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As the pressure gradient increases, the wind velocity increases. This is because a larger pressure gradient indicates a greater difference in pressure between two points, leading to a stronger force exerted on the air. This stronger force results in faster wind velocities.
On a weather map, the lines of equal pressure (isobars) also illustrate the pressure gradient or change of pressure per distance. The higher the pressure gradient, the higher the winds speed. Thus, when the isobars are close together, the gradient is high, and winds are higher than where the isobars are further apart. Wind can also be affected by local considerations, hills, valleys, and buildings can modify the gradient wind's direction and speed.
The wind at a standard height of 10 m 33 ft above ground. Differs from the geostrophic wind and the gradient wind because of friction with the Earth's surface.
Closer spacing of isobars indicates stronger pressure gradient force, leading to higher wind speeds. The tighter the isobars, the faster the wind will blow. Conversely, wider spacing of isobars typically indicates weaker pressure gradient force and lower wind speeds.
There must be a difference in air pressure between two regions. The pressure gradient force must be present to drive air from high-pressure areas to low-pressure areas. The Coriolis effect must influence the direction of the wind as it flows along the pressure gradient.