I believe most of us know about the ionosphere, and skywave propagation, but I'm kind of tripping up on the D-layer. If the ionospheric D-layer absorbs HF signals (40 meters, for example) during the day, how does my signal at night reach another station in, say, Australia, who's in daylight? Shouldn't the signal be absorbed by the D-layer before it reaches him? And if it is, how is it that HF signals can go long-path or reach the other side of the globe?

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    $\begingroup$ i have heard RTW signals a few times, the first was in 1987 on 10Mhz with WWV, with a 0.7second delayed echo (RTW signal delays are about 0.7 seconds), and then a few years ago while listening to Gander Radio on 8891khz, the echoes were multiple echoes, and the signals were stronger than the direct path, and again, the delays were 0.7s. this happened just about every night for a week, and it always coincided with passage of the grey line over their location. haven't heard it since. i guess solar conditions not quite right for it now. $\endgroup$ Commented Dec 23, 2017 at 1:49

2 Answers 2


The D region does not affect all HF (3 MHz to 30 MHz) in the same way. For low frequencies, 2 to 4 MHz, the D region absorbs most signals during the sunlight times of the day. However, somewhere around the 3.5 to 4.5 MHz zone, the absorption starts to fall off as frequency is increased and these signals will penetrate the D region and reach the E region where they are reflected back to Earth.

As the frequency of signals increases more, reaching 10 MHz and beyond, the attenuation caused by the D region falls significantly and signal strengths improve. Also, signals will penetrate further into and thru the E region reaching the F1 region as frequency increases more and again such signals are reflected back to Earth.

So, attenuation of signals (absorption by D-region) affects those signals of the 160 and 80 meter band mostly with some lesser attenuation taking place at 40 meter band at some times but usually this is not nearly as strong as the lower frequencies. Above the 40 meter band, essentially no attenuation by the D-layer.


There is also gray-line propagation, where signals can travel around the world at the circular dusk/dawn annulus. In that region, it is neither totally dark nor totally light.

Long-Path QSOs are usually made following the path of this grayline (shown below). However, QSOs via the shortest path is more common than long-path (which has greater attenuation). Hams have worked DX for over 100 years using this...

  • In the period before, during, and after Sunset
  • In the period before, during, and after Sunrise

It is not unusual to hear the same station with an echo on it. That's usually caused by receiving the short path signal first, followed by the delayed long-path signal.

Grayline region

  • $\begingroup$ There are even "double-echos" (which I have heard). In that case, the signal has arrived over three paths, all of varying length. $\endgroup$ Commented Dec 7, 2017 at 20:08

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