Η Ατμόσφαιρα σε Υδροστατική Ισορροπία
The reason for the presence of the atmosphere is the earth’s gravitational field. In this chapter, the atmospheric motions are ignored and the atmosphere is assumed to be in static equilibrium, which means that the force of gravity is balanced by the vertical pressure gradient force. First, the hydr...
| Κύριοι συγγραφείς: | , |
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| Μορφή: | 7 |
| Γλώσσα: | Greek |
| Έκδοση: |
2016
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| Διαθέσιμο Online: | http://repository.kallipos.gr/handle/11419/3275 |
