Quote:
Originally Posted by reedeb
I asked a ham friend and THIS is his explanation.
Skip is the bending of signals when they interact with various charged particle layers that surround the earth.
Lift is the bouncing of signals between low (relatively speaking) layers of charged particules.
This condition frequently occurs along the edge of electrically active storms. The signal bounces between the
Layers, exiting hundreds of miles from its enterence point. Also called conduiting.
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I believe the proper term is ducting. It is very common on the low band channels and to some extent on the VHF band. on rare occasions, you might even see this happen on the lower UHF frequencies.
When I was living in New England, I could almost pick the occasions by just watching the storm fronts on the national weather charts. It was not uncommon for a large storm to be about mid way between the Gulf Coast and Canada to cause the ducting to occur. Depending on the speed of the storm it would last from just a few minutes to several hours in length. Stations along the Gulf would be able to talk with the stations in Canada. As the storms go closer to New England, the points of the two ends of the ducting would change. The New England stations might be able to talk with Texas and then as the storm moved to the north east, that other end point would shift more to the north and east on the distant end and then you would be able to talk with Arkansas, then Kentucky and maybe Tennessee. It would fade out after a while because the storm front would get to close to provide the right end points.
The stronger the storm front, the better the ducting would be.