''The perspective appearance of thingsto him was very remarkable. The lowestbed of vapour that first appeared ascloud was pure white. in detachedfleeces, increasing as they rose; they presentlycoalesced, and formed, as he expressesit, a sea of cotton, tufting hereand there by the action of the air in theundisturbed part of the clouds. Thewhole became an extended white floor ofcloud, the upper surface being smoothand even. Above this white floor he observed.at great and unequal distances, avast assemblage of thunder-clouds. eachparcel consisting of whole acres in thedensest form: he compares their formand appearance to the smoke of piecesof ordnance, which had consolidated asit were into masses of snow, and penetratedthrough the upper surface ofwhite floor of the common clouds. thereremaining visible and at rest. Someclouds had motions in slow and variousdirections forming an appearance trulystupendous and majestic."Later in the account:-"In the course of the balloon's tract itwas much affected by the water (a circumstanceobserved in former aerialvoyages). At one time the direction ofthe balloon kept continually over thewater, going directly towards the sea, somuch so all to endanger the aeronaut:the mouth of the balloon was openedand he in two minutes descended into anunder-current blowing from the sea."DUST DEVIL ON SEA-BREEZE FRONTWHEN a "very well-developed" dustwhirl tracked across ldris Airport,<strong>16</strong> miles south 01 Tripoli. on 31st May,1964, its centre moved directly over thecontrol tower and meteorological officearea, breaking a window, throwing radioequipment off a table. and making "anoise like a small explosion".The dust whirl was estimated to bemoving at about 10 kts.; its base wasabout SO yards in diameter and its top,estimated to be at about 2,000 ft., hada diameter of about 2S0 yards. It hadcome across mainly cultivated land sodid not contain much dust. but a largenumber of pieces of paper and vegetationwere "circling cyclonically at allheights". As it passed., the met. officebarograph showed an instantaneous falland rise of 35 mb.This was the only dust whirl seen thatday. As it passed, the north to northeastsea breeze penetrated to Idris, itsspeed being 10 kt. initially, increasinglater to 15 kt.J. B. McGinnigle, who describes theevent in the Meteorological Magazinefor Oct., 1964 (Vol. 93, pp. 313-6), comesto this conclusion:-"The combination of the very unstableair mass, large positive energy area (asshown on the tephigram) and very highair and ground temperatures. furtherallied to the marked horizontal convergenceof the sea-breeze front, would behighly conducive to the formation of avigorous vortex which would developon the front as a wave depression. Thevortex would move along the sea-breezefront with the direction of the wind inthe? lower levels and the circulationwould probably be maintained to afew thousand feet. The Wheelus Field(upper air) ascent gives the wind at2.000 ft. at this time as 290·, 8 kL It istherefore suggested that this very largedust whirl was a small vigorous wavedepression on the sea-breeze front.OBITUARYANGUS MACAULAYHE Aberdeen <strong>Gliding</strong> <strong>Club</strong> has suffereda very sad loss with the deathTof their C.P.I. Angus Macaulay, whodied on 28th <strong>No</strong>vember after a shortillness. Angus, who was 40, served forsome years ~s a pilot with the R.A.F.,where he gained flying experience onmany types 01 aircraft. When he returned56to civilian life he joined our dub andsoon beeame an instructor, being appointedas C.P.I. in 1961. His kind natureand understanding of pupils' difficultiesbas helped so many of us. He was alsoresponsible for our Tug aircraft, whichhe organized with that keen efficiencywhich was so typical of him.We shall all miss him very much.He leaves a wife and three youngchildren. J. P. W.
iBOOK REVIEW•Great Flights and Air Adventures, by NORMAN MACMILLAN. Published1964 by G. Bell and Sons Ltd., London. Price 21s.HIS book is subtitled "From Balloons to Spacecraft", and the 22 chapters cer·T tainly show variety. The first is an account of Gerden Cooper's orbital flight in1963, the next of a distance record by balloon from England to Russia in 1907. thethird of the earliest cross-Channel flights, the fourth of the first crossing of theAlps by aeroplane, and so on.Captain Macmillan uses published material almost entirely and rewrites it injournalistic style. Yet my favourite Macmillan book remains his first, "The Art ofF ying", pUblished in 1928, in which he wrote about the ways of the air like asailplane pilot. But he seems to have "written himself out" on the subject in thatonc book, for he never took up gliding, and his 19 subsequent books have beenalmost entirely about other people's flights, though this one includes a flight ofhis over the Andes.In the present b00k, gliding gets only two chapters, both devoted to the flyingcareer of Hanna Reitsch and evidently based on her autobiography (except that heplaces the Rossitten gliding centre in Pomerania instead of East Prus.~ia). The firstof the two starts with her first cloud flight, in which she lost control in a cu·nim,and the second ends with her imprisonment for 15 months by the Americanauthorities because they thought she had been Hitler's pilot. (The identity of Hitler'sprivate pilot has since been disc.losed in a book, ~Hit1er's Pilot", by Hans Baur,published in English translation in 1958; he held down the job from 1932 till thelast days in the Berlin bunker.) In between, much flying in various aircraft isdescribed, including a detailed account of her crossing of the Alps in a SperberJunior from Salzburg to the Piave valley in 1937.The last five chapters are devoted to space travel and include most of themanned flights. The book would make interesting reading for any young aviation"fan",Some Further Observations from Aircraft of Temperatures andHumidities near Stratocumulus Cloud, by J. G. MooRE, B.SC. MeteorologicalOffice Scienti.fic Paper <strong>No</strong>.. 19. Published 1964 by H.M. StationeryOffice, 'London. Price 3s.TRATOCUMULUS cloud sheets are known to be formed from water vapourSlifted by convection and turbulence from the moist layer of air just above theearth's surface. Yet, although sailplane pilots have often found thermals belowstratocumulus, they never seem to have been lifted by these thermals right intothe cloud.This paper gives observations from 11 meterological flights below, throughand above stratocumulus - eight in the daytime, two at night and one at sunset,at! in the Farnborough area. In each flight, runs were made at every 250 ft. levelexcept for the first 500 ft. above the cloud top, where they were made at every 100 ft.This paper is l'Iot interested in thermals as such, but it gives temperaturereadings at the various heights, plotted on a tephigram, and from these One canaSSume that the air has been stirred by thermals at any level where there is anadiabatic lapse rate. So here is a summary (by the reviewer) of the findings, givingthe time and date of each flight:-(1) Dry adiabatic lapse rate up to and through the cloud layer to its top:10.00-13.00 G.M.T., 24th October; 10.10-12.50, 19th March.. (2) Dry adiabatic rate up to and part of the way throug'h the cloud layer:1~.20-17.30, 18th March; 18.00-20.30, 23rd Oct.; 18.00-20.30, 3rd <strong>No</strong>v.; 10.30-12.30,,bth March (most of the way through a layer 1,500 ft. thick).57
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SA LP A&GLIDIGFebruary - March 1965
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SAILPLANE& GLIDINGOFFICIAL ORGAN OF
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1965 WORLD G,LIDINGCHAMPIONSHIPSHE
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FRED SLINGSBY'S RETIREMENTANY are t
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D-34(o)D·36Polyt 3Kria7
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- Page 17 and 18: TESTING A SOVIET DISCOPLANEBy V. IV
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- Page 29 and 30: of the Sheffield gale. The other is
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- Page 53 and 54: wings ar~ lewel. If you can do this
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