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KRONFELD ON GLIDING AND SOARING.pdf - Lakes Gliding Club

KRONFELD ON GLIDING AND SOARING.pdf - Lakes Gliding Club

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294 <strong>KR<strong>ON</strong>FELD</strong> <strong>ON</strong> <strong>GLIDING</strong> & <strong>SOARING</strong><br />

to the ocean's breakers, accommodate themselves to the<br />

currents. This zone of surf and breaker-like activity<br />

generally extends to a height varying from six thousand<br />

five hundred to ten thousand feet above the ground.<br />

When the wind encounters an obstacle, it has to give way.<br />

If a tower or a low hill rises from the plain, the wind's<br />

simplest way is to go round it. If, on the other hand, a<br />

long chain of hills crosses the wind's course, it must go<br />

CURRENTS <strong>ON</strong> HILLSIDE<br />

COURSE OF CURRENTS MAINLY OVER THE HILL, HENCE<br />

MUCH UPWIND<br />

over it. If we keep our eyes open, we can observe these<br />

natural phenomena every day and note all the various<br />

ways in which currents are formed. In a snowstorm there<br />

is generally a patch free from snow behind any isolated<br />

obstacle, showing the path of the wind around it. From<br />

the course of the snowflakes round the corners of houses,<br />

over roofs and past any obstacle, it is possible to acquire<br />

knowledge which can be put into immediate practice on<br />

a larger scale when soaring in the high mountains. In<br />

summer we may ascertain the direction of the breeze from

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