Grid Convergence Angle Calculator
Computes grid convergence from latitude, longitude and the central meridian for map projections.
Inputs
Grid convergence γ between true north and grid north — projection-derived, with the first-order approximation beside it — and grid → true azimuth under a printed sign convention.
Enter the values and press Calculate.
Or load an example to see a worked result.
Batch from CSV
One row per calculation, with a header row. Values use the units currently selected in the form above. Up to 10,000 rows; nothing is uploaded.
How the method works
A fixed worked example to explain the method — it is not your result.
Before you rely on this: First-pass guide only. Verify safety-critical or regulated work against the relevant standards, your project requirements and a qualified professional.
How to use this calculator
- Enter the latitude and longitude.
- Choose the projection: enter a Transverse Mercator central meridian, or let UTM pick the zone (standard or one you enter).
- Optionally enter a grid bearing to convert to a true azimuth.
- Press Calculate. The precise and approximate values are shown side by side with their difference.
How it works
Sign convention (always printed with the result): γ is the clockwise angle from true north to grid north, so true azimuth = grid azimuth + γ.
Precise: γ comes from the same Krüger-series Transverse Mercator kernel as the UTM converters. Its sign and size agree with a finite difference of proj4's own projection to about 1×10⁻⁸°. It is offered within 6° of the central meridian and marked unavailable beyond, rather than replaced with the approximation.
Approximation: γ ≈ (λ − λ₀) sin φ. It is exact on the central meridian and at the equator and drifts with distance from the meridian.
Worked example
−31.95°, 116°, central meridian 117°. Approximation +0.529179°, precise +0.529218° (the approximation is 0.141″ smaller). A grid bearing of 100° is a true azimuth of 100.529218°.
Common mistakes
- Applying γ with the wrong sign. Check the printed convention before adding or subtracting.
- Using the approximation several degrees from the meridian, where it drifts by arcseconds.
- Confusing grid convergence with magnetic declination.
Frequently asked questions
Why does grid convergence matter?
Bearings on a map grid differ from true bearings by the convergence angle; surveyors apply it when relating grid and true north.
Does grid convergence change with the date?
No. Grid convergence is pure geometry — it depends only on where you are relative to the central meridian, not on time. The angle that changes with date is magnetic declination (true north vs magnetic north); use the Magnetic Declination Calculator for that.
Related tools
- Azimuth to Bearing Converter
- UTM Zone Finder from Coordinates
- Magnetic Declination Calculator
- Combined Scale Factor Helper
- Coordinate Precision Estimator (Decimal Places to Metres)
- UTM Scale Factor Calculator
Explore more in Surveying, Coordinates, GIS & CAD.
Cite this tool
Zerdly. (2026). Grid Convergence Angle Calculator. Retrieved from https://www.zerdly.com/tools/grid-convergence-angle-calculator/
Tip: Enter any known values to calculate the remaining results.
Designed to run locally in your browser. Tool inputs are not intentionally stored by Zerdly unless stated otherwise.



