Where is hazardous wind shear commonly encountered?

Hazardous wind shear is commonly encountered in areas of temperature inversions and near thunderstorms due to the unique atmospheric conditions present in these environments. A temperature inversion occurs when a layer of warm air traps cooler air near the surface, creating a stable atmosphere that can lead to significant changes in wind speed and direction over short vertical distances. This condition often results in strong wind shear, as the wind at higher altitudes can be dramatically different from the surface winds.

Additionally, thunderstorms are associated with intense upward and downward drafts, which also contribute to significant wind shear. The rapid changes in wind patterns around thunderstorms can create very turbulent conditions, posing a challenge for flight operations. Understanding these factors is essential for pilots and meteorologists to ensure safety when flying in these conditions.