What would be an indicator of a microburst event?

A microburst is a small, localized downdraft that produces an intense blast of wind at or near the surface, usually associated with thunderstorms. The primary characteristic of a microburst is sudden wind shear, which refers to a rapid change in wind speed and direction over a short distance. This makes sudden wind shear near the surface a key indicator of a microburst event.

When a microburst occurs, it can create extremely hazardous conditions for aircraft, as the sudden downdrafts can lead to rapid loss of altitude, making awareness of wind shear crucial for flight safety.

Heavy, steady rainfall, consistent cloud cover at high altitude, and gradual temperature changes do not specifically denote the presence of a microburst. While they might be features associated with broader weather patterns, they lack the immediate and intense wind characteristics that define microbursts.