AN important application of the science of Meteorology to Aviation is inconnection with the provision of accurate data for navigation This aspect of thesubject involves a knowledge of what may be termed “windstructure,” that is, the horizontal variation of wind with place andtime, and the variation with height within the atmospheric layer in which flyingnormally takes place

In discussing the variation of wind with height it is desirable first to assume astandard of reference The wind near the surface of the ground is of little usein this respect since it is subject to many local variations The most convenientstandard is the undisturbed wind in the lowest layer which is free fromfluctuations caused by the upward propagation of disturbances from the surfaceof the earth

THE CHAIRMAN Ladies and Gentlemen, before calling on Dr Thurston to read hispaper, I will read a few letters that I have received from persons connectedwith aeronautics, expressing regret at not being able to attend here thisevening

(Letters were read from Colonel Moore-Brabazon, Mr Hart Sanders, Mr Richards, MrMelville Jones, General Brooke-Popham, General Cadman Vickers, Captain deHavilland, Mr Chadwick, Mr Bruce and Captain F M Green )

Now, Ladies and Gentlemen, as Dr Thurston is so well known in the Aeronauticalworld it is hardly necessary to say anything by way of introduction, but onlyask him to read his paper