Air pockets, referring to areas of sudden and unexpected turbulence experienced in flight, are primarily caused by rapid changes in air pressure and wind speed. The provided reference incorrectly identifies the causes of air pockets. Here's a breakdown of the actual mechanisms:
Factors Contributing to Air Pocket Formation:
-
Clear Air Turbulence (CAT): This is the most common cause and is often difficult to predict. It occurs in areas with strong wind shear, where winds change speed or direction rapidly over a short distance. Jet streams are often associated with CAT.
-
Mountain Waves: When air flows over mountains, it can create waves in the atmosphere similar to ripples in a pond. These waves can break and cause turbulence.
-
Thermal Activity: Rising columns of warm air (thermals) and sinking columns of cool air can create bumpy conditions, especially on hot days. This is more common at lower altitudes.
-
Thunderstorms: Although the referenced information mentions thunderstorms, they don't directly cause air pockets in the sense of small, isolated voids. Rather, they are regions of severe turbulence due to strong updrafts, downdrafts, and wind shear.
-
Wake Turbulence: Large aircraft leave behind swirling vortices of air. These vortices can cause significant turbulence for smaller aircraft that fly through them.
Why the Initial Information is Incorrect:
The provided reference links air pocket formation to "thunderstorms, volcanic activity, and sea level rise." While thunderstorms do cause turbulence, the term "air pocket" is a misnomer; the turbulence is due to strong air currents, not literal pockets of air. Volcanic activity can release ash into the atmosphere, which can damage aircraft engines but isn't typically described as creating air pockets. Sea level rise is unrelated to air turbulence.
In Summary:
Air pockets, more accurately described as areas of turbulence, result from abrupt changes in wind speed and direction, often due to clear air turbulence, mountain waves, thermal activity, thunderstorms, or wake turbulence.