GEOS 112L - Introduction to Earth Science |
The flattening of planets: In class I stated the hypothesis that the shape of a planet can be used to deduce its physical state, whetehr it is mostly solid, liquid or gaseous. In this exercise you will calculate the flattening for all planets and the sun. If you'd like you can also throw in some of the major moons as well. Planetary flattening (F) can be expressed by the following formula:
where req is the equatorial radius of the planet and rp is the polar radius of the planet (see figure above). For a perfect sphere both radii are identical and we get a flattening of 0%, for flattened planets rp is smaller than req and you should get a positive number. Muliplying the result by 100 expresses your result in percent. Assignment:
What to turn in:
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