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WFO Lake Charles, LA  Winter 2005
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Aircraft Icing
By Mark Wiley, Journeyman Forecaster

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.

TYPES OF ICE

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.
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.
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. 

Picture of ice on wings

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.  

Freezing drizzle is commonly formed when droplets collide and coalesce with other droplets.  As the droplets grow in size, they begin to fall as drizzle.  Large scale icing can develop north of a surface warm front.  Along and north of the warm front, the warmer air lifts over the colder air, forming stratus clouds conducive to icing.

ICING RISK Cumulus Clouds Stratiform Clouds Rain and Drizzle
HIGH 0 to -20 C
(32 to -4 F)
0 to -15 C
(32 to 5 F)
0 C and below
(32 F and below)
MEDIUM -20 to -40 C
(-4 to -40 F)
-15 to -30 C
(5 to -22 F)
 
LOW less than -40 C
(less than -40 F)
less than -30 C
(less than -22 F)
 


To find out where icing is forecast or occurring from the NWS Lake Charles web page, click on the aviation link where you’ll find more links for icing sigmets as well as any pireps.  There is also a link to the Aviation Digital Data Service (ADDS) with a detailed icing forecast.  Don’t forget to request pireps (and make some of your own) along your route if you suspect icing to be a potential problem.

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Page last modified: January 4, 2005

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