Magnetic Variation (Declination)
Magnetic variation (declination) is the angular difference between true north and magnetic north, vital for accurate navigation in aviation, maritime, and land ...
Magnetic declination is the angle between true and magnetic north, essential for accurate compass-based navigation and updated regularly due to Earth’s magnetic field changes.
Magnetic declination is a fundamental concept for anyone involved in navigation—whether by air, sea, or land. This guide provides a detailed, aviation-focused exploration of magnetic declination, its calculation, operational implications, and regulatory context, incorporating the latest scientific and industry standards.
Magnetic declination (also known as magnetic variation) is the horizontal angle between geographic (true) north and magnetic north at a specific place on Earth. Depending on your location, magnetic north (the direction a compass points) can be east or west of true north. This angle is measured in degrees, minutes, and is designated east or west (e.g., “10° 30′ E” or “5° 45′ W”).
Declination is crucial for:
The value of magnetic declination is not static. It changes with location and over time due to the dynamic nature of Earth’s magnetic field—a phenomenon known as secular variation. This requires regular updates to navigation systems, procedures, and charts.
Understanding the different “north” references is essential for accurate navigation:
| Reference North | Definition | Usage Context |
|---|---|---|
| True North | Direction to the geographic North Pole | Map reading, GPS, astronomy |
| Magnetic North | Direction a magnetic compass points (Earth’s local magnetic field) | Compass navigation, aviation |
| Grid North | North along map grid lines (map projection) | UTM maps, military operations |
True North is a fixed point—where the Earth’s axis meets its northern surface.
Magnetic North is a wandering point influenced by the Earth’s molten core, currently moving northwestward at 55–60 km/year (NOAA, WMM 2020).
Grid North is defined by map projections (e.g., UTM grids) and is a mathematical construct for practical map reading.
In aviation, runway numbers and heading references are based on magnetic north, except in polar regions (above 70°N/S), where true north is used due to magnetic unreliability.
Agencies like NOAA and the International Association of Geomagnetism and Aeronomy (IAGA) publish the World Magnetic Model (WMM) and the International Geomagnetic Reference Field (IGRF) every five years to provide up-to-date declination data. ICAO mandates that aeronautical charts and procedures be updated with the latest variation information.
Example: The magnetic north pole’s rapid drift in recent years prompted an out-of-cycle WMM update in 2019.
Deviation is the error caused by magnetic influences inside the aircraft (or ship/vehicle), such as metal structures and electrical systems. It is unique to each compass installation and must be measured and corrected by a process known as compass compensation or a compass swing.
Both declination (a geographic value) and deviation (a local error) must be corrected for precise navigation.
Isogonic charts are vital for quickly determining local declination. The agonic line shifts over time; for example, it currently passes through the central US and Canada, moving due to secular variation.
Multiple methods exist, including:
| Source | Accuracy | Update Frequency | Use |
|---|---|---|---|
| Chart | Moderate | Varies | General navigation |
| WMM/IGRF | High | 5 years | Aviation, maritime |
| Field Measurement | Very high | As needed | Surveying |
| Avionics | High | Automatic | Commercial aviation |
| Mobile/Web | High | Real-time | All users |
Conversions:
Example:
True heading = 090°, declination = 12° W → Magnetic heading = 090° + 12° = 102°
Runways are numbered according to their magnetic alignment, rounded to the nearest 10°. If declination changes enough to shift the magnetic heading, the runway number must be changed (e.g., 17 becomes 16 if its magnetic heading drops from 174° to 166°). This is regulated per ICAO Annex 14 and published via NOTAMs and AIPs.
Above 70° latitude, magnetic compasses become unreliable. ICAO Doc 7030 requires true north references in navigation and ATC instructions. Aircraft must be equipped to display true heading, and crews must be trained in true north operations.
Deviation is managed by performing a compass swing—aligning the aircraft with known headings and recording compass errors. Deviation cards are updated after maintenance, equipment changes, or if deviation exceeds regulatory limits (typically 10° for aviation).
Both are updated every five years and underpin all global navigation systems.
Solar flares and coronal mass ejections can cause short-term magnetic anomalies, especially at high latitudes. Although typically minor for aviation, severe storms may temporarily affect compass readings and inertial systems. ICAO and national agencies issue Space Weather Advisories when such events are expected to impact navigation or communications.
Pilots must:
Regions like the South Atlantic Anomaly or areas near large iron deposits can have unpredictable declination. Pilots should consult NOTAMs, AIP supplements, or scientific references for local advisories and, when possible, rely on GPS and radio navigation.
Magnetic declination is a foundational element of global navigation, affecting everything from flight planning and runway numbering to chart creation and compass use. Regular updates and proper corrections are essential for safety and accuracy, with global standards enforced by ICAO and national authorities.
Stay informed, keep your data current, and always account for both declination and deviation to ensure safe, precise navigation.
Magnetic declination, also called magnetic variation, is the angle between true north (geographic north) and magnetic north (the direction a compass points). It is crucial in aviation for converting between magnetic headings (used by compasses and ATC) and true headings (used in chart plotting and high-latitude operations). The value varies by location and changes over time due to Earth’s shifting magnetic field.
Magnetic declination changes due to secular variation, the slow movement of Earth’s magnetic field. Agencies like NOAA and IAGA update models (WMM, IGRF) every five years. Pilots and navigators must use current data to ensure navigation accuracy; outdated values can cause significant heading errors, especially over long distances or in areas with high variation.
Declination (variation) is a geographic difference between true and magnetic north, affecting all compasses in a region. Deviation is a local compass error caused by magnetic influences inside the aircraft or vessel, unique to each compass installation. Both must be corrected for precise navigation.
Runways are numbered according to their magnetic heading rounded to the nearest 10°. As local magnetic declination changes, the runway’s magnetic heading may shift enough to require renumbering for accuracy and compliance with ICAO/FAA standards. This ensures consistency for pilots and air traffic controllers.
Pilots use declination values to convert between true and magnetic headings when planning routes, flying compass headings, or interpreting charts. Modern avionics often apply corrections automatically, but pilots must understand and verify these values for redundancy and in situations where manual navigation is required.
Keep your navigation systems and procedures up to date with the latest magnetic declination data. Ensure safe, precise operations by applying current variation values in your charts and flight planning.
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