rime ice


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Related to rime ice: Aircraft icing

rime ice

rime ice
Jagged appearance of rime ice.
A type of icing that can be called a freezing fog. It forms as a thick, frosty deposit when objects with subfreezing temperatures encounter a fog. In such a case, the minute fog droplets freeze and adhere to the cold surface. It can also occur when an aircraft flies through certain types of clouds. The entrapped air in the ice gives it a crystalline opaque appearance. See also glaze ice.
An Illustrated Dictionary of Aviation Copyright © 2005 by The McGraw-Hill Companies, Inc. All rights reserved
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Power levers pushed to maximum torque, we accelerated down the runway, pulled the nose up, raised the gear, hit IFR at 1,000 feet, and again noted the light rime ice attaching itself to the leading edge of the wing.
Altitude flexibility yields options for dodging rime ice and nearby alternates provide choices if things just aren't working out.
The pilot subsequently picked up some light rime ice during the approach and turned on all of the airplane's deicing equipment.
"The pilot reported picking up light rime ice while descending from 9000 feet for a GPS approach.
Plowing upward through this stratus deck--so much for forecasts of instability, eh?--you start accumulating a bit of rime ice. All the old salts around the airport seem to think it's best to just keep climbing in this situation.
The airplane picked up light rime ice during descent, breaking out at around 1700 feet MSL, or 900 feet AGL.
I once flew our Aztec 6190Y down ILS final to Midway right behind another Aztec in the winter, and I had a lot less rime ice on the leading edge of the wing than the other Aztec.
I had a trace of rime ice and assumed the pilot pitot tube had burned out.
The original plan was to make an evening flight, but when the time came, gusts were over 30 knots across the Northeast and ceilings ranged from 900 to 3000 with reports of moderate rime ice in several places.
As the airplane climbed through 11,000 feet msl, the captain noted light rime ice accumulating.
we cross 1000 feet of cloud with a dusting of rime ice. We do the same at the next layer and pop out on top with light rime on the leading edges.