A unit vector is a vector of norm one in a normed vector space. For a nonzero vector v, vector normalization produces one by dividing by ∥v∥. In a real Euclidean space, this keeps the direction and removes the magnitude. The zero vector cannot be normalized because its norm is zero.
For v=(3,4) with Euclidean norm 5, the corresponding unit vector isThe Euclidean vector can therefore be reconstructed as v=5v: size and direction are distinct pieces of information. The standard basis vectors are familiar unit vectors, but a unit vector need not point along a coordinate axis.
v=(53,54),∥v∥22=259+2516=1.
Normalization keeps direction and places the endpoint on the unit circle
. The original Euclidean vector (3,4) has magnitude 5. Its vector normalization (3/5,4/5) lies on the unit circle. The enlarged right panel also shows its negative, which has the same Euclidean norm and the opposite direction. Details.Vector normalization converts a nonzero vector in a normed vector space into a unit vector. Absolute homogeneity of a norm givesThe direction is unchanged by multiplying by a positive real scalar. For c>0, ∥cv∥=c∥v∥ and cv=v; for a negative real scalar, cv=−v. Thus (3,4) and (6,8) normalize to the same unit vector, while (−3,−4) normalizes to its negative. This decomposition is useful for specifying a direction independently of a force, velocity or displacement magnitude.
∥v∥v=∥v∥∥v∥=1.
In a complex normed vector space, a nonzero complex scalar c instead gives cv=(c/∣c∣)v. The remaining complex argument is not removed by normalization. For a pure quantum state, vectors differing only by this overall global phase represent the same physical state; vector normalization alone does not identify them.
The zero vector cannot be normalized this way. The construction also applies in a function space: an eigenfunction of a Sturm-Liouville problem can be scaled to unit weighted norm byThe positive weight w specifies the weighted inner product. Multiplication by this nonzero constant preserves the eigenvalue equation and its homogeneous boundary conditions.
ynormalized(x)=∫abw(s)∣y(s)∣2dsy(x).
Vector normalization is not a linear map. With e1=(1,0) and e2=(0,1),Consequently, adding individually normalized directions does not generally give the direction of the original vector sum. Compute the intended vector sum first, then normalize it if it is nonzero. Cancellation is a further boundary case: v+(−v)=0 has no normalized direction even though both nonzero summands do. A numerical algorithm must check that case before dividing by the norm.
e1+e2=21(1,1)=(1,1)=e1+e2.
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- Angular separation
- A norm-closed dual subspace need not be weak-star closed
- Apparent-gravity camera frame
- Approximate eigenvector
- Areal velocity
- Astronomical horizon
- Axial angular velocity of a symmetric top
- Axis of rotation
- Azimuthal unit vector
- Biot-Savart law
- Cartesian basis
- Causal Dirac spinor current
- Central spring stiffness matrix
- Commuting plane reflections
- Contact slip displacement
- Continuation predictor-corrector step
- Continuous dual space
- Coriolis acceleration in local Earth coordinates
- Coulomb's law
- Cross-polytope
- Cross product equation with a fixed unit vector
- Curl in spherical coordinates
- Declination
- Del in cylindrical and spherical coordinates
- Derivative along a curve
- Diagonal scaling for a two-dimensional linear system
- Directional derivative
- Directional measurement of trailing-edge thickness
- Directional stretch
- Direction vector
- Doppler frequency along a trajectory
- Dot product
- Effective rank of a covariance matrix
- Eigenvector
- Electron spin
- Equal-frequency light between equal-speed inertial observers
- Equal-length crystallographic root configurations in a plane
- Equatorial coordinate system
- Exact two-dimensional power iteration
- Exponential of a Pauli vector
- Extreme point
- Faraday rotation from circular phases
- FRET dipole orientation factor
- Gear tooth sliding
- Gnomonic projection
- Gradient
- Gradient in orthogonal coordinates
- Gravity gradiometry
- Great-circle distance
- Ground state
- Ground-state degeneracy
- Gyroscope direction reference
- Half-turn
- Helium-3 A phase
- Hermitian operator
- Hermitian quadratic form
- Horizontal coordinate system
- Householder transformation
- Ideal rigid link
- Inertia tensor
- Inertia tensor of paired point masses
- Interference (wave propagation)
- Inverse of an axis-angle linear map
- Inverse of a scalar plus a cross-product operator
- Isotropic orientation fourth moment
- Isotropic rotational diffusion in three dimensions
- Jones matrix
- Latitude law of Foucault precession
- Left singular vector
- Lever arm
- Low-rank approximation
- Malus's law
- Minimum pairwise dot-product sum of three unit vectors
- Nearest points to the origin on a positive-definite ellipsoid
- Numerical-range endpoint approximate-eigenvalue theorem
- Orbital-frame rotation from inclination and node
- Orthogonal projection of a circle between planes
- Outward conormal of a surface boundary
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A unit vector is a vector that has a magnitude of exactly one. Unit vectors are typically used to indicate direction without regard to magnitude. In mathematical terms, a unit vector is often denoted with a "hat" symbol, such as \(\hat{u}\). For any vector \(\mathbf{v}\), the unit vector in the direction of \(\mathbf{v}\) can be computed by dividing the vector by its magnitude (or length).
