May 14, 2009  

Greetings!

AIRMET Zulu does not catch all widespread icing events AIRMET Zulu

     AIRMET Zulu is issued by the Aviation Weather Center for a widespread area of icing.  Widespread is defined as icing that is affecting or is forecast affect an area greater than 3,000 square miles.  For reference, 3,000 square miles is a little over half the size of the state of Connecticut.   

     AIRMET Zulu isn't designed to put a fence around you all possible areas of structural icing, even widespead icing.  One example, is icing associated with deep moist convection, better known as thunderstorms.  Even before towering cumulus reach the point of letting go of that first lightning strike, you won't likely see an AIRMET issued for this field of cumuliform clouds.  In many cases, these areas of potential icing don't typically meet the AIRMET criteria.  This is a frequent occurrence throughout the summer.

Current Icing Product (CIP) Severity     Notice that in the icing AIRMETs image above (click here for a larger image) that AIRMET Zulu isn't present anywhere in Illinois, Missouri or Arkansas despite the high probability of icing as shown on the Current Icing Product (CIP) shown on the left (click here for a larger image). 

     Turns out that most of the icing in the Mid-Mississippi Valley area is due to moist deep convection as shown on the image below (click here for a larger image).  The freezing level is likely in the the low teens, so flight at or above the freezing level will result in heavy icing and possible supercooled large drop (SLD) icing.          

     Once thunderstorms reach convective SIGMET criteria, the Aviation
Convective SIGMETs Weather Center will put a fence around this area and call it a convective SIGMET. Convective SIGMETs always imply the possibility for severe icing so the Aviation Weather Center doesn't issue AIRMET Zulu or a SIGMET for severe icing since it would be redundant.  Keep in mind that icing still may exist around any convective cells at an altitude above the freezing level.  Often thunderstorms produce convective debris that isn't likely turbulent, but may contain supercooled liquid water.  All pilots should anticipate a high probability of intense icing flying into visible moisture around convectivity activity and there will not likely be an AIRMET or SIGMET telling you about it.

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