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Now
that winter is upon us, the potential for aircraft icing is something
that all pilots need to be aware of. Aircraft icing destroys the smooth
flow of air, increasing drag while decreasing the ability of the airfoil
to create lift.
The
actual weight of the ice on the airplane is insignificant when compared
to the airflow disruption it causes. As power is added to compensate
for the additional drag and the nose is lifted to maintain altitude, the
angle of attack is increased, allowing the underside of the wings and
fuselage to accumulate additional ice. Ice accumulates on every exposed
frontal surface of the airplane-not just on the wings, propeller, and
windshield, but also on the antennas, vents, intakes, and cowlings. It
builds in flight where no heat or boots can reach it. Ice can cause
antennas to vibrate so severely that they break. In moderate to severe
conditions, a light aircraft can become so iced up that continued flight
is impossible. The airplane may stall at much higher speeds and lower
angles of attack than normal. It can roll or pitch uncontrollably, and
recovering may be impossible. Ice can also cause engine stoppage by
either icing up the carburetor or, in the case of a fuel-injected
engine, blocking the engine’s air source.
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TYPES OF
ICE |
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RIME ICE |
Has a
rough, milky white appearance and generally follows the contours of
the surface closely. Much of it can be removed by de-icing
systems or prevented by anti-ice. |
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CLEAR (OR GLAZE) ICE |
Generally
clear and smooth, but does contain some air pockets that result in a
lumpy, translucent appearance. The larger the accretion, the
less glaze ice conforms to the shape of the wing. Clear ice is
denser, harder, and usually more transparent than rime ice, and
harder to break. |
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MIXED ICE |
As
the name implies, it is a combination of rime and clear ice. |
Wind tunnel and flight tests have shown that frost, snow, and ice
accumulations on the leading edge or upper surface of the wing no
thicker or rougher than a piece of course sandpaper can reduce lift by
30 percent and increase drag up to 40 percent. Larger accretions can
reduce lift even more and can increase drag by 80 percent or more.
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Fronts
and low pressure areas are the biggest ice producers, but isolated
air mass instability with plenty of moisture can generate enough ice
in clouds to make light aircraft flight inadvisable.
Freezing rain and drizzle is the ultimate enemy that can drastically
roughen large surface areas or distort airfoil shapes and make
flight extremely dangerous or impossible in a matter of a few
minutes. Freezing rain occurs when precipitation from warmer air
aloft falls through a temperature inversion into below freezing air
underneath. The larger droplets may impact and freeze behind the
area protected by surface deicers. |
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