Last weekend we had an excellent sailing trip from Nieuwpoort to Ramsgate and back again. And as it happens on such occasions, conversation touched the subject of Coriolis forces, which is important - for sailors - to understand the deviations of air flows when they move from high to low pressure areas (deviation to the right in the Northern hemisphere, deviation to the left in the Southern hemisphere).
Often these conversations get needlessly complex. So here is my stab at it. The Coriolis force is a pseudo force, just as the centrifugal force is a pseudo force. You only need these pseudo forces to explain things if you are an observer on Earth who is not able to imagine how things would look from a distance. I was told a sailor must be able to see his boat from a bird’s perspective, so sailor, just fly a bit higher and watch the Earth from a few thousand (nautic) miles and you can forget about Coriolis and rely on more basic physics:
1. Newtonian inertia: tendency of an object to maintain its state of uniform motion (unless acted on by an external force).
2. The velocity of an object making a rotational movement (e.g. a rock on the surface of the Earth) is the ‘rotational velocity’ times the distance to the rotational axis. This means that a rock on the equator moves faster than a rock on the Tropic of Capricorn or the Tropic of Cancer.
3. Context: air moves in a thin layer around the Earth.
So what happens to an air particle that moves from South to North in the Northern hemisphere: since it is stuck in this thin layer around Earth, it moves to an area where the Earth’s velocity is lower than the velocity of the particle, and since it wants to keep its velocity, it moves along a line that curves to the right. The same reasoning can be applied for moving from North to South and for the equivalent cases in the Southern hemisphere.
When moving from West to East in the Northern hemisphere the reasoning is as follows: the (air) particle’s speed is larger than the speed of the underlying surface of the Earth. Because of its higher tangential speed the particle has the tendency to get thrown out of its orbit and move away from the Earth’s axis, but since it is locked in this thin layer, it can only do so by deflecting to the South, thus making a curve with a deviation to the right. Again, similar reasonings can be made for East to West and for the cases on the Southern hemisphere.
So no talking about Coriolis or other pseudo forces needed to understand air movements on Earth.