interesting. The propagation is probably by
daytime D-layer reflection, which typically exhibits a flat maximum at
noon time. This is conspicuouis eg. on the DCF / HGA plots from 4X and
YO, and on Eu Loran-C signals as well. On the sea path between G and
TF, this may be augmented by a groundwave component with relatively
little attenuation.
BTW Stefan's strong DFCW signal is producing
an unusual modulation effect on Halldór's grabber, as both the
background noise and all other signals seem to brighten up during the
dashes. Just like a kind of negative AGC...
Best 73,
Markus (DF6NM)
Sent: Sunday, November 20, 2011 5:41 PM
Subject: LF: TF3HZ