Compute direction angles α, β, γ from a 2D or 3D vector, direction cosines, azimuth/elevation, compass visualization, angle bars, and direction cosine identity verification.
Every nonzero vector in space points in a specific direction that can be described by the angles it makes with the coordinate axes. In 3D, these direction angles α (with x-axis), β (with y-axis), and γ (with z-axis) along with their cosines completely characterize the vector's orientation. The fundamental identity cos²α + cos²β + cos²γ = 1 connects them and provides a built-in verification check.
This calculator computes direction angles and cosines for 2D and 3D vectors. Enter the components and instantly see all three direction angles in degrees or radians, the corresponding direction cosines, azimuth (horizontal angle in the xy-plane), and elevation (angle above or below the xy-plane). An interactive compass visualization shows the azimuth direction with a needle indicator, making it easy to interpret the result spatially.
Direction angle bars provide a visual comparison: are the angles roughly equal (as for the vector (1,1,1)) or highly skewed toward one axis? The direction summary table collects all computed angles alongside their cosines for quick reference, and the properties table summarizes the key identities governing direction cosines.
Direction angles appear throughout physics (e.g., force resolution, crystallography), computer graphics (camera orientation, lighting calculations), navigation (heading and pitch), and antenna engineering (beamforming). Understanding how a vector's components map to directional properties is a core skill in applied linear algebra.
Choose from six presets covering symmetric vectors, axis-aligned vectors, and common textbook problems. Toggle between degrees and radians to match your preferred convention. The calculator updates all outputs in real time, so you can explore how rotating a vector by changing one component affects all three direction angles and the azimuth/elevation pair.
Computing direction angles requires magnitude calculation, division, and inverse cosine for each axis — three separate arccos evaluations in 3D, plus converting between radians and degrees. Azimuth and elevation add atan2 calls. This calculator handles all of it for 2D and 3D vectors: direction angles α, β, γ in degrees and radians, direction cosines, azimuth, elevation, and the identity check cos²α + cos²β + cos²γ = 1. Six presets cover uniform, axis-aligned, and general cases. Essential for anyone working with orientations in physics, navigation, or 3D graphics.
cos α = x/‖v‖, cos β = y/‖v‖, cos γ = z/‖v‖; azimuth = atan2(y, x); elevation = atan2(z, √(x²+y²))
Result: α ≈ 73.40°, β ≈ 64.62°, γ ≈ 31.00°
‖v‖ = √(4 + 9 + 36) = 7. cos α = 2/7 → α ≈ 73.40°. cos β = 3/7 → β ≈ 64.62°. cos γ = 6/7 → γ ≈ 31.00°. Check: (2/7)² + (3/7)² + (6/7)² = 4/49 + 9/49 + 36/49 = 1 ✓.
The **direction angle** θᵢ is the angle between a vector v and the positive iᵗʰ coordinate axis. For 3D vectors: cos α = vₓ/‖v‖, cos β = vᵧ/‖v‖, cos γ = vₘ/‖v‖. These three cosines are exactly the components of the unit vector û, and they satisfy the **fundamental identity** cos²α + cos²β + cos²γ = 1 (since ‖û‖ = 1). Direction angles always range from 0° to 180°: 0° means the vector is parallel to the axis, 90° means perpendicular, and 180° means antiparallel.
**Azimuth** (φ) is the angle in the xy-plane measured counterclockwise from the +x axis, computed as atan2(y, x) (range −180° to 180°). **Elevation** (θ) is the angle above or below the xy-plane: atan2(z, √(x²+y²)) (range −90° to 90°). Together, azimuth and elevation define a direction on the unit sphere and are used in navigation (heading + pitch), antenna design (beam pointing), and 3D audio (sound source placement). Converting to spherical coordinates (r, θ, φ) from Cartesian is a routine change-of-variables in physics and engineering.
In **robotics**, direction cosines define end-effector orientation in rotation matrices. In **physics**, the direction of a force determines its torque about a pivot: τ = r × F depends on the angle between r and F. In **computer graphics**, the dot product of a surface normal’s direction with the light direction determines shading intensity (Lambert’s cosine law). In **meteorology**, wind direction is reported as azimuth from north. Any time a quantity has direction, these angles and cosines are the mathematical language used to describe it.
Direction angles α, β, γ are the angles a vector makes with the positive x, y, and z axes respectively. They range from 0° (parallel) to 180° (antiparallel) and fully specify the vector's orientation in 3D space.
Direction cosines are the cosines of the direction angles: cos α, cos β, cos γ. They equal the unit vector's components and satisfy the identity cos²α + cos²β + cos²γ = 1.
They are identical. The unit vector v̂ = (cos α, cos β, cos γ). This means direction cosines give you both the angle information and the normalized direction components.
Azimuth is the angle in the xy-plane measured from the +x axis (using atan2, range −180° to 180°). Direction angle α is the angle from the x-axis in full 3D space (range 0° to 180°). They differ when the vector has a z-component.
Elevation is the angle above or below the xy-plane, computed as atan2(z, √(x²+y²)). It ranges from −90° (pointing straight down) to +90° (pointing straight up). Together with azimuth, it defines the direction in spherical coordinates.
Yes. The vector (1, 1, 1) has α = β = γ ≈ 54.74°, since cos α = 1/√3 for each axis. This is the only direction (up to sign) with equal direction angles.