The Japanese station JA3YBK was received in
The main signal must have arrived directly via the
short-path. The second signal which starts where the red line ends, has most
likely propagated via the long-path. The distance from
The third signal which starts at the end of the green line, is probably the short-path signal with an extra round around the earth. As the earth’s circumference is about 40 000 km, it is delayed by about 40000/300 000 ≈ 133 ms (or rather 138 ms which is the established round-trip time, taking into account an additional 1400 km path length due to reflections between the ground and the ionosphere). As the AGC was on (in Fast mode on my K2), one cannot make amplitude comparisons of the echoes.
On 30 November 2003 the sunspot number reached 116, much higher than the smoothed average for 2003 which was 63.7. But as propagation is only weakly correlated with daily sunspot numbers (see Correlation Between MUF and Solar Flux on C. Luetzelschwab K9LA's excellent propagation site), this only partially explains the unusual propagation. A much more important factor is that Southern Norway and Central Japan were connected by the grayline at the time, that the propagation paths did not pass too close to any of the polar regions, and that the K-index was only 1 so the there wasn't much disturbance near the polar regions anyway. See figure below for grayline at the time (generated by GeoClock).
(A Norwegian language version of this report appeared in Amatørradio in september 2007: Trippelekko fra Japan)
Here is a recording of the Swedish station SM6CNN in contact with me on 29. October 2003, 22:42 UTC on 28.024 MHz. The direct distance is about 275 km. Note the noise-like signal which is typical for signals that have been reflected off the aurora on the higher HF and on VHF frequencies. There was a strong geomagnetic disturbance that day with the K-index at Dombås, Norway reaching a value of 9 which explains the occurrence of aurora reflection.
Here is a recording of JW/DJ3KR on Spitzbergen from 24. August 2007, at about 21:45
UTC. This was only a few minutes after I had contact with him on 7.002 MHz.
Notice the fluttery character of his signal. On this day it wasn’t too
bad and it wasn’t too hard to copy his signal, but on other occasions,
signals that travel over the polar zone may be impossible to copy correctly.
The K-index
at Tromsø, which lies between
Recently, a facility with big enough antenna (300 by 365 m)
and high enough power (3.6 MW) was used to set a new
record for how low in frequency on HF one can get echoes from the moon.
This was also done during the HAARP moonbounce experiment which encouraged radio amateurs to listen on 19 and 20 January
2008. At my location in
Below is the result of analysis of a such a recording. It is shown here with kind permission from T. Hammond, N0SS, in
This gives a distance to the moon of 0.5*2.39*3e5 km ≈ 358,000 km and a velocity component of the moon away from the earth of 0.5*3e8*7/7.407.5e6 ≈ 140 m/s (moon-earth movement + rotation of both the transmitter and the receiver relative to the moon). Press images for larger figures.
See also YouTube video from K7AGE in California on 19 January 2008. The best echoes start at 4:20 in the video, at 9:55 the display changes to amplitude display, and at 13:15 the frequency changes to 7407.5 kHz.
Signals in the 1.8 – 4 MHz range may pass the ionosphere and be ducted in the magnetosphere out to a distance of several earth radii over to the opposite hemisphere where they will be reflected on top of the ionosphere. The round-trip time varies with the latitude of the transmitter, or to be more accurate with the position relative to the magnetic Equator. Typical delay times are 140 - 300 ms. At my location near Oslo, Norway, the expected delay is about 308 ms, but unfortunately I have yet to hear such an echo.
1. The first echo is from a signal which has followed the path in the left-hand figure below out to a distance of about 1.5 times the radius of the earth over to the Southern hemisphere where it has been reflected back. The recording was done by G3PLX on 26. November 2006, at about 21 UTC (also local time), on 1998 kHz. It has a delay of 210-220 ms, consistent with his location in Northern England. The transmitted signal was a chirp using a 100 Watt SSB transmitter with a 50 m longwire antenna. Note the stereo effect as the transmitter and receiver are in the right and left channels respectively. The chirps are exactly 5 sec apart, timed against GPS, so this will enable one to calculate the exact samplerate, which is about 8100Hz. Listen to the signal here (with kind permission from P. Martinez, G3PLX).
2. On 17. February 2006, at 0345 UTC (2245 local time) K4MOG heard his own 3.5 MHz signal coming back to him
after 165-168 ms. He explained this
as the travel time around the earth (138 ms) plus delay in the
transmitter/receiver switching. I would like to offer an alternative
explanation as it is very seldom that signals at this low frequency travel
around the world. At his location in
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Here
is an echo recorded by CB
station 20CB110 in Norway (Radøy 50 km North
of Bergen on the West coast) on frequency 27.025 MHz on 11 May 12.21 UTC. The
main echo is delayed by as much as 7.5 seconds. The FM-signal was emitted from
a 5/8 wavelength vertical antenna with a radial system. Notice the double echo
(easy to hear initially on the word ‘test’). The second delay comes
about 0.45 seconds after the first one. At this time there was sporadic E
propagation to central
Mode conversion is one among the list of the Five Most Likely Explanations for Long Delayed Echoes. The magnetospheric duct echo above corresponds to explanation no 1, and is the mechanism which is best understood.
Norwegian language versions:
©LA3ZA, Sverre Holm
13 Apr 2009.