The magnitude of the Coriolis force depends on the speed of the object, the latitude at which the object is located, and the mass of the object.
The magnitude of frictional force depends on the nature of the surfaces in contact and the normal force pressing the surfaces together.
The size of an electric force depends on the amount of charge on the objects involved and the distance between them. The force increases with the magnitude of the charges and decreases as the distance between the charges increases.
magnitude and direction more accurate magnitude and sence.
Magnitude and direction.
An electric force depends on the magnitude of the charges involved and the distance between the charges. The force increases with the magnitude of the charges and decreases with an increase in the distance between them.
The magnitude of the Coriolis force is influenced by the speed of the object, the latitude of the object, and the Earth's rotation rate. Objects moving faster or situated at higher latitudes will experience a greater Coriolis force.
The magnitude of frictional force depends on the nature of the surfaces in contact and the normal force pressing the surfaces together.
The size of an electric force depends on the amount of charge on the objects involved and the distance between them. The force increases with the magnitude of the charges and decreases as the distance between the charges increases.
magnitude and direction more accurate magnitude and sence.
Magnitude and direction.
An electric force depends on the magnitude of the charges involved and the distance between the charges. The force increases with the magnitude of the charges and decreases with an increase in the distance between them.
Every force has a magnitude and direction.
The magnitude of force depends on the mass and acceleration of an object, as described by Newton's second law of motion (F = ma). The force exerted is directly proportional to the mass of the object and the acceleration it experiences.
Arrows represent the direction and magnitude of the force. The direction is indicated by the arrow's orientation, while the length of the arrow indicates the magnitude of the force.
A reduction in surface wind speed will have a minor effect on the Coriolis force. The Coriolis force is primarily influenced by the Earth's rotation and the object's velocity, not the speed of the wind. Therefore, a decrease in wind speed will not significantly alter the Coriolis force.
The effect that a reduction in surface wind speed will have on the Coriolis force is to reduce the effect of the Coriolis force. Winds blowing at higher speeds are pulled on more by the Coriolis force, which somewhat alters the direction in which they blow.
The Coriolis force was described by French mathematician and engineer Gaspard-Gustave de Coriolis in 1835. He formulated the concept to explain the deviations in the motion of objects on a rotating surface.