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Irishwolf
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Can somebody please explain ( properly)with examples , how the right hand rule describes the direction of coriolis acceleration? please!
Thanks that does help, but I am still puzzled on how to determine the cartesian coordinates (x,y,z) , for the rotating reference frame ? any ideas please?TheShrike said:The Coriolis term is [itex]\textbf{}F_C{}[/itex] = -2m[itex]\textbf{}Ω[/itex][itex]\times[/itex][itex]\textbf{}v[/itex]
Where Ω is the angular velocity and v is the velocity of the body you are observing from the rotating reference frame.
To give an example imagine you are rotating with some constant angular velocity. For definiteness let's say you are rotating counter-clockwise. Then the angular velocity vector points upwards out of your head.
Now you observe a body somewhere around you. To determine the direction of the Coriolis effect you take the cross product between your angular velocity and the velocity of the body.
Again, for definiteness, let's say when you first observe the body it is directly in front of you and has a velocity to your left. (After this instant things will change of course, but that is what we are trying to find out).
Using the right-hand rule your thumb is pointing upwards in the direction of angular velocity. Your index finger points in the direction of the velocity of the body which should be to your left. Now your middle finger should point towards yourself, but there is a minus sign we must look at, so the Coriolis effect points outwards away from you, rather than towards you.
I hope that is correct and that it helps.
Coriolis acceleration is a phenomenon that occurs due to the rotation of the Earth. It is an apparent acceleration experienced by objects moving on a rotating body, such as the Earth, and is responsible for the deflection of objects moving in a straight line relative to the rotating body.
The Coriolis acceleration is calculated using the formula a = 2Ω x v, where a is the Coriolis acceleration, Ω is the angular velocity of the rotating body, and v is the velocity of the moving object. This formula follows the right hand rule, where the direction of the acceleration is perpendicular to both the angular velocity and the velocity of the object.
The right hand rule is used to determine the direction of the Coriolis acceleration. By pointing the thumb of the right hand in the direction of the angular velocity and the fingers in the direction of the velocity of the object, the direction of the acceleration can be determined by the direction in which the palm is facing.
No, the Coriolis acceleration varies with latitude. As the Earth is a rotating sphere, the angular velocity changes with latitude, resulting in a varying Coriolis acceleration. This is why the Coriolis effect is stronger near the poles and weaker near the equator.
The Coriolis acceleration plays a significant role in the formation of weather patterns. It causes air and water masses in the atmosphere and oceans to deflect, which creates circulation patterns such as hurricanes and typhoons. These patterns are important for regulating the Earth's climate and weather systems.