How does the wind normally behave in a hurricane?

In a hurricane, the behavior of the wind is characterized by a phenomenon known as backing and an increase in speed as it approaches the storm's center. As the hurricane intensifies, winds within the surrounding areas tend to rotate inwards towards the low-pressure center of the storm. This rotation causes the wind to back, meaning it shifts counterclockwise in the Northern Hemisphere, particularly as one gets closer to the eye of the hurricane.

Additionally, as the wind converges toward the center, the speed of the wind increases significantly. This is due to the conservation of angular momentum and the steep pressure gradient that exists in hurricanes. As air is drawn into the center, it accelerates, resulting in the characteristic high wind speeds associated with hurricanes.

In contrast, a straight-line wind pattern, a veering of wind with decreased speed, or calm conditions would not accurately describe the dynamic and intense nature of winds in a hurricane environment. The conditions are quite turbulent and chaotic rather than stable or devoid of activity.