In 1932, Baird was the first person in Britain to demonstrate ultra-short wave transmission.

The long wave transmission can also be heard in much of Europe during day and night, including parts of Great Britain.

Beneath the Eromanga basin in the mantle below 200 km is a region of fast seismic wave transmission.

The energy transmission from an impulse break derives not from mass displacement, but from wave transmission.

During this period he had the idea of position fixing by means of phase comparison of continuous wave transmissions.

The lead-lined walls were intercepting the wave transmissions, thought Pirx.

Similarly, people listening to short wave transmissions are SWLing.

To limit access to foreign broadcasts, the Central Committee decreed that factories take out components allowing short wave transmission.

However, consumers easily found the necessary spare parts on the black market and veterans fixed radios to receive short wave transmission.

In December 1953, short wave transmissions started at Wiederau.