What is turbulence in meteorological terms?

Turbulence in meteorological terms refers to any irregular or disturbed flow that produces gusts or eddies in the atmosphere. It occurs when air flows are disrupted by various factors, such as terrain, temperature gradients, or wind shear. This disturbed flow can create varying levels of intensity, potentially leading to an unpredictable and chaotic movement of air. It's commonly encountered during flight and can significantly influence weather patterns and conditions.

This definition emphasizes the nature of turbulence as an irregular phenomenon, distinguishing it from smooth or laminar flow, which is characterized by much more orderly, consistent air movement. Choices describing a type of weather front or a low-pressure area do not capture the essence of turbulence but rather represent specific meteorological formations or patterns.