What Is Magnetic Declination and Why It Matters
Magnetic declination is the horizontal angle between the direction your compass needle points (Magnetic North) and the direction of the geographic North Pole (True North). Because the Earth’s magnetic field is generated by slow, chaotic convection of molten iron in the outer core, Magnetic North is not a fixed point — it drifts continuously, currently shifting from Canada toward Siberia at roughly 55 km per year.
This drift means that any compass reading you take — whether from a traditional baseplate compass, a smartphone magnetometer, or an aircraft instrument — is slightly “wrong” relative to the map under your feet. Depending on where you stand, the offset can be anywhere from 0° near the agonic line (currently running through central USA and eastern India) to more than 20° in parts of Alaska, Scandinavia, southern Brazil, and South Africa. Our calculator tells you exactly how much to correct for, using the latest World Magnetic Model (WMM-2025) coefficients.
Who Needs a Declination Calculator?
Even in 2026, declination silently distorts the work of millions of people who never realise it. If you fall into any of these groups, a quick declination check is essential before you commit to a reading:
