jartsa said:
Let's say I build a 500 m long circular road around the north pole. Then I drive on the road at speed 20 m/s, to the east.
There will be a noticeable inertial force to the south.
Is that inertial force a Coriolis force?
Well: in Meteorology that effect is indeed referred to as 'Coriolis effect'.
Instead of thinking about a road, I suggest to consider a hovercraft, a big one. (The biggest hovercrafts have a mass of several hundreds of tons)
A hovercraft that is hovering in place is co-rotating with the Earth's rotation. A hovering craft doesn't have a tendency to drift towards the equator because the Earth's shape gives rise to the required centripetal force.
The Earth has an equatorial bulge; the distance from the Earth's center to the equator is about 20 kilometers more than the distance from the center to (each of) the poles.
You can calculate that at 45 degrees latitude an incline (towards the nearest pole) of 0.1 degree is needed to provide the required centripetal force. The Earth's bulge provides just that incline.
When that hovercraft has a velocity relative to the Earth then you get dynamic effects.
- When the hovercraft is cruising due east it is circumnavigating the Earth faster than equilibrium speed, so it tends to veer off course, towards the equator
- When the hovercrat is cruising due west it is circumnavigating the Earth slower than equilibrium speed, so it tends slide towards the nearest pole.
- And of course there are also tendencies to veer off course when moving due north and due south.
In meteorology those tendencies in the various directions are grouped under a single name: 'Coriolis effect'. The magnitude of the tendency to veer off is given by the expression: 2mΩv
where:
m = mass of the moving object
Ω = angular velocity of the Earth
v = velocity relative to the Earth
This expression, 2mΩv, is valid for any direction of motion relative to the Earth.
In Meteorology it makes sense to organize things like that. In meteorology you simply say: 'the Coriolis effect is the same in all directions', and you take it from there.
Some people may argue that it's better to restrict the expression 'Coriolis effect' to radial motion only. But for meteorology that is highly unpractical. It would deprive you of a way of thinking about general properties of atmospheric flow efficiently.
Some additionanl remarks:
Getting back to the hovercraft, cruising due east. What you
notice is a need to compensate for a tendency to veer off. When cruising due west the hovercraft's propulsion system must itself provide the required extra centripetal force. It's not necessary to think about that situation in terms of 'an inertial force that tends to deflect you'. You are quite aware of what is going on. When cruising east you need to compensate for insufficient centripetal force. Conversely, when cruising west there is a surplus of centripetal force.
Meteorology is (among other things) the study of fluid motion of the atmosphere. Oceanography is (among other things) the study of fluid motion of the Earth's oceans. Those two fields of fluid dynamics have many parallels, in particular the terrestrial Coriolis effect. The general term is 'Geophysical fluid dynamics'. So the more general statement is that in Geophysical fluid dynamics these rotation-of-Earth-effects are referred to as 'Coriolis effect'.