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| | USATODAY.com |
 | | In simple terms, in the Northern Hemisphere, while the Coriolis force is pushing the wind toward the right, the pressure-gradient force, caused by air pressure differences, is pushing the air toward the center of the area of low pressure, and for various reasons is stronger then the Coriolis force. |
 | | The face that the Coriolis force is zero at the equator and very week near the equator, explains why tropical cyclones such as hurricanes and typhoons won't form on the equator even though the other factors there, such as warm ocean water, would make them likely. |
 | | Understanding the Coriolis force is difficult, in addition to the material on Alistair Fraser's Coriolis FAQ, you'll find a different way of looking at things by going to the Rotating Frames of Reference in Space and on Earth section of NASA's From Stargazers to Starships Web book. |
| www.usatoday.com /weather/resources/basics/coriolis-understanding.htm (533 words) |
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