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COMBAT AND COMPETITION.pdf - Lakes Gliding Club

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<strong>COMBAT</strong> <strong>AND</strong> <strong>COMPETITION</strong><br />

weak and narrow. And fortunately the only time that happened turned<br />

out to be a no contest day.<br />

When penetration was needed the laminar flow wing came into its<br />

own and 'speed to fly' began to make real sense. This method of<br />

soaring as fast as possible from A to B, adjusting your airspeed<br />

between thermals according to the average rate of climb in the last<br />

thermal, had been developed by Paul MacCready in the United States.<br />

An excellent article by Nick Goodhart had appeared in a recent issue<br />

of Sailplane and <strong>Gliding</strong> explaining how to apply the MacCready<br />

calculations to the polar curve of a glider and use it in the air.<br />

That year too the number of speed tasks brought home more than<br />

ever the excitement, and the suspense, of racing to a goal. Our early,<br />

almost intuitive, final glide computations - say four miles per thousand<br />

feet - adjusted for some vaguely estimated tailwind - plus 20% added<br />

height for the wife and child! - were slowly becoming more scientific.<br />

Tony D2 had already followed up Nick's ideas on MacCready and<br />

shown us how to use the Cobb Slater variometer with the addition of<br />

a hexagonal pencil as a speed to fly director. But his Mark I final glide<br />

computer was yet to come.<br />

Until that day those of us who thought about it were guided by<br />

another simple rule which went something like this. Is the aiming point<br />

- that distant airfield you were so anxious to reach - moving upwards<br />

on your canopy as you get closer? - if so you need more height. Is it<br />

moving downwards? - increase your speed. Stationary? - you lucky<br />

chap! - but beware of downcurrents on the way.<br />

However you approached the final glide there were moments of<br />

tension and uncertainty. Perhaps it was late and the convection was<br />

already dying, or a gap in the clouds ahead might indicate a<br />

downdraught area which could force you to land short. Worse still, sea<br />

air penetrating inland on a day with good convection could mean a<br />

complete absence of thermals, and a possible headwind, on those last<br />

vital ten or fifteen miles.<br />

Failure to complete the course, even by a matter of inches, could<br />

be catastrophic. A total loss of speed marks - too awful to contemplate.<br />

And for some strange reason the closer you were to success the more<br />

marginal it seemed. Then came the magic moment when it was in the<br />

bag, when you could start winding up the speed, and there was only<br />

a last long dive to the line.<br />

Sheer pleasure and raw competitive emotion filled those last<br />

glorious seconds. As the speed rose in final crescendo you felt<br />

168

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