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References: [ +subject:/^(?:^\s*(re|sv|fwd|fw)[\[\]\d]*[:>-]+\s*)*LF\:\s+RE\:\s+Re\:\s+QRN\s*$/: 2 ]

Total 2 documents matching your query.

1. LF: RE: Re: QRN (score: 1)
Author: [email protected]
Date: Thu, 8 Jul 2010 08:57:05 +0200
<snip at 20kHz Well, I would say that the differences of amplitude of VLF signals between day and night are due the presence or absence of the D layer and that the deep morning and evening dips are
/rsgb_lf_group-archives/html/rsgb_lf_group/2010-07/msg00131.html (9,375 bytes)

2. LF: Re: Re: QRN (score: 1)
Author: "Alan Melia" <[email protected]>
Date: Thu, 8 Jul 2010 16:49:59 +0100
Hi Dave that may be it he talks in it about bubbles formed over mountains ....due to updraughts??shadowing on the western side??.... doing tests on a 55kHz signal from Dixon Ca. I seem to remember. T
/rsgb_lf_group-archives/html/rsgb_lf_group/2010-07/msg00386.html (12,632 bytes)


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