Grid convergence is the angular difference between true north and grid north at a given location on a map projection. It arises because map projections distort the Earth’s surface, causing meridians to curve relative to the projection’s grid.
In a Transverse Mercator or similar conformal projection, the convergence can be expressed analytically as a function of the point’s latitude (Ο), longitude (Ξ»), and the projection’s central meridian (Ξ»β). This relationship allows surveyors to correct bearing measurements taken on the ground to the grid system used in national coordinate databases.
Accurate calculation of grid convergence is essential for highβprecision engineering tasks such as aligning infrastructure, integrating GPS data, and performing cadastral mapping. The calculator below implements the standard formula for convergence in a conformal projection.
What is grid convergence in map projections?
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Results are for informational purposes only and do not constitute professional advice.
