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In the Northern hemisphere, the direction is clockwise... In the Southern, it turns anti-clockwise.
The Coriolis Effect, a consequence of Earth's rotation, causes this.
When i goes over the surface of the Earth it appears to veer right into a Coriolis Effect in the Northern Hemisphere
Axial tilt of the wart moving, or the Coriolis Effect.
gyres in the northern hemisphere circulate clockwise, while the gyres in the southern hemisphere circulate counterclockwise
Right in the northern hemisphere, left in the southern hemisphere.
The Coriolis effect is the clockwise deflection of air in the north hemisphere and the counterclockwise deflection in the Southern Hemisphere.
The Coriolis effect is the clockwise deflection of air in the north hemisphere and the counterclockwise deflection in the Southern Hemisphere.
The deflection of particles to the right in the Northern hemisphere and to the left in the southern hemisphere is known as the Coriolis effect.
The deflection is to the right of the path of motion of the wind.
In the Northern hemisphere, the direction is clockwise... In the Southern, it turns anti-clockwise.
it's to the right.
The Coriolis effect holds that because the Earth is spinning, surfacewaters move in a clockwise direction in the Northern Hemisphere and in acounterclockwise direction in the Southern Hemisphere.
The coriolis effect deflect objects right in the northen hemisphere due to the raotation of the earth from west to east in the counterclockwise direction.
The Coriolis Effect is an apparent deflection of moving objects when they are viewed from a rotating reference frame. Moving objects on the surface of the Earth experience a Coriolis force, and appear to veer to the right in the northern hemisphere, and to the left in the southern hemisphere.
The observed effect of the Coriolis force, especially the deflection of objects or substances (such as air) moving along the surface of the Earth, rightward in the Northern Hemisphere and leftward in the Southern Hemisphere. The Coriolis effect is named after the French engineer Gustave Gaspard Coriolis (1792-1843).
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.