During this same period, Edward Appleton of King's College, Cambridge was carrying out experiments that would lead to him winning the Nobel Prize in Physics. Using a BBC transmitter set up in 1923 in Bournemouth and listening for its signal with a receiver at Oxford University, he was able to use changes in wavelength to measure the distance to a reflective layer in the atmosphere then known as the Heaviside layer. After the initial experiments at Oxford, an NPL transmitter at Teddington was used as a source, received by Appleton in an out-station of King's College in the East End of London.