Navigation • Surveying • Mathematics • Engineering

Advanced Vector Bearing Calculator

Convert bearings and components, combine vectors, solve navigation routes, correct wind or current, analyze traverses, and inspect every calculation step.

Calculator Mode

Choose a vector or bearing task

Inputs

Components to Bearing

Format: magnitude,bearing[,weight,label]. Bearing uses the selected angle unit.
Format: distance,bearing[,label].
Formula Reference

Core formulas used

Components from bearing

East = r × sin(θ)
North = r × cos(θ)

Bearing from components

θ = atan2(East, North)
θ = (θ + 360°) mod 360°

Magnitude

|v| = √(x² + y²)

Dot product

A · B = AₓBₓ + AᵧBᵧ

Projection

projᵦ(A) = (A·B / |B|²)B

Great-circle distance

d = 2R asin(√a)
Instructions

How to use this calculator

Select a calculation mode that matches your available data. Enter components, bearings, coordinates, or multiple vector rows. Choose the correct angle and distance units before calculating.

Review the result cards, detailed steps, diagram, and table. Use CSV export for spreadsheets. Use Print or PDF to create a formatted report from your browser.

For navigation data, verify coordinate signs and the bearing convention. For magnetic corrections, use a current declination value. For survey work, inspect misclosure before applying adjustments.

Saved Data

Calculation history

Reference

Bearing conventions and practical notes

A navigation bearing starts at north and increases clockwise. A mathematical direction angle starts at east and increases counterclockwise. Converting between them requires a ninety-degree axis rotation and normalization.

Quadrant bearings use north or south first, followed by an acute angle and east or west. Whole-circle bearings avoid quadrant ambiguity. Back bearings point exactly opposite the original direction.

Vector components preserve both magnitude and direction. East and north components are especially useful for surveying, aviation, marine navigation, GIS, robotics, and engineering force analysis.

Geographic calculations treat Earth as a sphere in this standalone version. Great-circle routes represent shortest spherical paths. High-precision geodesy may require an ellipsoidal library and a selected datum.

Magnetic declination varies by position and date. Grid convergence depends on the map projection. Never treat an old correction value as universally valid.

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Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.