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Training Tip: Standing up for turbulenceTraining Tip: Standing up for turbulence

What’s the most remarkable item (that’s a hint) in this surface weather report?

KBGR 071953Z 19022G30KT 10SM FEW090 SCT250 23/09 A3008 RMK AO2 PK WND 18034/1940 SLP185 ACSL NW-NE T02280094

Photo by David Tulis.

Yes, the wind’s strong and gusty, but that’s not it.

Visibility's fine, no help there.

There are some clouds at two levels of the atmosphere, but ho-hum. And the altimeter setting of 30.08 inches is as normal as can be.

We’ve now pushed all the way over to the remarks (there’s that hint again) section, where we find and decode the shorthand note about 34-knot peak blasts of that southerly wind. We’re getting warmer, but we are not quite there yet.

Leapfrogging the sea-level pressure (SLP) entry, next we encounter an observation quite unusual for this airport that sits in flat country at 200 feet msl: “ACSL NW-NE.”

This item would be no mystery to a glider pilot, or to a powered-aircraft pilot who flies in mountain country. Down in the flatlands, however, it may feel forgivable to be flustered—but free yourself of that formulation before your flight test.

The notation ACSL warns that “altocumulus standing lenticular clouds” are observed northwest through northeast of the airport. It is there, at considerable distance, where many of Maine’s most majestic mountains are situated; the observation suggests that a mountain wave, often associated with severe turbulence or worse, has formed across the region.

The FAA publication Tips on Mountain Flying discusses the mountain wave phenomenon: “When the wind speed is above about 25 knots and flowing perpendicular to the ridge lines, the air flow can form waves, much like water flowing over rocks in a stream bed. The waves form down wind from the ridge line and will be composed of very strong up and down drafts, plus dangerous rotor action under the crests of the waves. If enough moisture is present, lenticular clouds can form to give a visual indication of the wave action. These clouds are reported in the remarks section of hourly sequence reports as ACSL (altocumulus standing lenticular) or CCSL (cirrocumulus standing lenticular).”

The clouds form at the peak of the mountain wave, and so appear to “stand” still. Seeing a remark about ACSL in a flatland airport weather observation demonstrates why, even if you don’t fly in the mountains, being able to interpret a novel weather phenomenon is critical to making safe decisions about flying.

It’s also testable material on your private pilot practical test. Check the weather information task under the preflight heading of the airman certification standards publication for details.

Dan Namowitz

Dan Namowitz

Associate Editor Web
Associate Editor Web Dan Namowitz has been writing for AOPA in a variety of capacities since 1991. He has been a flight instructor since 1990 and is a 30-year AOPA member.
Topics: Training and Safety, Aeronautical Decision Making, Flight Planning
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