Resolution of vectors

A cricket ball leaves a fielder's hand at some odd angle, half of the throw carrying it forward down the pitch, half of it carrying it upward against gravity. Nobody re-derives the throw from scratch — instead, every physicist's first move is to split it into two clean, independent pieces: how much is going sideways, and how much is going up. That single move, splitting one slanted vector into two perpendicular pieces, is called resolution of vectors, and it is arguably the single most-used trick in the whole of mechanics. Resolution is the mirror image of the vector addition you have just studied. Addition takes two vectors and merges them into one; resolution takes one vector and unfolds it back into two — but this time along directions you choose, almost always a pair of mutually perpendicular axes. Because the pieces are perpendicular, ordinary right-triangle trigonometry, sin⁡θ\sin\theta and cos⁡θ\cos\theta, does all the work, and the whole messy geometry of arrows-at-angles collapses into plain algebra. This is not a one-chapter trick. Every projectile problem later in this very chapter starts by resolving the launch velocity into a horizontal piece that never changes and a vertical piece that obeys gg. Every incline problem in Laws of Motion resolves gravity along and perpendicular to the slope. Every circular-motion problem resolves the centripetal pull into components. In this article you will learn exactly how a vector is broken into rectangular components, how those components are written using the unit vectors i^\hat i and j^\hat j, how to run the process backward to recover the original vector, and how to avoid the single most common mark-losing mistake in the whole topic: getting the quadrant of the angle wrong.

Key takeaways
  • Resolution splits one vector into two perpendicular components along axes of your choosing — the reverse operation of vector addition.
  • For a vector A⃗\vec A at angle θ\theta to the xx-axis, the components are Ax=Acos⁡θA_x = A\cos\theta and Ay=Asin⁡θA_y = A\sin\theta.
  • In unit-vector form, A⃗=Axi^+Ayj^\vec A = A_x\hat i + A_y\hat j — this is the standard way to write any 2-D vector for calculation.
  • The reverse process recovers magnitude and direction: A=Ax2+Ay2A = \sqrt{A_x^2+A_y^2} and θ=tan⁡−1(Ay/Ax)\theta = \tan^{-1}(A_y/A_x), with the quadrant fixed by the signs of AxA_x and AyA_y, not by the calculator alone.
  • Resolution turns vector addition into simple arithmetic: components add component-wise, A⃗+B⃗=(Ax+Bx)i^+(Ay+By)j^\vec A+\vec B = (A_x+B_x)\hat i+(A_y+B_y)\hat j — the method used throughout the rest of the chapter.
  • Choosing axes aligned with a problem's geometry (along an incline, along the initial velocity of a projectile) makes the components far simpler to compute.
  • Key idea: any vector in a plane can be written as A⃗=Acos⁡θ i^+Asin⁡θ j^\vec A = A\cos\theta\,\hat i + A\sin\theta\,\hat j, and this component form is what makes vector addition, projectile motion and circular motion all reduce to ordinary algebra.
The core insight

Resolving a vector A⃗\vec A at angle θ\theta into rectangular components Ax=Acos⁡θA_x=A\cos\theta and Ay=Asin⁡θA_y=A\sin\theta (so A⃗=Axi^+Ayj^\vec A = A_x\hat i+A_y\hat j) turns two-dimensional vector problems into two independent one-dimensional algebra problems, and the reverse relations A=Ax2+Ay2A=\sqrt{A_x^2+A_y^2}, θ=tan⁡−1(Ay/Ax)\theta=\tan^{-1}(A_y/A_x) (quadrant fixed by sign) let you recover the original vector exactly.

Where it fits in the syllabus

This topic sits directly inside the prescribed CBSE Class 11 Physics scope for Motion in a Plane: "resolution into rectangular components" is named explicitly alongside vector addition/subtraction and unit vectors. It follows the graphical triangle and parallelogram laws of vector addition and feeds straight into the analytical method of vector addition, which is nothing but resolution applied to two vectors and added component-wise. Everything below stays within algebra and right-triangle trigonometry in two dimensions — no 3-D geometry, no vector triple products, both of which are explicitly out of scope for this board.

The physical picture

Picture a vector A⃗\vec A drawn from the origin of an xyxy-plane, making an angle θ\theta with the positive xx-axis. Drop a perpendicular from the tip of A⃗\vec A onto the xx-axis; the foot of that perpendicular marks off a length AxA_x along the xx-axis, and the perpendicular itself has length AyA_y along the yy-axis. Together AxA_x and AyA_y are the two legs of a right triangle whose hypotenuse is A⃗\vec A, so ordinary trigonometry gives them directly:

Ax=Acos⁡θAy=Asin⁡θA_x = A\cos\theta \qquad A_y = A\sin\theta

where: AA is the magnitude (length) of the vector, θ\theta is the angle it makes with the chosen xx-axis (measured counter-clockwise), AxA_x is the component along the xx-axis (the projection of A⃗\vec A onto the xx-axis), and AyA_y is the component along the yy-axis. Physically, AxA_x and AyA_y are what the vector is "worth" along each axis on its own — for a force, AxA_x is the part of the force pulling along xx and AyA_y the part pulling along yy, and each behaves in every calculation exactly like an independent one-dimensional vector along its own axis. Once you have the two components, the original vector can be rebuilt exactly using the unit vectors i^\hat i (a vector of length 1 along xx) and j^\hat j (a vector of length 1 along yy):

A⃗=Axi^+Ayj^=Acos⁡θ i^+Asin⁡θ j^\vec A = A_x\hat i + A_y\hat j = A\cos\theta\,\hat i + A\sin\theta\,\hat j

This is the standard component form of a vector, and it is the form used for essentially every calculation from here through projectile motion and circular motion. It is worth being clear about what Axi^A_x\hat i and Ayj^A_y\hat j actually are: they are two genuine, separate vectors, one lying entirely along the xx-axis and one entirely along the yy-axis, whose vector sum reconstructs A⃗\vec A by the very same triangle law used for adding any two vectors. Nothing new is being invented here — resolution is just vector addition run in reverse. The process also runs backward. Given the components AxA_x and AyA_y of any vector, its magnitude and direction are recovered by:

A=Ax2+Ay2θ=tan⁡−1(AyAx)A = \sqrt{A_x^2 + A_y^2} \qquad \theta = \tan^{-1}\left(\frac{A_y}{A_x}\right)

where: the magnitude formula is simply the Pythagoras theorem applied to the right triangle formed by AxA_x, AyA_y and A⃗\vec A, and θ\theta is the angle whose tangent is the ratio of the opposite side (AyA_y) to the adjacent side (AxA_x). This inverse-tangent step is where most marks are lost in exams, because a calculator's tan⁡−1\tan^{-1} always returns a value strictly between −90∘-90^\circ and +90∘+90^\circ, regardless of which quadrant the vector actually lies in — you must look at the signs of AxA_x and AyA_y separately to place the angle correctly, a point developed fully in Worked example 2 below.

Figure
A vector at an angle to the x axis with dashed perpendiculars to both axes showing the horizontal component A x equals A cos theta and the vertical component A y equals A sin theta, forming a right triangle with the vector as hypotenuse
Resolving vector A into components A x and A y x y A A x = A cos theta A y = A sin theta theta The dashed lines are the projections of A onto each axis and form a right triangle with A as hypotenuse

Resolution also makes vector addition mechanical: if A⃗=Axi^+Ayj^\vec A = A_x\hat i+A_y\hat j and B⃗=Bxi^+Byj^\vec B = B_x\hat i+B_y\hat j, adding them simply means adding the like components,

A⃗+B⃗=(Ax+Bx)i^+(Ay+By)j^\vec A + \vec B = (A_x+B_x)\hat i + (A_y+B_y)\hat j

which is exactly the analytical method of vector addition covered in the next article — resolution is the tool that makes that method possible.

Derivation ADeriving the rectangular components of a vector from a right triangle

The goal here is to show, from nothing more than the definition of sine and cosine in a right triangle, why Ax=Acos⁡θA_x = A\cos\theta and Ay=Asin⁡θA_y = A\sin\theta are the correct components of a vector A⃗\vec A at angle θ\theta to the xx-axis, and why the same two relations can be inverted to recover AA and θ\theta from the components — the two-way relationship that underlies every use of resolution in this chapter and beyond.

Step 1. Set up the triangle. Draw A⃗\vec A from the origin, tip at angle θ\theta above the xx-axis. Drop a perpendicular from the tip straight down to the xx-axis, meeting it at a point PP. This creates a right triangle with the origin, PP, and the tip of A⃗\vec A as its three vertices, the right angle sitting at PP. The side from the origin to PP has length AxA_x; the side from PP up to the tip has length AyA_y; the hypotenuse, from the origin to the tip, is A⃗\vec A itself, of length AA.

Step 2. Apply the definitions of sine and cosine. In this right triangle, θ\theta is the angle at the origin. The side adjacent to θ\theta is the one along the xx-axis, of length AxA_x, and the hypotenuse has length AA, so by the definition of cosine, cos⁡θ=Ax/A\cos\theta = A_x/A. The side opposite θ\theta is the vertical side of length AyA_y, so by the definition of sine, sin⁡θ=Ay/A\sin\theta = A_y/A.

Step 3. Rearrange for the components. Multiplying both sides of each relation by AA gives Ax=Acos⁡θA_x = A\cos\theta and Ay=Asin⁡θA_y = A\sin\theta. These are the rectangular components: the magnitude of the vector times the cosine (for the axis the angle is measured from) and times the sine (for the perpendicular axis).

Step 4. Invert to recover magnitude and direction. Squaring and adding the two component relations gives Ax2+Ay2=A2cos⁡2θ+A2sin⁡2θ=A2(cos⁡2θ+sin⁡2θ)=A2A_x^2+A_y^2 = A^2\cos^2\theta+A^2\sin^2\theta = A^2(\cos^2\theta+\sin^2\theta) = A^2, using the identity cos⁡2θ+sin⁡2θ=1\cos^2\theta+\sin^2\theta=1. Taking the square root gives A=Ax2+Ay2A = \sqrt{A_x^2+A_y^2}. Dividing the two original relations instead, Ay/Ax=(Asin⁡θ)/(Acos⁡θ)=tan⁡θA_y/A_x = (A\sin\theta)/(A\cos\theta) = \tan\theta, so θ=tan⁡−1(Ay/Ax)\theta = \tan^{-1}(A_y/A_x), valid once the correct quadrant has been fixed by the signs of AxA_x and AyA_y separately.

Step 5. Read the result. The pair Ax=Acos⁡θA_x = A\cos\theta, Ay=Asin⁡θA_y = A\sin\theta and its inverse pair A=Ax2+Ay2A=\sqrt{A_x^2+A_y^2}, θ=tan⁡−1(Ay/Ax)\theta=\tan^{-1}(A_y/A_x) are exact for any vector in a plane and any choice of perpendicular axes — nothing about the physical nature of the vector (force, velocity, displacement) enters the derivation, which is why the same two lines of algebra reappear in every chapter that uses vectors.

Worked examples

Board level - resolving a force at a given angle

A force of magnitude 50 N acts at an angle of 37∘37^\circ above the horizontal. Resolve it into horizontal and vertical components. (Use sin⁡37∘≈0.6\sin 37^\circ \approx 0.6, cos⁡37∘≈0.8\cos 37^\circ \approx 0.8.)

Step 1. Choose axes matching the problem: horizontal as the xx-axis, vertical as the yy-axis, with θ=37∘\theta = 37^\circ measured from the horizontal.

Step 2. Apply Fx=Fcos⁡θF_x = F\cos\theta: Fx=50×0.8=40 NF_x = 50\times 0.8 = 40\ \text{N}.

Step 3. Apply Fy=Fsin⁡θF_y = F\sin\theta: Fy=50×0.6=30 NF_y = 50\times 0.6 = 30\ \text{N}.

Step 4. Write the component form and verify: F⃗=40i^+30j^ N\vec F = 40\hat i + 30\hat j\ \text{N}, and 402+302=1600+900=2500=50 N\sqrt{40^2+30^2} = \sqrt{1600+900} = \sqrt{2500} = 50\ \text{N}, matching the given magnitude exactly.

The horizontal component is 40 N and the vertical component is 30 N.

Competitive level - recovering magnitude and direction, with correct quadrant

A displacement vector has components Δx=−3 m\Delta x = -3\ \text{m} and Δy=4 m\Delta y = 4\ \text{m}. Find its magnitude and the angle it makes with the positive xx-axis.

Step 1. Apply the magnitude formula: ∣Δr⃗∣=(−3)2+42=9+16=25=5 m|\Delta\vec r| = \sqrt{(-3)^2+4^2} = \sqrt{9+16} = \sqrt{25} = 5\ \text{m}.

Step 2. Find the reference angle using magnitudes only, to avoid sign confusion: tan⁡θref=∣4/(−3)∣=4/3  ⟹  θref≈53.1∘\tan\theta_{ref} = |4/(-3)| = 4/3 \implies \theta_{ref} \approx 53.1^\circ.

Step 3. Fix the quadrant from the signs: Δx\Delta x is negative and Δy\Delta y is positive, so the vector points up and to the left — the second quadrant.

Step 4. Convert the reference angle to the true angle measured counter-clockwise from the positive xx-axis, for the second quadrant that means θ=180∘−θref=180∘−53.1∘=126.9∘\theta = 180^\circ - \theta_{ref} = 180^\circ - 53.1^\circ = 126.9^\circ.

The displacement is 5 m at 126.9° from the positive x-axis. Timing note: in an exam, budget about 30 seconds to compute the reference angle with tan⁡−1\tan^{-1} of the magnitude ratio, then a further 10 seconds just to look at the two signs and place the angle in the right quadrant — skipping that second step is the single most common way this question loses marks, even when the arithmetic is otherwise perfect.

Common traps

  • Applying θ=tan⁡−1(Ay/Ax)\theta = \tan^{-1}(A_y/A_x) mechanically without checking the quadrant from the signs of AxA_x and AyA_y — a calculator's tan⁡−1\tan^{-1} only ever returns an angle between −90∘-90^\circ and 90∘90^\circ, so answers in the 2nd or 3rd quadrant need a manual 180∘180^\circ correction, and answers in the 4th quadrant need a 360∘360^\circ correction if angles are being measured as positive values.
  • Swapping sine and cosine — remember Ax=Acos⁡θA_x = A\cos\theta (the side adjacent to the angle) and Ay=Asin⁡θA_y = A\sin\theta (the side opposite the angle), always relative to the axis θ\theta is measured from.
  • Adding magnitudes instead of using Pythagoras when recovering the resultant magnitude — a frequent slip is writing A=Ax+AyA = A_x + A_y instead of the correct A=Ax2+Ay2A=\sqrt{A_x^2+A_y^2}.
  • Mixing degrees and radians mid-calculation, especially when a calculator's mode has been left on the wrong setting from a previous question — always confirm the mode before evaluating sin⁡\sin, cos⁡\cos or tan⁡−1\tan^{-1}.
  • Choosing axes that fight the geometry of the problem instead of aligning with it — any pair of perpendicular axes is mathematically valid, but axes chosen along an incline or along a projectile's initial velocity usually turn a two-line calculation into a much longer, error-prone one.

You should be able to…

  • Resolve a given vector into rectangular components along chosen perpendicular axes, using Ax=Acos⁡θA_x=A\cos\theta and Ay=Asin⁡θA_y=A\sin\theta.
  • Write any 2-D vector in unit-vector component form Axi^+Ayj^A_x\hat i+A_y\hat j, and explain what Axi^A_x\hat i and Ayj^A_y\hat j physically represent.
  • Recover a vector's magnitude and direction from its components using A=Ax2+Ay2A=\sqrt{A_x^2+A_y^2} and θ=tan⁡−1(Ay/Ax)\theta=\tan^{-1}(A_y/A_x), fixing the quadrant correctly from the signs of AxA_x and AyA_y.
  • Verify a resolution by checking that Ax2+Ay2\sqrt{A_x^2+A_y^2} reproduces the original magnitude.
  • Add two vectors by adding their components separately, anticipating the analytical method of the next article.
  • Justify why choosing axes aligned with a problem's geometry (an incline, an initial velocity direction) simplifies the resulting algebra.

Ask the tutor: Not sure which quadrant your resolved vector falls in, or how to pick smart axes for a tricky incline or projectile diagram — ask the AI tutor to walk through your specific vector step by step.

Do the axes I resolve a vector along always have to be horizontal and vertical?

No. Any pair of mutually perpendicular directions works, and the formulas Ax=Acos⁡θA_x=A\cos\theta, Ay=Asin⁡θA_y=A\sin\theta hold as long as θ\theta is measured from whichever direction you have called the "x-axis." On an incline, it is standard to resolve gravity along the slope and perpendicular to the slope rather than horizontal-vertical, because that choice makes the resulting equations much shorter. The physics does not care which axes you pick — only your algebra gets easier or harder.

Why does A x equal A cos theta and not A sin theta? I keep mixing them up.

It depends only on which side of the right triangle is adjacent to the angle you are using. If θ\theta is measured from the xx-axis, then the xx-axis side is adjacent to θ\theta, so Ax=Acos⁡θA_x=A\cos\theta (cosine is always adjacent over hypotenuse), and the yy-axis side is opposite θ\theta, so Ay=Asin⁡θA_y=A\sin\theta. If a problem instead gives you the angle measured from the yy-axis, the roles of sine and cosine literally swap. The fix is not to memorize a rule blindly but to redraw the small right triangle every time and read off which side is adjacent to the given angle.

My answer for theta came out negative from the calculator. Is that wrong?

Not necessarily wrong, but it needs interpreting. A negative tan⁡−1\tan^{-1} result just means the reference angle is being measured below the positive xx-axis, which is correct behaviour if your vector genuinely has Ay<0A_y<0 and Ax>0A_x>0 — that is the fourth quadrant, and reporting a negative angle (or equivalently 360∘360^\circ minus that magnitude) is fine. The problem only arises when Ax<0A_x<0, because then the true angle needs a 180∘180^\circ adjustment that the calculator will never apply on its own. Always sketch the quadrant from the signs before trusting the raw calculator output.

Is resolving into more than two components ever needed in this chapter?

In principle a vector can be resolved along any number of directions, but for the two-dimensional motion covered in this CBSE chapter, two mutually perpendicular components are always enough, since any two non-parallel directions in a plane fully determine a vector. You will not be asked to resolve into three or more components here; full three-dimensional resolution and vector triple products are beyond this board's Class 11 prescription and are left for higher study.

Before this

Where this leads