonde ionogram text.
The maps are based on a melding of ionosonde data from various geographically separated ionosonde sources.
The map algorithms average the differential between the ionosonde curves and that forms contours.
Also, there's the "Spread F index, or fxI, upon which the MUFs are calculated, and may be utilized for map source data.
The best NVIS propagation frequency usually happens between the foF2 and the fxI.
The maps show different things.
One is the Critical F2.
The other is the foF2.
The following image is a recent high-resolution global map of F2-layer critical frequencies. This corresponds to the maximum radio frequency that can be reflected by the F2-region of the ionosphere at vertical incidence (that is, when the signal is transmitted straight up into the ionosphere). ...
This map can be used to determine the frequencies that will always be returned to the Earth. Transmitted frequencies higher than the indicated contours (which are given in MHz) may penetrate the ionosphere, resulting in lost power to space. Frequencies lower than the indicated contours will never penetrate the ionosphere. Lower foF2 values indicate a weaker ionosphere and correspond to regions with lower Maximum Usable Frequencies (MUFs). Higher foF2 values indicate a stronger ionosphere and correspond to regions with higher MUFs.