Circular Motion and Polar Coordinates - Complete Interactive Lesson
Part 1: Uniform Circular Motion
Uniform Circular Motion
Part 1 of 7 — Circular Motion
An object moving in a circle at constant speed is undergoing uniform circular motion. Despite constant speed, the object is accelerating because the direction of velocity is always changing.
Kinematics of Circular Motion
Quantity
Symbol
Formula
Period
T
Time for one revolution
Frequency
f
f=1/T
Angular velocity
ω
ω=2πf=2π/T
Speed
v
v=ωr
Arc length
s
s=rθ
Position Vector
For circular motion of radius r in the xy-plane:
r(t)=rcos(ωt)
Velocity Vector
v(t)=
The magnitude: ∣v∣=rω=v (constant). The direction is tangent to the circle — perpendicular to at every instant.
Centripetal Acceleration
Differentiating velocity:
a(t)=
Flat Curve: Car on a Turn
For a car of mass m on a flat circular turn of radius r:
The static friction provides the centripetal force:
fs=m
Part 1 Summary
Concept
Formula
Speed
v=ωr=2πr/T
Centripetal acceleration
a
Part 2: Centripetal Acceleration Derivation
Centripetal Acceleration Derivation
Part 2 of 7 — Circular Motion
On the AP Physics C exam, you may need to derive the centripetal acceleration formula from first principles. Let's build this up rigorously.
Method 1: Calculus Derivation
Start with position in polar-like Cartesian form:
r
Part 3: Banked Curves
Banked Curves
Part 3 of 7 — Circular Motion
Banked curves are inclined roadways designed so that the normal force provides some (or all) of the centripetal force needed for turning.
Frictionless Banked Curve
For a car on a banked curve (angle β) with no friction, the only forces are gravity and the normal force.
Vertical equilibrium:Ncosβ=mg
Radial (horizontal, toward center):
Part 4: Vertical Circles
Vertical Circles
Part 4 of 7 — Circular Motion
In vertical circular motion, gravity alternately aids and opposes the centripetal acceleration, making the analysis position-dependent. This is a favorite AP Physics C topic.
Forces at Key Positions
For a mass m on a string (or track) of radius r, moving at speed v:
At the Top
Both gravity and tension point toward the center (downward):
m
Part 5: Non-Uniform Circular Motion
Non-Uniform Circular Motion
Part 5 of 7 — Circular Motion
When an object moves in a circle with changing speed, it has both centripetal (radial) and tangential components of acceleration.
Decomposing Acceleration
a=a
Part 6: Problem-Solving Workshop
Problem-Solving Workshop
Part 6 of 7 — Circular Motion
Strategy for Circular Motion Problems
Step
Action
1
Identify the circular path and radius r
2
Draw FBD at the specified point
3
Establish radial direction (toward center) and tangential direction
4
Apply ∑F (radial)
Part 7: Review & Applications
Review & Applications
Part 7 of 7 — Circular Motion
Complete Topic Reference
Concept
Formula
Part
Speed
v=rω=2πr/T
1
Centripetal acceleration
x^
+
rsin(ωt)y^
dtdr
=
−rωsin(ωt)x^+
rωcos(ωt)y^
r
dtdv=
−rω2cos(ωt)x^−
rω2sin(ωt)y^
a(t)=−ω2r(t)
This acceleration points radially inward (toward the center) and has magnitude:
ac=ω2r=rv2
Important: Centripetal Force is NOT a New Force
Centripetal acceleration is caused by a real force (or combination of forces) directed toward the center. Common sources:
Situation
Centripetal Force
Ball on a string
Tension
Car on a curve
Static friction
Planet orbiting
Gravity
Electron in B-field
Magnetic force
Banked curve (no friction)
Normal force component
Newton's second law in the radial direction:
∑Fr=mac=mrv2=mω2r
AP Tip: Never list "centripetal force" as a force on a free body diagram. It's a net force requirement, not a separate force.
rv2
≤
μsmg
Maximum speed before skidding:
vmax=μsgr
Worked Example
A car takes a flat turn of radius 50 m. If μs=0.8 and g=10 m/s²:
vmax=0.8×10×50=400=20 m/s=72 km/h
Conical Pendulum
A mass m swings in a horizontal circle on a string of length L at angle θ from the vertical:
Vertical equilibrium:Tcosθ=mg
Radial (centripetal):Tsinθ=mω2r=mω2Lsinθ
Dividing: tanθ=ω2r/g=ω2Lsinθ/g
ω=Lcosθg
T=ω2π=2πgLcosθ
Notice: the period depends on the angle θ and string length L, but not on the mass.
c
=
v2/r=
ω2r
Centripetal force
Fc=mv2/r
Max speed (flat curve)
vmax=μsgr
Position vector
r(t)=rcos(ωt)x^+rsin(ωt)y^
Next up: Part 2 — Centripetal Acceleration Derivation, proving ac=v2/r rigorously using calculus.
(
t
)
=
rcos(ωt)x^+
rsin(ωt)y^
First derivative (velocity):
v=dtdr=−rωsin(ωt)x^+rωcos(ωt)y^
Second derivative (acceleration):
a=dtdv=−rω2cos(ωt)x^−rω2sin(ωt)y^
a=−ω2r
The magnitude: ∣a∣=ω2r. Since v=ωr:
ac=ω2r=rv2
The minus sign in a=−ω2r shows the acceleration is anti-parallel to r — it points toward the center.
Method 2: Geometric/Limit Derivation
Consider an object moving at constant speed v around a circle of radius r. In a small time Δt, the velocity vector rotates by angle Δθ=ωΔt.
Change in Velocity
The velocity vectors at times t and t+Δt both have magnitude v but differ in direction by Δθ.
Using the isoceles triangle formed by v(t), v, and :
∣Δv∣=2vsin(
For small Δθ: sin(Δθ/2)≈Δθ/2:
∣Δv∣≈vΔθ=vωΔt
Average Acceleration
∣aavg∣
Taking the limit Δt→0 gives the instantaneous acceleration:
ac=limΔt→0
Direction of Δv
As Δt→0, the direction of Δv becomes perpendicular to , which means it points . This completes the derivation.
Method 3: Polar Coordinates (Advanced)
In polar coordinates, the unit vectors r^ and θ^ rotate with the object:
r^=cosθx^+sinθy^θ^=−sinθx^+cosθ
Key derivatives:
dtdr^=θ
General Acceleration in Polar Coordinates
r=rr^
For uniform circular motion: r˙=0, r¨=0, (constant), :
a=−rω2r^
This is purely radial (centripetal), confirming ac=rω2=v2/r.
Why This Matters
The full polar coordinate acceleration formula is essential for non-uniform circular motion and orbital mechanics (Part 5 and beyond). The terms have physical meaning:
Term
Name
Direction
r¨−rθ˙2
Radial acceleration
Part 2 Summary
Three equivalent derivations of ac=v2/r:
Method
Key Step
Calculus
Differentiate r(t) twice
Geometric
Small-angle limit of Δv triangle
Polar coordinates
Use rotating unit vectors r^, θ^
Key Results:
a=−ω2r (always points toward center)
Next up: Part 3 — Banked Curves, applying centripetal force analysis to tilted roadways.
Nsinβ=rmv2
Dividing these equations:
tanβ=rgv2
vdesign=rgtanβ
This is the design speed — the one speed at which friction is unnecessary.
Worked Example
A highway curve has r=200 m and is banked at β=15°.
vdesign=200(10)tan15°=2000(0.268)=536=23.2 m/s≈83 km/h
Banked Curve with Friction
When the car's speed differs from the design speed, friction is needed.
Case 1: v>vdesign (Too Fast)
The car tends to slide up the bank. Friction acts down the incline (inward component helps centripetal force).
Vertical:Ncosβ−fsinβ=mg
Radial:Nsinβ+fcosβ=mv2/r
With f=μsN at the maximum speed:
vmax=rg⋅
Case 2: v<vdesign (Too Slow)
The car tends to slide down the bank. Friction acts up the incline.
vmin=rg⋅
If μs>tanβ, then vmin= (friction is strong enough to hold the car stationary on the bank).
Speed Range
vmin≤v≤vmax
This range widens with more friction and narrows to a single value (vdesign) as μs→0.
Detailed Derivation: vmax
Let's carefully derive the maximum speed formula. Forces on the car when going too fast (friction points down the bank):
Decompose forces along vertical and horizontal (centripetal):
Normal force: magnitude N, tilted at angle β from vertical.
Friction: magnitude f=μsN, along the bank surface (perpendicular to N), pointing down and inward.
Vertical equilibrium (ay=0):Ncosβ−μ
Horizontal (centripetal, ar=v2/r):N
Dividing:rgv2=
Dividing numerator and denominator by cosβ:
rgv2=
vmax=rg
Note: The formula resembles the tangent addition formula: tan(β+ϕ)=1−tanβtanϕ where . So where .
Part 3 Summary
Concept
Formula
Design speed (no friction)
v=rgtanβ
Max speed (with friction)
vmax=rg1−
Min speed (with friction)
vmin=rg
Compact form
v2=rgtan(β±ϕ), ϕ=arctan
Next up: Part 4 — Vertical Circles, where the centripetal force requirement changes with position.
g
+
Ttop=
rmvtop2
Ttop=rmvtop2−mg
At the Bottom
Tension points toward center (up); gravity points away (down):
Tbot−mg=rmvbot2
Tbot=rmvbot2+mg
At an Arbitrary Angle θ from Bottom
The component of gravity toward the center: mgcosθ (measuring θ from the bottom).
Wait — let's be precise. If θ is measured from the vertical (i.e., from the bottom position):
T−mgcosθ=rmv2
Minimum Speed at the Top
At the top of a vertical circle, the minimum speed occurs when the tension (or normal force) drops to zero. At that point, gravity alone provides the centripetal force:
mg=rmvmin2
vmin,top=gr
If the speed drops below this, the object leaves the circular path.
Minimum Speed at the Bottom (for Complete Loop)
Using energy conservation from bottom to top:
21mvbot2
With vtop=gr:
21vbot2=
vmin,bot=5gr
Tension Difference (Top vs Bottom)
Tbot−Ttop=
Using energy conservation: vbot2−vtop2=:
Tbot−Ttop=
This result is independent of the speed — the tension difference is always 6mg.
Vertical Circle on a Track (Normal Force)
For a ball rolling inside a circular loop track, the analysis is similar but the normal force replaces tension:
At the Top (Inside of Loop)
Ntop+mg=rmvtop2
(both N and mg point toward center)
At the Bottom (Inside of Loop)
Nbot−mg=rmv
The minimum speed condition at the top is the same (vmin=gr), when .
Outside of a Hump
For a car going over a hill of radius r:
mg−N=rmv2
N=mg−rmv2
The car leaves the road when N=0:
vleave=gr
Worked Example: Roller Coaster
A roller coaster starts from height h above the top of a circular loop of radius r. What is the normal force at the top of the loop?
By energy conservation from start to top of loop (height =2r):
mgh=21
At the top: N+mg=mvtop2/r
For N≥0: h≥5r/2. This means the starting height must be at least 2.5r above the bottom of the loop.
Part 4 Summary
Position
Centripetal Equation
Bottom
T−mg=mv2/r
Top
T+mg=mv2/r (string)
Top
N+mg=mv2/r (track)
Hill crest
mg−N=mv2/r
Key Result
Value
Min speed at top
gr
Min speed at bottom (full loop)
Next up: Part 5 — Non-Uniform Circular Motion, where both speed and direction change simultaneously.
c
r^
+
atθ^
Component
Direction
Formula
Cause
Centripetal ac
Toward center
v2/r
Changes direction
Tangential at
Along velocity
dv/dt
Changes speed
The total acceleration magnitude:
∣a∣=ac2+at2=(rv2)2+(
Angular Quantities
Linear
Angular
Relation
s (arc length)
θ (angle)
s=rθ
v (speed)
ω (angular velocity)
v=rω
at (tangential)
α (angular acceleration)
at=
α=dtdω=dt2d2θ
Full Polar Coordinate Analysis
Recall from Part 2, the general acceleration in polar coordinates:
a=(r¨−rθ˙2)r^+(rθ¨+2r˙θ˙)θ^
For circular motion (r = constant, r˙=0, r¨=0):
a=−rω2r
where ω=θ˙ and α=θ¨.
Example: Constant Angular Acceleration
A disk starts from rest and accelerates at α=2 rad/s². At t=3 s, a point at r=0.5 m from the center has:
ω=αt=6 rad/sv=rω=3 m/s
ac=rω2=0.5(36)=18 m/s
∣a∣=18
Angle of net acceleration from radial direction:ϕ=arctan(ac
The acceleration is almost purely centripetal because ω has built up substantially.
Energy and Work in Non-Uniform Circular Motion
The work-energy theorem applies component-by-component:
Centripetal force does no work (perpendicular to displacement).
Tangential force does work:Wt=∫Ftds=∫Ftrdθ
dtdK=F
Since centripetal force ⊥ velocity, only the tangential component changes the kinetic energy.
Power in Circular Motion
P=Ftv=Ftrω=τ
where τ=Ftr is the torque.
Worked Example: Vertical Circle with Gravity
A ball on a string swings in a vertical circle. At angle θ from the bottom:
Tangential acceleration (due to gravity):
at=−gsinθ
(negative because gravity decelerates the ball as it rises)
Speed as a function of angle (using energy conservation):
21mv2=
Centripetal acceleration at angle θ:ac=r
Tension at angle θ:T=rm
Part 5 Summary
Concept
Formula
Tangential acceleration
at=rα=dv/dt
Centripetal acceleration
ac=v2/r=rω2
Total acceleration
$
Only Ft does work
P=Ftv=
Vertical circle: v2(θ)
v02−
Next up: Part 6 — Problem-Solving Workshop with challenging circular motion problems.
r
=
mv2/r
5
Apply ∑Ft=mat (tangential, if non-uniform)
6
Use energy conservation to relate speeds at different positions
Problem 2: Conical Pendulum with Calculus
A mass m hangs from a string of length L and swings in a horizontal circle, making angle θ with the vertical. Show that the period is T=2πLcosθ/g and find dT/dθ.
Solution
From Part 1: ω=g/(Lcosθ), so:
T=ω2π=2π
Differentiating with respect to θ:
dθdT=2π⋅
dθdT=−πsinθ
dθdT=−
Since dT/dθ<0 for 0<θ<90°: as the angle increases, the period decreases. A wider swing means a faster revolution (shorter period).
For small angles: T≈2πL/g (simple pendulum period) — this is the maximum period.
Problem 3: Bead on a Rotating Hoop
A bead slides frictionlessly on a circular hoop of radius R that rotates about a vertical axis with angular speed ω. Find the equilibrium angle θ from the bottom of the hoop.
Setup
The bead is at angle θ from the bottom of the hoop. Its distance from the rotation axis is r=Rsinθ.
Forces on the bead:
Normal force N (perpendicular to the hoop, along the radius)
Gravity mg (downward)
Radial direction (toward rotation axis):Nsinθ=mω2Rsinθ
Vertical direction:Ncosθ=mg
From the radial equation (for θ=0):
N=mω2R
Substituting into vertical:
mω2Rcosθ=mg
cosθ=ω2Rg
Analysis
If ω2R>g (fast rotation): cosθ<1, so θ>. The bead rises.
This is a beautiful example of a bifurcation: the equilibrium jumps from θ=0 to a nonzero value at ω=ωc.
Workshop Summary
Key Problem Types
Type
Strategy
Flat curve
Friction = centripetal, vmax=μsgr
Banked curve
Resolve N and f into radial and vertical
Vertical circle
Energy for speeds, N2L for forces at each position
Conical pendulum
Vertical = mg, horizontal = centripetal
Rotating hoop
Bifurcation at ωc=g/R
Next up: Part 7 — Review & Applications, bringing it all together.
ac=v2/r=ω2r
1, 2
Position vector
r=rcos(ωt)x^+rsin(ωt)y^
2
acceleration derivation
a=−ω2r
2
Design speed (banked)
v=rgtanβ
3
Min speed at top of loop
vmin=gr
4
Min speed at bottom of loop
vmin=5gr
4
Tangential acceleration
at=rα=dv/dt
5
Total acceleration
$
\vec{a}
Application: Centrifuge
A centrifuge of radius R=0.15 m spins at n=3000 RPM.
Angular velocity:ω=2π×603000=100π≈314 rad/s
Centripetal acceleration:ac=ω2R=(100π)
In units of g:gac
Application: Car on a Banked Curve
An engineer designs a highway exit ramp with r=200 m for a design speed of 60 km/h (16.7 m/s).
Required banking angle:tanβ=rgv2=
With μs=0.7, maximum safe speed:v
Application: Kepler's Third Law (Preview)
For a planet of mass m orbiting a star of mass M in a circular orbit:
Gravitational force = centripetal force:r2GMm=rmv2
v=rGM
Period:T=v2πr=2πr
T2=GM4π
This is Kepler's Third Law: T2∝r3.
Geostationary Orbit
For a satellite orbiting with T=24 hours:
r=(4π2GMT
r=(4π2
This is about 35,800 km above Earth's surface.
🎉 Topic Complete: Circular Motion
You've mastered the full AP Physics C treatment of circular motion:
Part
Topic
Status
1
Uniform circular motion
✅
2
Centripetal acceleration derivation
✅
3
Banked curves
✅
4
Vertical circles
✅
5
Non-uniform circular motion
✅
6
Problem-solving workshop
✅
7
Review & applications
✅
Key Takeaway: Circular motion problems require (1) identifying the center and radius, (2) applying Newton's second law in the radial direction with ∑Fr=mv2/r, and (3) using energy conservation for speed relationships. The calculus-level content (derivations, polar coordinates, angular kinematics) is what distinguishes AP Physics C from AP Physics 1.
(
t
+
Δt)
Δv
2
Δθ
)
=
Δt∣Δv∣=
vω=
rv2
Δt∣Δv∣
=
vω=
rv2
v
radially inward
y
^
˙
θ^
=
ωθ^
dtdθ^=−θ˙r^=−ωr^
v=r˙r^+rθ˙θ^
a=(r¨−rθ˙2)r^+(rθ¨+2r˙θ˙)θ^
θ˙
=
ω
θ¨=0
r^
−rθ˙2
Centripetal acceleration
−r^
rθ¨
Tangential (angular) acceleration
θ^
2r˙θ˙
Coriolis term
θ^
v⊥a in UCM (constant speed)
v⋅a=0⟹∣v∣ is constant
1−μstanβ
tanβ+μs
1+μstanβ
tanβ−μs
0
s
N
sin
β
=
mg
N(cosβ−μssinβ)=mg
N=cosβ−μssinβmg
sin
β
+
μsNcosβ=
rmv2
N(sinβ+μscosβ)=rmv2
cosβ−μssinβsinβ+μscosβ
1−μstanβ
tanβ+μs
⋅
1−μstanβtanβ+μs
tanβ+tanϕ
tanϕ=μs
vmax2=rgtan(β+ϕ)
ϕ=arctan(μs)
μ
s
tan
β
tanβ+μs
1
+
μs
tan
β
tanβ−μs
μs
=
21mvtop2+
mg(2r)
21
g
r
+
2gr=
25gr
rm(vbot2−vtop2)
+
2mg
4
g
r
rm(4gr)
+
2mg=
4mg+
2mg=
6mg
bot2
Ntop=0
=
m(g−rv2)
m
vtop2
+
mg(2r)
vtop2=2g(h−2r)
N=rm⋅2g(h−2r)−mg=mg(r2h−5)
5gr
Tension difference (top vs bottom)
6mg
dt
dv
)
2
r
α
^
+
rαθ^
2
at=rα=0.5(2)=1 m/s2
2
+
12
=
325=
18.03 m/s2
at
)
=
arctan(181)≈
3.2°
⋅
v=
Ftv
ω
21
m
v02
−
mgr(1−
cosθ)
v2=v02−2gr(1−cosθ)
v2
=
rv02−
2g(1−
cosθ)
v2
+
mgcosθ=
rmv02−
2mg(1−
cosθ)+
mgcosθ
T=rmv02−mg(2−3cosθ)
τ
ω
2
g
r
(
1
−
cosθ)
gLcosθ
21
(gLcosθ)−1/2
⋅
g−Lsinθ
gcosθL
⋅
cosθ1
gLcos3θ
πLsinθ
0
If ω2R<g (slow rotation): cosθ>1 is impossible — the bead stays at the bottom (θ=0).