Джордж Хэдли: Англиялық заңгер және ауа-райы зерттеушісі

English lawyer and amateur meteorologist

George Hadley (12 February 1685 – 28 June 1768) was an English lawyer and amateur meteorologist who proposed the atmospheric mechanism by which the trade winds are sustained, which is now named in his honour as Hadley circulation. As a key factor in ensuring that European sailing vessels reached North American shores, understanding the trade winds was becoming a matter of great importance at the time. Hadley was intrigued by the fact that winds which should by all rights have blown straight north had a pronounced westerly flow, and it was this mystery he set out to solve.

Hadley was born in London, England to George Hadley (High Sheriff of Hertfordshire) and Katherine FitzJames. He had an unremarkable childhood, and was eclipsed in his early years by his older brother John Hadley (1682–1744), the inventor of the octant (a precursor to the sextant). With John and his other brother Henry, George had constructed effective Newtonian telescopes. George Hadley entered Pembroke College, Oxford, on 30 May 1700, and on 13 August 1701 became a member of Lincoln's Inn, where his father purchased chambers for him. He was called to the bar on 1 July 1709, but remained more interested in mechanical and physical studies than in legal work For 7 years, succeeding William Derham, he was in charge of interpreting the meteorological diaries sent to the Royal Society from observers around the world, mainly in Britain and Scandinavia. He tried to correlate the data in the different temperature and pressure scales then in use and attempted to deduce general patterns that emerged over time. He twice published an account of the results in the Philosophical Transactions of the Royal Society. and on 22 May that year published a short paper in the Philosophical Transactions (vol. 39, 1735, 58–62) giving an explanation of the trade winds. In 1686, Edmond Halley had proposed a theory in an attempt to explain the trade winds, a theory which remained the most widely known internationally almost to the beginning of the 19th century. George Hadley's version recognised that the Earth's rotation plays a role in the direction taken by an air mass moving relative to the Earth, an element that had been missing in Halley's proposal.