Winds don't blow directly north or south. The movement of wind is affected by the rotation of the Earth. The Earth's rotation causes wind to travel in a curved path rather than a straight line. The curving of moving objects, such as wind, by the Earth's rotation is called the Coriolis Effect.
The coriolis effect, a product of the Earth's rotation, essentially "turns" the direction of air flow from one that goes directly from high to low pressure (which happens on a non-rotating surface) to one that either spirals toward lower pressure at an angle or blows parallel to the pressure gradient (a full 90 degree turn).
Winds don't blow directly north or south. The movement of wind is affected by the rotation of the Earth. The Earth's rotation causes wind to travel in a curved path rather than a straight line. The curving of moving objects, such as wind, by the Earth's rotation is called the Coriolis Effect.
it could affect by the hemisphere
What is coriolis effect
The influence of earths rotation is called the Coriolis effect. The coriolis effect causes wind to curve instead of going in a straight line.
The Coriolis Effect.
Coriolis effect
Coriolis effect global winds and continental deflections are all factors that control surface currents.
it is called the Coriolis effect
it affected influince winds because coriolis can go out of control so it makes winds stronger.
the Coriolis effect
The influence of earths rotation is called the Coriolis effect. The coriolis effect causes wind to curve instead of going in a straight line.
The influence of earths rotation is called the Coriolis effect. The coriolis effect causes wind to curve instead of going in a straight line.
The Coriolis Effect.
Coriolis or Coriolis effect
The Coriolis effect has the least effect on winds in equatorial regions and the most effect on winds in polar regions. Coriolis effect deflects winds to the right of their initial direction in the northern hemisphere and left of their initial direction in the southern hemisphere.
Coriolis Effect
Coriolis effect
The Coriolis effect
Coriolis effect
Coriolis effect