An object's speed and direction of movement remain constant unless a force is exerted on it.
This principle applies to any object, including air, which has mass.
Air at rest stays stationary; air in motion continues to move at the same speed and direction unless acted upon by a force.
The upward directed pressure gradient force is significant, especially as air pressure decreases with altitude.
This creates a paradox as one might think high pressure should propel us into space.
Gravity balances this upward force, resulting in no net force acting on us.
To change an object's movement (speed or direction), a net force must be present:
Example using a golf ball and two golf clubs hitting it from opposite sides:
If both forces are equal and opposite, the ball will not move; it stays stationary.
The air's movement indicates the presence of a net force acting upon it.
Pressure gradient is crucial for understanding wind:
Higher pressure inside a balloon demonstrates the concept; pop it and air rushes out due to higher internal pressure.
Isobars on a map connect points of equal pressure; they illustrate pressure gradients:
Closer isobars indicate a steep pressure gradient, predicting stronger winds.
Wider spaced isobars reflect a weak pressure gradient, resulting in calmer winds.
Coriolis effect affects the movement of air, water, and other objects on Earth's surface:
In the Northern Hemisphere, deflection is to the right;
In the Southern Hemisphere, deflection is to the left.
This effect is crucial for understanding wind patterns and ocean currents as air moves from areas of high pressure to low pressure.