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The Coriolis effect is the result of the earth's rotation having an effect on things on it's surface most notably wind and water. This effect can produce the starting winds for hurricanes and keeps them from moving towards the equator.
The Coriolis effect results in a deflection of fluid flows (to the right in the Northern Hemisphere and left in the Southern Hemisphere). Because the distance around the Earth decreases as one moves away from the equator, and because the Earth rotates in a counter clockwise direction as seen from the north pole, air and water masses are deflected to the east as they move from the equator to the poles, and to the west as they move from the poles to the equator. This has profound effects on the flow of the oceans. In particular it means the flow goes around high and low pressure systems, permitting them to persist for long periods of time. As a result, tiny variations in pressure can produce measurable currents. A slope of one part in one million in sea surface height, for example, will result in a current of 1 cm/s at mid-latitudes. The fact that the Coriolis effect is largest at the poles and weak at the equator results in sharp, relatively steady western boundary currents which are absent on eastern boundaries
As a consequence of the Coriolis effect large scale wind currents get deflected relative to a pressure gradient, to the right in the southern hemisphere and to the left in the northern hemisphere. As a result, large scale pressure systems rotate, such as hurricanes, which are strong low-pressure systems. This rotation actually allows storms to become better organized and intensify even further. At the equator, where the Coriolis effect is essentially nonexistent storms cannot organize in such a fashion, and so usually nothing more than disorganized bands of weak thunderstorms develop.
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The Coriolis effect is the result of the earth's rotation having an effect on things on it's surface most notably wind and water. This effect can produce the starting winds for hurricanes and keeps them from moving towards the equator.
The Coriolis effect is caused by the rotation of the Earth and the inertia of the mass experiencing the effect. This force causes moving objects on the surface of the earth to be deflected in a clockwise sense (with respect to the direction of travel) in the Northern Hemisphere and in a counter-clockwise sense in the Southern Hemisphere.
The Coriolis effect
The swirling of winds, ocean currents, bathroom drains, tornados and similar is a result of the Coriolis effect. Thechnically it is descrined as a deflection of moving objects when they arei placed in a rotating reference frame.
Coriolis Effect
The Coriolis effect results in a deflection of fluid flows (to the right in the Northern Hemisphere and left in the Southern Hemisphere). Because the distance around the Earth decreases as one moves away from the equator, and because the Earth rotates in a counter clockwise direction as seen from the north pole, air and water masses are deflected to the east as they move from the equator to the poles, and to the west as they move from the poles to the equator. This has profound effects on the flow of the oceans. In particular it means the flow goes around high and low pressure systems, permitting them to persist for long periods of time. As a result, tiny variations in pressure can produce measurable currents. A slope of one part in one million in sea surface height, for example, will result in a current of 1 cm/s at mid-latitudes. The fact that the Coriolis effect is largest at the poles and weak at the equator results in sharp, relatively steady western boundary currents which are absent on eastern boundaries
As a consequence of the Coriolis effect large scale wind currents get deflected relative to a pressure gradient, to the right in the southern hemisphere and to the left in the northern hemisphere. As a result, large scale pressure systems rotate, such as hurricanes, which are strong low-pressure systems. This rotation actually allows storms to become better organized and intensify even further. At the equator, where the Coriolis effect is essentially nonexistent storms cannot organize in such a fashion, and so usually nothing more than disorganized bands of weak thunderstorms develop.
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