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Very simply, by finding air which is going up faster
than it is going down! In short, a glider regains
the height (and therefore, its potential energy) by
flying in upcurrents that are rising faster than it
is falling. This energy comes from the sun and manifests
itself in three main ways: as thermals, as slope lift
and as a phenomena called wave. The latter two are
caused by the wind blowing onto a hill or a mountain.
Although glider racing generally uses thermals, slope
and wave lift can be also be used. We will concentrate
on thermal driven cross-country.
Thermal cross-country
Thermals are basically rising currents warm air (and
if they could be visualised, they would like the blobs
in a lava lamp). When air near the ground is heated
to a higher temperature than its surroundings, it
will tend to rise when disturbed. It will continue
to rise if the air around it is cooler, as it is less
dense. For instance a cornfield, or a town, will tend
to generate and trap a lot of warm air in the sunshine.
When the warmer air is gently blown towards another
feature, such as line of trees, or a lake (which has
cooler air over it), it will then separate and rise.
Thus to generate the best thermals, you need energy
(the sun), a varying landscape to give contrast and
colder air above the ground. The best days are often
those that have fair weather cumulus; a cumulus cloud
is formed by the water in the rising air condensing
out as the air cools. However, even on cloudless days
(called 'blue days'), there are usually thermals.
There are no clouds because the rising air doesn't
cool enough to form a cloud (or it contains too little
water). The gusts of wind we experience on the ground
on warm sunny days are caused by the ascent of thermals
- you can often feel the wind suddenly get warmer
then colder.
These thermals supply the energy a pilot of a glider
needs to go cross-country. On a good day, thermals
can be found every 5-15 miles, depending on the terrain
and how high they are going. Generally speaking, the
higher the better. In the UK, this can be anything
from a 1000ft to 10,000ft, depending on the time of
year, how much moisture is in the air and how cold
the air is. Good soaring days are often preceded by
cold nights. Unfortunately, what goes up, must come
down. Between the thermals, the air is usually coming
down (and is known as 'sink'), so pilots try and minimise
the time they spend in the sink and maximise the time
they spend in the 'lift'. Thus, to go cross-country,
a pilot will circle in the rising air to gain height,
then cruise at a higher speed to the next thermal
(and will go especially fast in the sink, thus reducing
the time in bad air). The speed at which the pilot
goes cross-country depends on many factors.
Next: Racing
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