Posted by physics on Thursday, August 13, 2009 at 1:41pm.
Yes, the fact that the Earth is an oblate spheroid varies the g vs over a sphere.
Centripetal force reduces apparent weight, not g, but many do not make that destinction.
Weight= mg -mv^2/r and v horizontally, the spin of the Earth, depends on latitude.
Now Mountains: g is a computed field vector dependent on Earth's Mass below it. If you go high on a mountain, you not only change elevation (reducing g) but you increase the mass pulling on you (increase g). Also, the material the mountain range is made of varies g (ie, the mountain range is granite or iron).
The drag is due to free fall, and should not have been mentioned. Actual acceleration to the Earth is g minus drag effects.
One last remark: Normally g is taught in HSchool as the acceleration due to gravity, in m/s^2. But you can do more with that, consider
Fgravity=mass*g or g= forcegravity/mass so g is in the units of N/kg, which is a force field. So consider g a force field intensity. This now puts a new light on the effects of the mountains...
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