inch. In the case of Hertzian wave telegraphy, we are, however, dealing with ether waves many hundreds of feet in length, and the waves sent out from Poldhu have a wave-length of a thousand feet or more, say one fifth to one quarter of a mile. The distance therefore between Poldhu and Cape Cod is only at most about twelve thousand wave-lengths, and stands in the same relation to the length of the Hertzian wave used as does a body the diameter of a pea to the wave-length of yellow light. There is unquestionably a large amount of diffraction or bending of the electric wave round the earth, and proportionately speaking it is larger than in the case of light waves incident on objects of the same relative size.
Quite recently Mr. H. M. Macdonald (see Proc. Roy. Soc. Lond., Vol. LXXI., p. 251) has submitted the problem to calculation, and has shown that the power required to send given electric waves 3,000 miles along a meridian of the earth is greater than would be required to send them over the same distance if the sea surface were flat in the ratio of 10 to 3. Hence the rotundity of the earth does introduce a very important reduction factor, although it does not inhibit the transmission. Mr. Macdonald 's mathematical argument has, however, been criticized by Lord Rayleigh and by M. H. Poincaré (see Proc. Roy. Soc, Vol. 72, p. 40, 1903).
The accomplishment of very long distances by Hertzian wave telegraphy is, however, not merely a question of power, it is also a question of wave-length. Having regard, however, to the possibility that the propagation which takes place in Hertzian wave telegraphy is not that simply of a free wave in space, but the transmission of a semiloop of electric strain with its feet tethered to the earth, it is quite possible that if it were worth while to make the attempt, an ether disturbance could be made in England sufficiently powerful to be felt in New Zealand.
Leaving, however, these hypothetical questions and matters of pure conjecture, we may consider some of the facts which have resulted from Mr. Marconi's long distance experiments. One of the most interesting of these is the effect of daylight upon the wave propagation. In one of his voyages across the Atlantic, when receiving signals from Poldhu on board the S. S. Philadelphia, he noticed that the signals were received by night when they could not be detected by day.[1] In these experiments Mr. Marconi instructed his assistants at Poldhu to send signals at a certain rate from 12 to 1 a. m., from 6 to 7 a. m., from 12 to 1 p. m. and from 6 to 7 p. m., Greenwich mean time, every day for a week. He has stated that on board the Philadelphia he did not
- ↑ See Proc. Roy. Soc, June 12, 1902. 'A note on the Effect of Daylight upon the Propagation of Electromagnetic Impulses Over Long Distances,' by G. Marconi.
