Long delayed echo
Long delayed echoes are radio echoes which return to the sender several seconds after a radio transmission has occurred. Delays of longer than 2.7 seconds are considered LDEs. LDEs are considered anomalous and have a number of proposed scientific origins.
History
These echoes were first observed in 1927 by civil engineer and amateur radio operator Jørgen Hals from his home near Oslo, Norway. Hals had repeatedly observed an unexpected second radio echo with a significant time delay after the primary radio echo ended. Unable to account for this strange phenomenon, he wrote a letter to Norwegian physicist Carl Størmer, explaining the event:At the end of the summer of 1927 I repeatedly heard signals from the Dutch short-wave transmitting station PCJJ at Eindhoven. At the same time as I heard these I also heard echoes. I heard the usual echo which goes round the Earth with an interval of about 1/7 of a second as well as a weaker echo about three seconds after the principal echo had gone. When the principal signal was especially strong, I suppose the amplitude for the last echo three seconds later, lay between 1/10 and 1/20 of the principal signal in strength. From where this echo comes I cannot say for the present, I can only confirm that I really heard it.
Physicist Balthasar van der Pol helped Hals and Stormer investigate the echoes, but due to the sporadic nature of the echo events and variations in time-delay, did not find a suitable explanation.
Long delayed echoes have been heard sporadically from the first observations in 1927 and up to the present day.
Five hypotheses
Shlionskiy lists 15 possible natural explanations in two groups: reflections in outer space, and reflections within the Earth's magnetosphere. Vidmar and Crawford suggest five of them are the most likely. Sverre Holm, professor of signal processing at the University of Oslo details those five; in summary,- Ducting in the Earth's magnetosphere and ionosphere at low HF frequencies. Some similarities with whistlers.
- Travel many times around the world. Signals can travel around the Earth seven times in one second. Such signals are also not uncommon.
- Mode conversion: Signals couple to plasma waves in the upper ionosphere.
- Reflection from distant plasma clouds coming originally from the Sun.
- Non-linearity in addition to mode conversion. Two transmitted signals combine to generate a difference frequency, which travels with a plasma wave, and then it is converted back.
Alternative hypotheses
Still others believe that LDEs are double EME reflections, i.e. the signal is reflected by the Moon and that reflected signal is reflected by the Earth back to the Moon and reflected again by the Moon back to the Earth.
When discussing the use of automated probes as a potential means of contact with extraterrestrial civilizations, American physicist Ronald Bracewell proposed that such probes might try to attract attention by sending back to us our own signals, citing the long delayed echoes as a possible case. This concept was expanded upon by Duncan Lunan, and also addressed by Holm.