Kinematics Formulas to Know for AP Physics 1

What You Need to Know

Kinematics is the math of motion (position, velocity, acceleration) without worrying about forces. In AP Physics 1, most kinematics questions boil down to: choose a coordinate system, translate words/graphs into variables, then use the right constant-acceleration or 2D component equations.

Core quantities (with meanings)
  • Position xx (1D) or r\vec r (2D): where you are.
  • Displacement Δx=xx0\Delta x = x - x_0: change in position.
  • Velocity vv or v\vec v: how fast and which direction your position changes.
  • Acceleration aa or a\vec a: how fast and which direction your velocity changes.
The big idea you must internalize

If acceleration is constant, the “Big 4” kinematics equations apply. If acceleration is not constant, you rely on graphs, areas, and definitions (still algebra-based).

Constant acceleration is the default AP Physics 1 kinematics model
  • “Free fall” near Earth: ay=ga_y = -g where g9.8 m/s2g \approx 9.8\ \mathrm{m/s^2} (often rounded to 10 m/s210\ \mathrm{m/s^2}), direction downward.
  • Projectile motion (no air resistance):
    • ax=0a_x = 0
    • ay=ga_y = -g
    • Motion in xx and yy are linked only by **time** tt.

Step-by-Step Breakdown

Use this every time you see a kinematics problem.

  1. Choose a coordinate system and write sign conventions

    • Pick +x or +y directions intentionally (often up is +y).
    • Write what is positive/negative before plugging numbers.
  2. List knowns/unknowns (by component if 2D)
    Typical variables:

    • x0, x, Δxx_0,\ x,\ \Delta x
    • v0, vv_0,\ v
    • aa
    • tt
  3. Decide: constant acceleration or not?

    • If constant acceleration is stated or implied (free fall, constant braking, constant thrust): use the Big 4.
    • If you’re given a graph v(t)v(t) or a(t)a(t) and it’s piecewise: use slope/area relationships.
  4. If motion is 2D, split into components

    • v0x=v0cosθv_{0x} = v_0\cos\theta
    • v0y=v0sinθv_{0y} = v_0\sin\theta
    • Solve xx-direction and yy-direction separately, then recombine if needed.
  5. Pick the equation that avoids your “extra” unknown
    Example decision point:

    • Need vv but not tt? Use v2=v02+2aΔxv^2 = v_0^2 + 2a\Delta x.
    • Need Δx\Delta x and have tt? Use Δx=v0t+12at2\Delta x = v_0 t + \tfrac{1}{2}at^2.
  6. Check units + reasonableness

    • Times should be positive.
    • Speeds shouldn’t come out negative (negative belongs to velocity components).
    • In free fall, if up is positive, then aya_y should be negative.
Micro-worked example (method in action)

A ball is thrown upward with v0y=+12 m/sv_{0y} = +12\ \mathrm{m/s} from y0=0y_0 = 0. Find time to peak.
1) Choose up as +y, so ay=9.8 m/s2a_y = -9.8\ \mathrm{m/s^2}.
2) At peak, vy=0v_y = 0.
3) Use vy=v0y+aytv_y = v_{0y} + a_y t:

0=12+(9.8)tt1.22 s0 = 12 + (-9.8)t \Rightarrow t \approx 1.22\ \mathrm{s}


Key Formulas, Rules & Facts

Definitions (always true)
RelationshipFormulaNotes
Average velocityvavg=ΔxΔtv_{\text{avg}} = \dfrac{\Delta x}{\Delta t}Displacement over time interval. Can be negative.
Average speedspeedavg=total distanceΔt\text{speed}_{\text{avg}} = \dfrac{\text{total distance}}{\Delta t}Uses distance, never negative.
Average accelerationaavg=ΔvΔta_{\text{avg}} = \dfrac{\Delta v}{\Delta t}Change in velocity over time.
Constant-acceleration (1D) “Big 4”

Assume aa is constant.

FormulaWhen to useNotes
v=v0+atv = v_0 + atYou want vv after time ttGreat for free fall, braking, speeding up.
Δx=v0t+12at2\Delta x = v_0 t + \tfrac{1}{2}at^2You want displacement with timeMost-used displacement equation.
v2=v02+2aΔxv^2 = v_0^2 + 2a\Delta xNo time given/wantedWatch signs: aΔxa\Delta x can be negative.
Δx=(v+v0)2t\Delta x = \tfrac{(v+v_0)}{2}tYou know average velocity for constant aaBecause vavg=v+v02v_{\text{avg}} = \tfrac{v+v_0}{2} when aa is constant.
Free-fall shortcuts (vertical motion)

Take up as +y (common choice):

  • ay=ga_y = -g
  • vy=v0ygtv_y = v_{0y} - gt
  • Δy=v0yt12gt2\Delta y = v_{0y} t - \tfrac{1}{2}gt^2
  • vy2=v0y22gΔyv_y^2 = v_{0y}^2 - 2g\Delta y

Facts you use all the time:

  • At the top of a vertical toss: vy=0v_y = 0 (but aya_y is still g-g).
  • If it returns to the same height (no air resistance): time up = time down, and vlanding=vlaunch|v_{\text{landing}}| = |v_{\text{launch}}| (direction flips).
Projectile motion (2D, no air resistance)

Split into independent components.

ComponentAccelerationVelocityPosition
Horizontal xxax=0a_x = 0vx=v0xv_x = v_{0x}x=x0+v0xtx = x_0 + v_{0x}t
Vertical yyay=ga_y = -gvy=v0ygtv_y = v_{0y} - gty=y0+v0yt12gt2y = y_0 + v_{0y}t - \tfrac{1}{2}gt^2

Vector magnitude relationships:

  • Speed: v=vx2+vy2v = \sqrt{v_x^2 + v_y^2}
  • Launch components: v0x=v0cosθv_{0x} = v_0\cos\theta, v0y=v0sinθv_{0y} = v_0\sin\theta

Special results (only when launch and landing heights match):

  • Time of flight: T=2v0sinθgT = \dfrac{2v_0\sin\theta}{g}
  • Range: R=v02sin(2θ)gR = \dfrac{v_0^2\sin(2\theta)}{g}
  • Max height above launch: H=v02sin2θ2gH = \dfrac{v_0^2\sin^2\theta}{2g}

If launch and landing heights are different, do not use the “same-height” shortcut formulas. Use component kinematics with y(t)y(t) instead.

Motion graphs (the algebra-based superpower)
GraphSlope meansArea means
xx vs ttslope =v= varea has no standard meaning here
vv vs ttslope =a= aarea =Δx= \Delta x
aa vs ttslope has no standard AP1 meaningarea =Δv= \Delta v

For straight-line segments on graphs:

  • Average velocity on a time interval: vavg=ΔxΔtv_{\text{avg}} = \dfrac{\Delta x}{\Delta t}
  • For a linear v(t)v(t) segment: area is triangle/trapezoid geometry.
Relative motion (often a quick plug-in)
  • Relative velocity in 1D: vA/B=vAvBv_{A/B} = v_A - v_B
  • Relative position: xA/B=xAxBx_{A/B} = x_A - x_B
Uniform circular motion (kinematics of turning)

AP Physics 1 often treats this as kinematics + dynamics later. Formulas you should know:

QuantityFormulaNotes
Centripetal acceleration magnitudeac=v2ra_c = \dfrac{v^2}{r}Points toward center. Not “new” acceleration type—just direction change.
Angular speed relationshipv=ωrv = \omega rConnects linear and angular.
Centripetal acceleration (angular form)ac=ω2ra_c = \omega^2 rUseful if given ω\omega.
Period/angular speedω=2πT\omega = \dfrac{2\pi}{T}Also f=1Tf = \dfrac{1}{T}.

Examples & Applications

Example 1: 1D constant acceleration (braking)

A car at v0=20 m/sv_0 = 20\ \mathrm{m/s} brakes with constant a=4 m/s2a = -4\ \mathrm{m/s^2}. How far to stop?

  • Stopping means v=0v = 0.
  • Use the no-time equation: v2=v02+2aΔxv^2 = v_0^2 + 2a\Delta x.

0=(20)2+2(4)ΔxΔx=50 m0 = (20)^2 + 2(-4)\Delta x \Rightarrow \Delta x = 50\ \mathrm{m}

Key insight: when time isn’t asked for (and not given), jump to v2=v02+2aΔxv^2 = v_0^2 + 2a\Delta x.

Example 2: Vertical toss (max height)

Throw upward with v0y=+14 m/sv_{0y} = +14\ \mathrm{m/s}. Find max height above launch.

  • At top: vy=0v_y = 0.
  • Use: vy2=v0y2+2ayΔyv_y^2 = v_{0y}^2 + 2a_y\Delta y with ay=ga_y = -g.

0=(14)2+2(9.8)ΔyΔy=19619.6=10 m0 = (14)^2 + 2(-9.8)\Delta y \Rightarrow \Delta y = \dfrac{196}{19.6} = 10\ \mathrm{m}

Key insight: max height problems are almost always “set v=0v=0 at the top.”

Example 3: Projectile launched from a height (no same-height shortcuts)

A ball is launched from y0=5 my_0 = 5\ \mathrm{m} with v0=10 m/sv_0 = 10\ \mathrm{m/s} at θ=30\theta = 30^\circ. Find time to hit the ground.

  • Compute components: v0y=10sin30=5 m/sv_{0y} = 10\sin 30^\circ = 5\ \mathrm{m/s}.
  • Vertical equation with ground at y=0y = 0:

0=5+(5)t12(9.8)t20 = 5 + (5)t - \tfrac{1}{2}(9.8)t^2

Solve quadratic; you’ll get two solutions, take the positive landing time (the other is unphysical).

Key insight: different start/end heights forces you into y(t)y(t) and a quadratic.

Example 4: Read a vvtt graph via area

If a particle has:

  • v=2 m/sv = 2\ \mathrm{m/s} from t=0t=0 to t=3 st=3\ \mathrm{s},
  • then increases linearly to v=6 m/sv = 6\ \mathrm{m/s} by t=5 st=5\ \mathrm{s},
    then displacement is area under v(t)v(t):
  • Rectangle: Δx1=(2)(3)=6 m\Delta x_1 = (2)(3) = 6\ \mathrm{m}
  • Trapezoid from 3 to 5 s: average velocity =2+62=4 m/s= \tfrac{2+6}{2} = 4\ \mathrm{m/s}, so Δx2=(4)(2)=8 m\Delta x_2 = (4)(2) = 8\ \mathrm{m}
  • Total: Δx=14 m\Delta x = 14\ \mathrm{m}

Key insight: for linear segments, treat areas as rectangles/triangles/trapezoids.


Common Mistakes & Traps

  1. Mixing up distance and displacement

    • Wrong: using total path length in vavg=Δx/Δtv_{\text{avg}} = \Delta x/\Delta t.
    • Why wrong: Δx\Delta x is straight-line change in position (with sign).
    • Fix: compute displacement from initial and final positions.
  2. Forgetting velocity and acceleration are vectors (sign matters)

    • Wrong: plugging a=9.8a = 9.8 when you chose up as positive.
    • Why wrong: in that coordinate, ay=9.8 m/s2a_y = -9.8\ \mathrm{m/s^2}.
    • Fix: write your sign convention first; attach signs to every component.
  3. Assuming v=0v = 0 means a=0a = 0

    • Wrong: saying acceleration is zero at the top of a toss.
    • Why wrong: gravity is still acting, so ay=ga_y = -g at all times (ignoring air).
    • Fix: only set vy=0v_y = 0 at the peak, not acceleration.
  4. Using same-height projectile formulas when heights differ

    • Wrong: using T=2v0sinθgT = \dfrac{2v_0\sin\theta}{g} when launched from a cliff.
    • Why wrong: that formula assumes landing height equals launch height.
    • Fix: use y=y0+v0yt12gt2y = y_0 + v_{0y}t - \tfrac{1}{2}gt^2 with the actual final yy.
  5. Component confusion in projectile motion

    • Wrong: letting vxv_x change because vv changes.
    • Why wrong: with no air resistance, ax=0a_x = 0 so vxv_x stays constant.
    • Fix: treat xx and yy separately; only vyv_y changes with gravity.
  6. Picking the wrong time (multiple solutions)

    • Wrong: taking the negative root from a quadratic in tt.
    • Why wrong: negative time usually corresponds to an earlier crossing before your chosen t=0t=0.
    • Fix: interpret roots physically; choose the time consistent with the scenario.
  7. Sign errors in v2=v02+2aΔxv^2 = v_0^2 + 2a\Delta x

    • Wrong: plugging Δx\Delta x as a positive magnitude automatically.
    • Why wrong: Δx\Delta x can be negative depending on your axis direction.
    • Fix: compute Δx=xx0\Delta x = x - x_0 with sign.
  8. Misreading graph area vs slope

    • Wrong: treating area under v(t)v(t) as acceleration.
    • Why wrong: slope gives acceleration; area gives displacement.
    • Fix: memorize: “slope tells the derivative; area tells the accumulation.”

Memory Aids & Quick Tricks

Trick / mnemonicWhat it helps you rememberWhen to use it
“Big 4” constant-aa setThe four core constant-acceleration equationsAny 1D constant-acceleration motion (including vertical free fall)
“Split projectile into xx and yyIndependence: ax=0a_x=0, ay=ga_y=-gEvery projectile problem
“At the top: vy=0v_y=0, not ay=0a_y=0Peak conditionMax height / time-to-peak
“Slope/Area rules”slope of x(t)=v\text{slope of }x(t)=v, slope of v(t)=a\text{slope of }v(t)=a, area under v(t)=Δxv(t)=\Delta x, area under a(t)=Δva(t)=\Delta vGraph-based kinematics
“Same-height projectile: T,R,HT, R, H shortcuts”T=2v0sinθgT = \dfrac{2v_0\sin\theta}{g}, R=v02sin(2θ)gR = \dfrac{v_0^2\sin(2\theta)}{g}, H=v02sin2θ2gH = \dfrac{v_0^2\sin^2\theta}{2g}Only if launch and landing heights match
“Centripetal: ac=v2/ra_c = v^2/r (points inward)”Turning requires inward accelerationUniform circular motion questions

Quick Review Checklist

  • You can write the definitions: vavg=Δx/Δtv_{\text{avg}} = \Delta x/\Delta t and aavg=Δv/Δta_{\text{avg}} = \Delta v/\Delta t.
  • You know the Big 4 constant-acceleration equations and when each is best.
  • You always choose an axis and keep signs consistent (especially for free fall).
  • For vertical motion, you automatically set ay=ga_y = -g (if up is positive).
  • For projectiles: ax=0a_x=0 so vxv_x is constant; y(t)y(t) controls flight time.
  • You can extract motion from graphs: slope vs area rules.
  • You avoid same-height shortcuts unless the start and end heights truly match.
  • You sanity-check units and physical direction (negative velocity is fine; negative speed isn’t).

You’ve got this—most kinematics points come from clean setup, consistent signs, and the right equation choice.