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Fictitious force
Fictitious force
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The Coriolis force is an example of a fictitious force. The camera on the right is rotating, so it represents a non-inertial reference frame. This is why the marble seems to be moved by a force.

A fictitious force, also known as an inertial force or pseudo-force, is a force that appears to act on an object when its motion is described or experienced from a non-inertial frame of reference. Unlike real forces, which result from physical interactions between objects, fictitious forces occur due to the acceleration of the observer’s frame of reference rather than any actual force acting on a body. These forces are necessary for describing motion correctly within an accelerating frame, ensuring that Newton's second law of motion remains applicable.[1][2]

Common examples of fictitious forces include the centrifugal force, which appears to push objects outward in a rotating system; the Coriolis force, which affects objects moving relative to the rotating frame, such as a wind parcel on Earth; and the Euler force, which arises when a rotating system changes its angular velocity (i.e., due to angular acceleration).

While these forces are not real in the sense of being caused by physical interactions, they are essential for accurately analyzing motion within accelerating reference frames, particularly in disciplines such as classical mechanics, meteorology, and astrophysics. Fictitious forces play a crucial role in understanding everyday phenomena, such as weather patterns influenced by the Coriolis effect and the perceived weightlessness experienced by astronauts in free-fall orbits. They are also fundamental in engineering applications, including navigation systems and rotating machinery.

According to general relativity theory we perceive gravitational force when spacetime is bending near heavy objects, so even this might be called a fictitious force.

Measurable examples of fictitious forces

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Passengers in a vehicle accelerating in the forward direction may perceive they are acted upon by a force moving them into the direction of the backrest of their seats for instance. An example in a rotating reference frame may be the impression that it is a force which seems to move objects outward toward the rim of a centrifuge or carousel.

The fictitious force called a pseudo force might also be referred to as a body force. It is due to an object's inertia when the reference frame does not move inertially any more but begins to accelerate relative to the free object. In terms of the example of the passenger vehicle, a pseudo force seems to be active just before the body touches the backrest of the seat in the car. A person in the car leaning forward first moves a bit backward in relation to the already accelerating car before touching the backrest. The motion in this short period seems to be the result of a force on the person; i.e., it is a pseudo force. A pseudo force does not arise from any physical interaction between two objects, such as electromagnetism or contact forces. It is only a consequence of the acceleration of the physical object the non-inertial reference frame is connected to, i.e. the vehicle in this case. From the viewpoint of the respective accelerating frame, an acceleration of the inert object appears to be present, apparently requiring a "force" for this to have happened.

As stated by Iro:[3]

Such an additional force due to nonuniform relative motion of two reference frames is called a pseudo-force.

— Harald Iro in A Modern Approach to Classical Mechanics p. 180

The pseudo force on an object arises as an imaginary influence when the frame of reference used to describe the object's motion is accelerating compared to a non-accelerating frame. The pseudo force "explains", using Newton's second law mechanics, why an object does not follow Newton's second law and "floats freely" as if weightless. As a frame may accelerate in any arbitrary way, so may pseudo forces also be as arbitrary (but only in direct response to the acceleration of the frame). An example of a pseudo force as defined by Iro is the Coriolis force, maybe better to be called: the Coriolis effect.[4][5][6] The gravitational force would also be a fictitious force (pseudo force) in a field model in which particles distort spacetime due to their mass, such as in the theory of general relativity.

Assuming Newton's second law in the form F = ma, fictitious forces are always proportional to the mass m.

The fictitious force that has been called an inertial force[7][8][9] is also referred to as a d'Alembert force,[10][11] or sometimes as a pseudo force.[12] D'Alembert's principle is just another way of formulating Newton's second law of motion. It defines an inertial force as the negative of the product of mass times acceleration, just for the sake of easier calculations.

(A d'Alembert force is not to be confused with a contact force arising from the physical interaction between two objects, which is the subject of Newton's third law – 'action is reaction'.[13][14] In terms of the example of the passenger vehicle above, a contact force emerges when the body of the passenger touches the backrest of the seat in the car. It is present for as long as the car is accelerated.)

Four fictitious forces have been defined for frames accelerated in commonly occurring ways:

Background

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The role of fictitious forces in Newtonian mechanics is described by Tonnelat:[16]

For Newton, the appearance of acceleration always indicates the existence of absolute motion – absolute motion of matter where real forces are concerned; absolute motion of the reference system, where so-called fictitious forces, such as inertial forces or those of Coriolis, are concerned.

— Marie-Antoinette Tonnelat in The Principles of Electromagnetic Theory and Relativity, p.113

Fictitious forces arise in classical mechanics and special relativity in all non-inertial frames. Inertial frames are privileged over non-inertial frames because they do not have physics whose causes are outside of the system, while non-inertial frames do. Fictitious forces, or physics whose cause is outside of the system, are no longer necessary in general relativity, since these physics are explained with the geodesics of spacetime: "The field of all possible space-time null geodesics or photon paths unifies the absolute local non-rotation standard throughout space-time.".[17]

On Earth

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The surface of the Earth is a rotating reference frame. To solve classical mechanics problems exactly in an Earthbound reference frame, three fictitious forces must be introduced: the Coriolis force, the centrifugal force (described below) and the Euler force. The Euler force is typically ignored because the variations in the angular velocity of the rotating surface of the Earth are usually insignificant. Both of the other fictitious forces are weak compared to most typical forces in everyday life, but they can be detected under careful conditions.

For example, Léon Foucault used his Foucault pendulum to show that the Coriolis force results from the Earth's rotation. If the Earth were to rotate twenty times faster (making each day only ~72 minutes long), people could easily get the impression that such fictitious forces were pulling on them, as on a spinning carousel. People in temperate and tropical latitudes would, in fact, need to hold on, in order to avoid being launched into orbit by the centrifugal force.

When moving along the equator in a ship heading in an easterly direction, objects appear to be slightly lighter than on the way back. This phenomenon has been observed and is called the Eötvös effect.

Detection of non-inertial reference frame

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Observers inside a closed box that is moving with a constant velocity cannot detect their own motion; however, observers within an accelerating reference frame can detect that they are in a non-inertial reference frame from the fictitious forces that arise. For example, for straight-line acceleration Vladimir Arnold presents the following theorem:[18]

In a coordinate system K which moves by translation relative to an inertial system k, the motion of a mechanical system takes place as if the coordinate system were inertial, but on every point of mass m an additional "inertial force" acted: F = −ma, where a is the acceleration of the system K.

Other accelerations also give rise to fictitious forces, as described mathematically below. The physical explanation of motions in an inertial frame is the simplest possible, requiring no fictitious forces: fictitious forces are zero, providing a means to distinguish inertial frames from others.[19]

An example of the detection of a non-inertial, rotating reference frame is the precession of a Foucault pendulum. In the non-inertial frame of the Earth, the fictitious Coriolis force is necessary to explain observations. In an inertial frame outside the Earth, no such fictitious force is necessary.

Example concerning Circular motion

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In the inertial frame of reference (upper part of the picture), the black ball moves in a straight line. However, the observer (brown dot) who is standing in the rotating/non-inertial frame of reference (lower part of the picture) sees the object as following a curved path due to the Coriolis or centrifugal forces present in this frame.

The effect of a fictitious force also occurs when a car takes the bend. Observed from a non-inertial frame of reference attached to the car, the fictitious force called the centrifugal force appears. As the car enters a left turn, a suitcase first on the left rear seat slides to the right rear seat and then continues until it comes into contact with the closed door on the right. This motion marks the phase of the fictitious centrifugal force as it is the inertia of the suitcase which plays a role in this piece of movement. It may seem that there must be a force responsible for this movement, but actually, this movement arises because of the inertia of the suitcase, which is (still) a 'free object' within an already accelerating frame of reference. After the suitcase has come into contact with the closed door of the car, the situation with the emergence of contact forces becomes current. The centripetal force on the car is now also transferred to the suitcase and the situation of Newton's third law comes into play, with the centripetal force as the action part and with the so-called reactive centrifugal force as the reaction part. The reactive centrifugal force is also due to the inertia of the suitcase. Now however the inertia appears in the form of a manifesting resistance to a change in its state of motion. [20]

Suppose a few miles further the car is moving at constant speed travelling a roundabout, again and again, then the occupants will feel as if they are being pushed to the outside of the vehicle by the (reactive) centrifugal force, away from the centre of the turn.

The situation can be viewed from inertial as well as from non-inertial frames.

  • From the viewpoint of an inertial reference frame stationary with respect to the road, the car is accelerating toward the centre of the circle. It is accelerating, because the direction of the velocity is changing, despite the car having constant speed. This inward acceleration is called centripetal acceleration, it requires a centripetal force to maintain the circular motion. This force is exerted by the ground upon the wheels, in this case, from the friction between the wheels and the road.[21] The car is accelerating, due to the unbalanced force, which causes it to move in a circle. (See also banked turn.)
  • From the viewpoint of a rotating frame, moving with the car, a fictitious centrifugal force appears to be present pushing the car toward the outside of the road (and pushing the occupants toward the outside of the car). The centrifugal force balances the friction between wheels and the road, making the car stationary in this non-inertial frame.

A classic example of a fictitious force in circular motion is the experiment of rotating spheres tied by a cord and spinning around their centre of mass. In this case, the identification of a rotating, non-inertial frame of reference can be based upon the vanishing of fictitious forces. In an inertial frame, fictitious forces are not necessary to explain the tension in the string joining the spheres. In a rotating frame, Coriolis and centrifugal forces must be introduced to predict the observed tension.

In the rotating reference frame perceived on the surface of the Earth, a centrifugal force reduces the apparent force of gravity by about one part in a thousand, depending on latitude. This reduction is zero at the poles, maximum at the equator.

The fictitious Coriolis force, which is observed in rotational frames, is ordinarily visible only in very large-scale motion like the projectile motion of long-range guns or the circulation of the Earth's atmosphere (see Rossby number). Neglecting air resistance, an object dropped from a 50-meter-high tower at the equator will fall 7.7 millimetres eastward of the spot below where it is dropped because of the Coriolis force.[22]

Fictitious forces and work

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Fictitious forces can be considered to do work, provided that they move an object on a trajectory that changes its energy from potential to kinetic. For example, consider some persons in rotating chairs holding a weight in their outstretched hands. If they pull their hand inward toward their body, from the perspective of the rotating reference frame, they have done work against the centrifugal force. When the weight is let go, it spontaneously flies outward relative to the rotating reference frame, because the centrifugal force does work on the object, converting its potential energy into kinetic. From an inertial viewpoint, of course, the object flies away from them because it is suddenly allowed to move in a straight line. This illustrates that the work done, like the total potential and kinetic energy of an object, can be different in a non-inertial frame than in an inertial one.

Gravity as a fictitious force

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The notion of "fictitious force" also arises in Einstein's general theory of relativity.[23][24] All fictitious forces are proportional to the mass of the object upon which they act, which is also true for gravity.[25][26] This led Albert Einstein to wonder whether gravity could be modeled as a fictitious force. He noted that a freefalling observer in a closed box would not be able to detect the force of gravity; hence, freefalling reference frames are equivalent to inertial reference frames (the equivalence principle). Developing this insight, Einstein formulated a theory with gravity as a fictitious force, and attributed the apparent acceleration due to gravity to the curvature of spacetime. This idea underlies Einstein's theory of general relativity. See the Eötvös experiment.

Mathematical derivation of fictitious forces

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Figure 2: An object located at xA in inertial frame A is located at location xB in accelerating frame B. The origin of frame B is located at XAB in frame A. The orientation of frame B is determined by the unit vectors along its coordinate directions, uj with j = 1, 2, 3. Using these axes, the coordinates of the object according to frame B are xB = ( x1, x2, x3).

General derivation

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Many problems require use of noninertial reference frames, for example, those involving satellites[28][29] and particle accelerators.[30] Figure 2 shows a particle with mass m and position vector xA(t) in a particular inertial frame A. Consider a non-inertial frame B whose origin relative to the inertial one is given by XAB(t). Let the position of the particle in frame B be xB(t). What is the force on the particle as expressed in the coordinate system of frame B?[31][32]

To answer this question, let the coordinate axis in B be represented by unit vectors uj with j any of { 1, 2, 3 } for the three coordinate axes. Then

The interpretation of this equation is that xB is the vector displacement of the particle as expressed in terms of the coordinates in frame B at the time t. From frame A the particle is located at:

As an aside, the unit vectors { uj } cannot change magnitude, so derivatives of these vectors express only rotation of the coordinate system B. On the other hand, vector XAB simply locates the origin of frame B relative to frame A, and so cannot include rotation of frame B.

Taking a time derivative, the velocity of the particle is:

The second term summation is the velocity of the particle, say vB as measured in frame B. That is:

The interpretation of this equation is that the velocity of the particle seen by observers in frame A consists of what observers in frame B call the velocity, namely vB, plus two extra terms related to the rate of change of the frame-B coordinate axes. One of these is simply the velocity of the moving origin vAB. The other is a contribution to velocity due to the fact that different locations in the non-inertial frame have different apparent velocities due to the rotation of the frame; a point seen from a rotating frame has a rotational component of velocity that is greater the further the point is from the origin.

To find the acceleration, another time differentiation provides:

Using the same formula already used for the time derivative of xB, the velocity derivative on the right is:

Consequently,

The interpretation of this equation is as follows: the acceleration of the particle in frame A consists of what observers in frame B call the particle acceleration aB, but in addition, there are three acceleration terms related to the movement of the frame-B coordinate axes: one term related to the acceleration of the origin of frame B, namely aAB, and two terms related to the rotation of frame B. Consequently, observers in B will see the particle motion as possessing "extra" acceleration, which they will attribute to "forces" acting on the particle, but which observers in A say are "fictitious" forces arising simply because observers in B do not recognize the non-inertial nature of frame B.

The factor of two in the Coriolis force arises from two equal contributions: (i) the apparent change of an inertially constant velocity with time because rotation makes the direction of the velocity seem to change (a dvB/dt term) and (ii) an apparent change in the velocity of an object when its position changes, putting it nearer to or further from the axis of rotation (the change in due to change in x j ).

To put matters in terms of forces, the accelerations are multiplied by the particle mass:

The force observed in frame B, FB = maB is related to the actual force on the particle, FA, by where:

Thus, problems may be solved in frame B by assuming that Newton's second law holds (with respect to quantities in that frame) and treating Ffictitious as an additional force.[18][33][34]

Below are a number of examples applying this result for fictitious forces. More examples can be found in the article on centrifugal force.

Rotating coordinate systems

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A common situation in which noninertial reference frames are useful is when the reference frame is rotating. Because such rotational motion is non-inertial, due to the acceleration present in any rotational motion, a fictitious force can always be invoked by using a rotational frame of reference. Despite this complication, the use of fictitious forces often simplifies the calculations involved.

To derive expressions for the fictitious forces, derivatives are needed for the apparent time rate of change of vectors that take into account time-variation of the coordinate axes. If the rotation of frame 'B' is represented by a vector Ω pointed along the axis of rotation with the orientation given by the right-hand rule, and with magnitude given by

then the time derivative of any of the three unit vectors describing frame B is[33][35] and as is verified using the properties of the vector cross product. These derivative formulas now are applied to the relationship between acceleration in an inertial frame, and that in a coordinate frame rotating with time-varying angular velocity ω(t). From the previous section, where subscript A refers to the inertial frame and B to the rotating frame, setting aAB = 0 to remove any translational acceleration, and focusing on only rotational properties (see Eq. 1): Collecting terms, the result is the so-called acceleration transformation formula:[36]

The physical acceleration aA due to what observers in the inertial frame A call real external forces on the object is, therefore, not simply the acceleration aB seen by observers in the rotational frame B, but has several additional geometric acceleration terms associated with the rotation of B. As seen in the rotational frame, the acceleration aB of the particle is given by rearrangement of the above equation as:

The net force upon the object according to observers in the rotating frame is FB = maB. If their observations are to result in the correct force on the object when using Newton's laws, they must consider that the additional force Ffict is present, so the end result is FB = FA + Ffict. Thus, the fictitious force used by observers in B to get the correct behaviour of the object from Newton's laws equals:

Here, the first term is the Coriolis force,[37] the second term is the centrifugal force,[38] and the third term is the Euler force.[39][40]

Orbiting coordinate systems

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Figure 3: An orbiting but fixed orientation coordinate system B, shown at three different times. The unit vectors uj, j = 1, 2, 3 do not rotate, but maintain a fixed orientation, while the origin of the coordinate system B moves at constant angular rate ω about the fixed axis Ω. Axis Ω passes through the origin of inertial frame A, so the origin of frame B is a fixed distance R from the origin of inertial frame A.

As a related example, suppose the moving coordinate system B rotates with a constant angular speed ω in a circle of radius R about the fixed origin of inertial frame A, but maintains its coordinate axes fixed in orientation, as in Figure 3. The acceleration of an observed body is now (see Eq. 1): where the summations are zero inasmuch as the unit vectors have no time dependence. The origin of the system B is located according to frame A at: leading to a velocity of the origin of frame B as: leading to an acceleration of the origin of B given by: Because the first term, which is is of the same form as the normal centrifugal force expression: it is a natural extension of standard terminology (although there is no standard terminology for this case) to call this term a "centrifugal force". Whatever terminology is adopted, the observers in frame B must introduce a fictitious force, this time due to the acceleration from the orbital motion of their entire coordinate frame, that is radially outward away from the centre of rotation of the origin of their coordinate system: and of magnitude:

This "centrifugal force" has differences from the case of a rotating frame. In the rotating frame the centrifugal force is related to the distance of the object from the origin of frame B, while in the case of an orbiting frame, the centrifugal force is independent of the distance of the object from the origin of frame B, but instead depends upon the distance of the origin of frame B from its centre of rotation, resulting in the same centrifugal fictitious force for all objects observed in frame B.

Orbiting and rotating

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Figure 4: An orbiting coordinate system B similar to Figure 3, but in which unit vectors uj, j = 1, 2, 3 rotate to face the rotational axis, while the origin of the coordinate system B moves at constant angular rate ω about the fixed axis Ω.

As a combination example, Figure 4 shows a coordinate system B that orbits inertial frame A as in Figure 3, but the coordinate axes in frame B turn so unit vector u1 always points toward the centre of rotation. This example might apply to a test tube in a centrifuge, where vector u1 points along the axis of the tube toward its opening at its top. It also resembles the Earth–Moon system, where the Moon always presents the same face to the Earth.[41] In this example, unit vector u3 retains a fixed orientation, while vectors u1, u2 rotate at the same rate as the origin of coordinates. That is, Hence, the acceleration of a moving object is expressed as (see Eq. 1): where the angular acceleration term is zero for the constant rate of rotation. Because the first term, which is is of the same form as the normal centrifugal force expression: it is a natural extension of standard terminology (although there is no standard terminology for this case) to call this term the "centrifugal force". Applying this terminology to the example of a tube in a centrifuge, if the tube is far enough from the center of rotation, |XAB| = R ≫ |xB|, all the matter in the test tube sees the same acceleration (the same centrifugal force). Thus, in this case, the fictitious force is primarily a uniform centrifugal force along the axis of the tube, away from the centre of rotation, with a value |Ffict| = ω2 R, where R is the distance of the matter in the tube from the centre of the centrifuge. It is the standard specification of a centrifuge to use the "effective" radius of the centrifuge to estimate its ability to provide centrifugal force. Thus, the first estimate of centrifugal force in a centrifuge can be based upon the distance of the tubes from the centre of rotation, and corrections applied if needed.[42][43]

Also, the test tube confines motion to the direction down the length of the tube, so vB is opposite to u1 and the Coriolis force is opposite to u2, that is, against the wall of the tube. If the tube is spun for a long enough time, the velocity vB drops to zero as the matter comes to an equilibrium distribution. For more details, see the articles on sedimentation and the Lamm equation.

A related problem is that of centrifugal forces for the Earth–Moon–Sun system, where three rotations appear: the daily rotation of the Earth about its axis, the lunar-month rotation of the Earth–Moon system about its centre of mass, and the annual revolution of the Earth–Moon system about the Sun. These three motions influence the tides.[44]

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Figure 5: Crossing a rotating carousel walking at a constant speed from the centre of the carousel to its edge, a spiral is traced out in the inertial frame, while a simple straight radial path is seen in the frame of the carousel.

Figure 5 shows another example comparing the observations of an inertial observer with those of an observer on a rotating carousel.[45] The carousel rotates at a constant angular velocity represented by the vector Ω with magnitude ω, pointing upward according to the right-hand rule. A rider on the carousel walks radially across it at a constant speed, in what appears to the walker to be the straight line path inclined at 45° in Figure 5. To the stationary observer, however, the walker travels a spiral path. The points identified on both paths in Figure 5 correspond to the same times spaced at equal time intervals. We ask how two observers, one on the carousel and one in an inertial frame, formulate what they see using Newton's laws.

Inertial observer

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The observer at rest describes the path followed by the walker as a spiral. Adopting the coordinate system shown in Figure 5, the trajectory is described by r(t): where the added π/4 sets the path angle at 45° to start with (just an arbitrary choice of direction), uR is a unit vector in the radial direction pointing from the centre of the carousel to the walker at the time t. The radial distance R(t) increases steadily with time according to: with s the speed of walking. According to simple kinematics, the velocity is then the first derivative of the trajectory: with uθ a unit vector perpendicular to uR at time t (as can be verified by noticing that the vector dot product with the radial vector is zero) and pointing in the direction of travel. The acceleration is the first derivative of the velocity: The last term in the acceleration is radially inward of magnitude ω2 R, which is therefore the instantaneous centripetal acceleration of circular motion.[46] The first term is perpendicular to the radial direction, and pointing in the direction of travel. Its magnitude is 2, and it represents the acceleration of the walker as the edge of the carousel is neared, and the arc of the circle travelled in a fixed time increases, as can be seen by the increased spacing between points for equal time steps on the spiral in Figure 5 as the outer edge of the carousel is approached.

Applying Newton's laws, multiplying the acceleration by the mass of the walker, the inertial observer concludes that the walker is subject to two forces: the inward radially directed centripetal force and another force perpendicular to the radial direction that is proportional to the speed of the walker.

Rotating observer

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The rotating observer sees the walker travel a straight line from the centre of the carousel to the periphery, as shown in Figure 5. Moreover, the rotating observer sees that the walker moves at a constant speed in the same direction, so applying Newton's law of inertia, there is zero force upon the walker. These conclusions do not agree with the inertial observer. To obtain agreement, the rotating observer has to introduce fictitious forces that appear to exist in the rotating world, even though there is no apparent reason for them, no apparent gravitational mass, electric charge or what have you, that could account for these fictitious forces.

To agree with the inertial observer, the forces applied to the walker must be exactly those found above. They can be related to the general formulas already derived, namely: In this example, the velocity seen in the rotating frame is: with uR a unit vector in the radial direction. The position of the walker as seen on the carousel is: and the time derivative of Ω is zero for uniform angular rotation. Noticing that and we find: To obtain a straight-line motion in the rotating world, a force exactly opposite in sign to the fictitious force must be applied to reduce the net force on the walker to zero, so Newton's law of inertia will predict a straight line motion, in agreement with what the rotating observer sees. The fictitious forces that must be combated are the Coriolis force (first term) and the centrifugal force (second term). (These terms are approximate.[47]) By applying forces to counter these two fictitious forces, the rotating observer ends up applying exactly the same forces upon the walker that the inertial observer predicted were needed.

Because they differ only by the constant walking velocity, the walker and the rotational observer see the same accelerations. From the walker's perspective, the fictitious force is experienced as real, and combating this force is necessary to stay on a straight line radial path holding a constant speed. It is like battling a crosswind while being thrown to the edge of the carousel. [48]

Observation

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Notice that this kinematical discussion does not delve into the mechanism by which the required forces are generated. That is the subject of kinetics. In the case of the carousel, the kinetic discussion would involve perhaps a study of the walker's shoes and the friction they need to generate against the floor of the carousel, or perhaps the dynamics of skateboarding if the walker switched to travel by skateboard. Whatever the means of travel across the carousel, the forces calculated above must be realized. A very rough analogy is heating your house: you must have a certain temperature to be comfortable, but whether you heat by burning gas or by burning coal is another problem. Kinematics sets the thermostat, kinetics fires the furnace.

See also

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References

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Further reading

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
A fictitious force, also known as a pseudo-force or inertial force, is an apparent force that seems to act upon an object in a —such as one that is accelerating or rotating—but originates solely from the motion of the observer's frame rather than any physical interaction between the object and its environment. These forces are introduced to make applicable in such frames, where they would otherwise appear violated, and they always act in proportion to the object's and the frame's . In , fictitious forces distinguish themselves from real forces, which have identifiable physical sources like or and corresponding reaction forces as per Newton's third law. A key criterion for identifying a fictitious force is the absence of a reaction force; for instance, in a linearly accelerating , a passenger feels pushed backward, but no external agent pushes them— the effect stems from the frame's acceleration. Prominent examples include the , which appears to push objects outward in a rotating frame like a merry-go-round, actually resulting from the object's resisting the curved path. Another is the , which causes moving objects in a rotating frame—such as a thrown on a spinning platform—to deflect perpendicular to their , influencing phenomena like the rotation of hurricanes (counterclockwise in the and clockwise in the Southern). Fictitious forces play a crucial role in practical applications and geophysical contexts, where Earth's slight rotation introduces subtle effects despite its near-inertial nature. For example, centrifuges exploit the to separate substances by , while the Coriolis effect guides long-range ballistics and ocean current patterns. In non-inertial frames, the effective force on an object is the vector sum of real forces and fictitious ones, allowing consistent predictions of motion; however, transforming to an inertial frame eliminates these artifacts, revealing only genuine interactions.

Introduction and Background

Definition and Historical Context

Fictitious forces, also known as pseudo-forces or inertial forces, are apparent forces that emerge when analyzing the motion of objects within a . These forces lack a tangible physical source, such as the interactions underlying or , and instead arise due to the or of the observer's frame relative to an inertial one. In such frames, the observed deviations from straight-line motion at constant speed—contrary to Newton's —necessitate the introduction of these fictitious terms to restore consistency with Newtonian mechanics. Newton's laws of motion hold strictly only in inertial reference , where no net external forces act on objects at rest or in uniform motion, and is proportional to applied forces. Non-inertial frames violate this by introducing extraneous accelerations, requiring fictitious forces to account for the apparent motion without altering the underlying physics. This distinction underscores that fictitious forces are mathematical artifacts, not real interactions, enabling the extension of Newtonian analysis to accelerated or rotating systems. The origins of concepts related to fictitious forces trace back to the 17th century, with introducing the term "" in 1659 to describe the apparent outward tendency of rotating bodies, deriving its mathematical form for uniform . built on this in his (1687), incorporating centrifugal effects into his theory of absolute space and motion; he used the rotating bucket experiment to demonstrate , treating such effects as real manifestations relative to absolute space rather than frame-dependent artifacts. Newton's framework established the equivalence of inertial frames moving uniformly relative to one another and laid essential groundwork for later analyses of apparent forces in accelerated systems. The explicit recognition of fictitious (or inertial) forces as corrections for non-inertial frames emerged in the , notably with Jean le Rond d'Alembert's 1743 principle, which introduced inertial forces to reformulate Newton's second law for constrained or accelerating motions. Leonhard Euler further developed these ideas in the context of rotating systems, systematically incorporating centrifugal effects into the dynamics of rigid bodies and fluids, as seen in his contributions to the for rotating machinery. By the late , critiqued Newtonian absolute space, proposing that and rotational effects arise from interactions with distant matter in the , influencing Albert Einstein's development of . Einstein, drawing on , reinterpreted rotation—and the associated fictitious forces—as relative to the cosmic distribution of mass, integrating them into a geometry where such forces reflect deviations rather than isolated frame artifacts. This perspective marked a profound shift, linking fictitious forces to broader gravitational phenomena.

Inertial vs. Non-Inertial Frames

In physics, an inertial reference frame is defined as one that moves with constant velocity relative to the distant stars, often referred to as the "," where hold exactly without the need for additional modifications. In such frames, the acceleration of an object is directly proportional to the net real force acting on it, as described by Newton's second law, F=ma\mathbf{F} = m \mathbf{a}, with no extraneous terms required to explain observed motions. This uniformity ensures that all frames moving at constant velocity relative to one inertial frame are themselves inertial, forming a class of equivalent reference systems under relativity. In contrast, a undergoes , either linear or rotational, relative to an inertial frame, necessitating the introduction of fictitious forces—also known as pseudo-forces—to reconcile the observed motions with Newton's laws. These additional terms, such as those arising from linear or , appear as effective forces in the within the non-inertial frame but have no physical origin in terms of interactions between objects. For instance, in a linearly accelerating frame, a pseudo-force proportional to the frame's and opposite in direction must be added to each object's mass to maintain the form of Newton's second law. Rotational non-inertial frames similarly require terms accounting for the frame's and to describe dynamics accurately. The key distinction between inertial and non-inertial frames lies in the absence or presence of these pseudo-components: in inertial frames, all forces contributing to are genuine interactions, whereas in non-inertial frames, every apparent force includes contributions from the frame's motion, which must be explicitly subtracted or accounted for to recover true physical forces. This criterion allows physicists to identify the frame type by checking whether Newton's laws apply without amendments; deviations indicate non-inertial conditions. A brief example illustrating local inertial behavior is a free-falling in a uniform , where the frame accelerates downward at gg, making it equivalent to an inertial frame for observers inside, as the pseudo-force cancels the gravitational effect.

Observable Examples

Centrifugal Force in Rotation

In a , the manifests as an apparent outward force acting on objects, directing them away from the axis of rotation. For instance, passengers in a navigating a sharp experience this force as a sensation of being pushed toward the outside of the turn, where loose objects like a may slide across the if is insufficient to counteract it. This effect arises because the rotating frame accelerates relative to an inertial observer, altering the perceived motion of objects within it. Physically, the centrifugal force is a fictitious or inertial force, meaning it has no counterpart as a real interaction in an inertial reference frame; instead, it accounts for the tendency of objects to continue in straight-line motion due to , as described by Newton's . In the rotating frame, this apparent force enables the application of Newton's second law in a modified form, but from an external inertial perspective—such as that of a stationary observer watching the car turn—the outward motion is simply the result of unopposed without any additional acting. The force's existence is thus frame-dependent, real and measurable only to those within the non-inertial system. One measurable effect of the is its role in simulating through rotation, as seen in proposed designs for space stations where a habitat spins to produce an outward that mimics Earth's gravitational pull, allowing astronauts to walk on the inner surface without experiencing . In such systems, the force helps maintain physiological health by providing the necessary loading on bones and muscles during long-duration missions. Similarly, in rides like the —a vertical spinning where riders are pressed against after the floor drops—the centrifugal force balances the riders' weight, creating the illusion of defying gravity through the apparent outward push. The magnitude of the centrifugal force is proportional to the square of the of the and the distance of the object from the axis, increasing with faster spin rates or greater radial separation, which directly influences the intensity of effects in applications like these.

Coriolis Effect in Motion

The Coriolis effect manifests as a fictitious force that causes a deflection of the path of any object moving within a , such as Earth's surface. This deflection arises because the rotating frame imparts an apparent to both the object's and the axis of , altering the observed relative to the frame. For instance, in the case of a launched horizontally, such as an artillery shell, the path appears to curve due to this effect rather than following a straight line in the rotating frame. Similarly, the motion of air masses, like those forming , experiences this deflection on a planetary scale. The direction of this deflection depends on the sense of and the hemisphere in which the motion occurs. In the , where is counterclockwise when viewed from above the , the Coriolis effect deflects moving objects to the right of their vector for horizontal motion. In the , the deflection is to the left due to the opposite perspective of the . This rightward or leftward bias is consistent for all directions of motion and is independent of the object's orientation, provided it has a component of to the axis. The Coriolis effect is negligible on small spatial and temporal scales, such as in everyday activities like tossing a indoors, where the deflection is on the order of micrometers and overwhelmed by other forces like . However, it becomes significant for large-scale motions, such as long-range projectiles traveling tens of kilometers or atmospheric flows spanning continents, where deflections can amount to several kilometers. Notably, the effect is zero for objects stationary relative to the rotating frame, as there is no to deflect, and also vanishes for purely radial motion aligned with the rotation axis, where the velocity is parallel to the frame's angular vector.

Applications on Earth

Weather Patterns and Ocean Currents

In the Earth's atmosphere, the deflects moving air masses to the right in the and to the left in the , influencing large-scale wind patterns. This deflection is crucial for the formation of cyclones, where winds rotate counterclockwise around low-pressure centers in the and clockwise in the , and anticyclones, which exhibit the opposite rotations: clockwise in the North and counterclockwise in the South. These rotational patterns arise from the balance between the and forces, shaping global weather systems. Similarly, in the oceans, the drives the circulation of major current systems, such as gyres, which are large-scale loops of circulating water. In the , it deflects surface currents to the right, resulting in clockwise gyres like the that includes the warm , which flows northward along the U.S. East Coast before curving eastward toward . In the , deflection to the left produces counterclockwise gyres, such as the . A key aspect of this influence is , where wind-driven surface currents interact with friction and the , causing water layers to spiral downward: the surface layer moves nearly in the wind direction but at a 45-degree angle due to Coriolis deflection, with deeper layers rotating further until the net transport is 90 degrees to the right of the wind in the and to the left in the . This spiral effect, extending to about 100 meters depth, contributes to the piling of water in gyre centers and sustains their overall circulation. The magnitude of the Coriolis deflection is determined by Earth's angular velocity of approximately 7.29×1057.29 \times 10^{-5} rad/s, which provides the scale for these effects in both atmosphere and oceans; however, the force vanishes at the , where no deflection occurs, explaining the absence of gyres or formation there. In practice, these fictitious forces interact with real forces, particularly pressure gradients, to achieve geostrophic balance, where the counters the , resulting in steady flows parallel to isobars or sea surface contours in large-scale systems. This balance dominates mid-latitude circulations, enabling winds and currents to flow without significant acceleration.

Engineering and Transportation Examples

In engineering and transportation systems, fictitious forces such as the play a critical role in designing safe and efficient structures for curved paths. For navigating banked curves or roundabouts, the appears to push the outward, requiring the banking angle to provide a component of the normal force that counters this effect and supplies the necessary centripetal acceleration. This design minimizes reliance on , allowing higher speeds without skidding; for instance, seatbelts and suspension systems are engineered to withstand the resulting lateral loads, preventing displacement. Trains on curved tracks experience a similar centrifugal load, which engineers address through superelevation, or the outer rail higher to balance the outward fictitious force with a gravitational component, thereby reducing lateral wheel-rail forces and enhancing stability. This adjustment ensures that the net aligns with the track's , with typical superelevation values ranging from 0 to 6 inches depending on speed and , resulting in experienced g-forces of up to 0.1g laterally for passengers at design speeds. Measurable in accelerometers, these forces inform track maintenance to prevent derailments. In , particularly during long-haul , the Coriolis effect introduces a fictitious deflection that can accumulate over time, altering the perceived inertial path relative to ; this is compensated in inertial navigation systems using gyroscopes that account for the Coriolis to maintain accurate heading and trajectory. Such corrections are essential for transoceanic flights, where uncompensated errors could lead to positional drifts of several kilometers. Amusement park roller coasters incorporate fictitious forces into their design to create thrilling yet safe experiences, with engineers calculating the apparent centrifugal and gravitational forces in loops and curves to limit passenger g-forces to between - and . For example, in vertical loops, the track is shaped so the fictitious outward force at the top combines with to keep riders seated without excessive restraint loads, verified through dynamic simulations that ensure structural integrity under these apparent accelerations.

Detection Methods

Identifying Non-Inertial Frames

A reference frame is considered non-inertial if it undergoes relative to an inertial frame, where encompasses both linear changes in and rotational motion. In such frames, do not hold in their standard form without the introduction of fictitious forces to account for the observed deviations. A primary theoretical criterion for identifying a non-inertial frame involves observing the of a , which experiences no real forces. In an inertial frame, this particle moves in a straight line at constant , adhering to the principle of inertia. Conversely, in a non-inertial frame, the same particle's path appears curved or accelerated, necessitating fictitious forces to explain the motion within that frame. Indicators of a non-inertial frame include the presence of apparent forces acting on objects that are stationary relative to the frame. For instance, in an elevator accelerating upward, a plumb line suspended inside deviates from the true vertical direction, as if pulled by an additional force opposite to the acceleration. This deviation arises because the frame's acceleration imparts a fictitious force on the bob, mimicking the behavior of a real force. All reference fixed to the Earth's surface are approximately non-inertial due to the planet's about its axis and its orbital motion around the Sun, both of which introduce small but measurable . These effects require fictitious forces, such as the centrifugal and Coriolis forces, to describe motion accurately in terrestrial coordinates. The provides a deeper connection, stating that locally, the uniform of a non-inertial frame is indistinguishable from a homogeneous . In this sense, the apparent forces in an accelerating frame, like that of the , replicate the effects of , underscoring why non-inertial frames demand fictitious forces to reconcile observations with inertial physics.

Experimental Verification

One of the earliest and most direct experimental verifications of fictitious forces, particularly the Coriolis effect arising from , was provided by Léon Foucault's demonstration in 1851. In this setup, a long with a heavy bob is suspended to swing freely in a plane, but due to the in the rotating frame, the plane of oscillation over time. At the latitude of (approximately 48.8° N), the precession period is about 32 hours, corresponding to a rotation rate of roughly 11.25° per hour, confirming the Earth's diurnal rotation without relying on astronomical observations. Building on this, Foucault extended his work in with a gyroscope experiment, which further illustrated the effects of non-inertial frames. A , consisting of a rapidly spinning rotor with high , maintains its axis of rotation fixed in inertial space due to conservation of . When placed on , the gyroscope's axis appears to precess relative to the ground, directly revealing the planet's rotation and the absence of true forces causing such motion in an inertial frame. This device provided simpler, more portable evidence of fictitious forces compared to the , as frictional losses could be minimized to observe the effect over shorter times. Modern iterations of these experiments employ gyroscopes for enhanced precision, detecting minute variations in influenced by Coriolis and centrifugal effects in non-inertial . Ring gyroscopes, for instance, measure rotational rates by comparing counter-propagating laser beams in a closed loop, achieving sensitivities that track Earth's spin to within 10^{-9} radians per second and even diurnal fluctuations. These instruments confirm the fictitious nature of forces like the centrifugal term, as they align with inertial predictions without additional real forces. Space-based observations offer compelling verification by contrasting non-inertial and inertial frames. Satellites in , analyzed in an inertial frame centered on 's mass, follow paths under alone, with no observable acting outward to balance ; instead, the orbital motion provides the necessary centripetal . This absence of fictitious forces in free-fall inertial frames, as seen in missions like GPS satellites maintaining stable s without rotational corrections beyond tidal effects, underscores that such forces are artifacts of the observer's accelerating reference frame on ./04%3A_Rigid_Body_Rotation/4.09%3A_Centrifugal_and_Coriolis_Forces)

Mathematical Derivation

General Coordinate Transformation

In classical mechanics, the analysis of motion in non-inertial reference frames requires accounting for the frame's motion relative to an inertial frame, where Newton's laws hold without modification. The general coordinate transformation begins with the position vector of a particle, expressed as rin=R(t)+rnon(t)\mathbf{r}_\text{in} = \mathbf{R}(t) + \mathbf{r}_\text{non}(t), where rin\mathbf{r}_\text{in} is the position in the inertial frame, R(t)\mathbf{R}(t) is the position of the non-inertial frame's origin relative to the inertial origin, and rnon(t)\mathbf{r}_\text{non}(t) is the position relative to the non-inertial origin. This relation assumes the use of vector calculus to handle relative motion, including differentiation in rotating systems. To derive the acceleration, one first obtains the velocity transformation by differentiating the position relation, yielding vin=R˙+r˙non+ω×rnon\mathbf{v}_\text{in} = \dot{\mathbf{R}} + \dot{\mathbf{r}}_\text{non} + \boldsymbol{\omega} \times \mathbf{r}_\text{non}, where ω\boldsymbol{\omega} is the vector of the non-inertial frame relative to the inertial frame, and dots denote time derivatives in the inertial frame. Differentiating again provides the acceleration in the non-inertial frame: anon=ainR¨2ω×vrelω×(ω×rnon)ω˙×rnon,\mathbf{a}_\text{non} = \mathbf{a}_\text{in} - \ddot{\mathbf{R}} - 2 \boldsymbol{\omega} \times \mathbf{v}_\text{rel} - \boldsymbol{\omega} \times (\boldsymbol{\omega} \times \mathbf{r}_\text{non}) - \dot{\boldsymbol{\omega}} \times \mathbf{r}_\text{non}, where ain\mathbf{a}_\text{in} is the acceleration measured in the inertial frame, vrel=r˙non\mathbf{v}_\text{rel} = \dot{\mathbf{r}}_\text{non} is the relative velocity in the non-inertial frame, R¨\ddot{\mathbf{R}} is the acceleration of the non-inertial origin, and ω˙\dot{\boldsymbol{\omega}} is the time derivative of the angular velocity. This transformation encapsulates the effects of both translational and rotational motion of the frame. In the non-inertial frame, Newton's second law is modified by introducing fictitious forces to restore the form Ftotal=manon\mathbf{F}_\text{total} = m \mathbf{a}_\text{non}. The fictitious force is thus Ffict=m(R¨+2ω×vrel+ω×(ω×rnon)+ε×rnon),\mathbf{F}_\text{fict} = -m \left( \ddot{\mathbf{R}} + 2 \boldsymbol{\omega} \times \mathbf{v}_\text{rel} + \boldsymbol{\omega} \times (\boldsymbol{\omega} \times \mathbf{r}_\text{non}) + \boldsymbol{\varepsilon} \times \mathbf{r}_\text{non} \right), where ε=ω˙\boldsymbol{\varepsilon} = \dot{\boldsymbol{\omega}} denotes the of the frame. The term mR¨-m \ddot{\mathbf{R}} represents the translational fictitious force arising from the linear of the frame's origin, while the term involving ε\boldsymbol{\varepsilon} gives the , which manifests in cases of non-uniform . These components ensure that observed accelerations in the non-inertial frame can be interpreted using real forces plus these apparent ones.

Forces in Linearly Accelerating Frames

In a reference frame undergoing constant linear acceleration af\vec{a}_f
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