Magnetic Navigation
Comprehensive treatment of Earth’s magnetic field for military navigation, including mathematical models (IGRF, WMM), compass deviation analysis, and space weather effects on magnetic navigation systems.
Earth’s Magnetic Field: Theoretical Foundation
The Geodynamo
Earth’s magnetic field originates from convective motion of molten iron in the outer core (depth ~2,900-5,100 km). This self-sustaining dynamo creates a field approximating a magnetic dipole tilted ~11.5° from the rotational axis.
| Parameter | Value | Notes |
|---|---|---|
Dipole moment |
7.94 × 10²² A·m² |
Decreasing ~5% per century |
Field at equator |
~30 μT (0.3 Gauss) |
Horizontal component |
Field at poles |
~60 μT (0.6 Gauss) |
Vertical component |
Core-mantle boundary field |
~400 μT |
10× surface strength |
Secular variation rate |
~0.1°/year |
Regional dependent |
The Seven Magnetic Elements
At any point on Earth, the magnetic field is characterized by seven interrelated elements:
Geographic North
│
│ D (Declination)
│╱
───────────────────── Horizontal plane
╲│
│
│ I (Inclination/Dip)
▼
F (Total)
X = H cos(D) (North component)
Y = H sin(D) (East component)
Z (Down component)
| Symbol | Name | Definition |
|---|---|---|
\(D\) |
Declination |
Angle between true north and magnetic north (horizontal plane) |
\(I\) |
Inclination (Dip) |
Angle between horizontal plane and total field vector |
\(H\) |
Horizontal Intensity |
Magnitude of horizontal component |
\(X\) |
North Component |
Horizontal component in true north direction |
\(Y\) |
East Component |
Horizontal component in true east direction |
\(Z\) |
Vertical Component |
Downward component (positive into Earth in Northern Hemisphere) |
\(F\) |
Total Intensity |
Magnitude of total field vector |
Mathematical Relationships
The seven elements are related by:
The Three Norths
Every navigator must understand three different "norths":
True North (★)
│
│ Grid Convergence (GC)
▼
Grid North (GN)
│
│ Magnetic Declination (δ)
▼
Magnetic North (MN)
True North (Geographic North)
-
Direction to the Geographic North Pole
-
Earth’s rotational axis intersection with surface
-
Fixed (doesn’t change)
-
What maps are aligned to
-
Symbol: ★ (star)
Grid North
-
Direction of northing grid lines on a map
-
Parallel to the central meridian of the map projection
-
Differs from True North except along central meridian
-
Deviation called Grid Convergence
-
Symbol: GN
Magnetic North
-
Direction a compass needle points
-
Location of Magnetic North Pole (currently ~86.5°N, 164°E in Arctic Canada)
-
MOVES approximately 55 km/year (toward Russia)
-
Deviation from True North called Magnetic Declination (or Magnetic Variation)
-
Symbol: MN or half-arrow
Magnetic Declination
Definition
Magnetic Declination (\(\delta\)) is the angle between True North and Magnetic North at a specific location.
East Declination |
Magnetic North is EAST of True North (positive) |
West Declination |
Magnetic North is WEST of True North (negative) |
The Declination Formula
|
Mnemonic: "East is least, West is best"
Or reverse: "CADET" - Compass Add Declination Equals True (for West declination) |
Example Calculations
Your compass reads: 045° (magnetic) Declination: 12° East True Bearing = 045° + 12° = 057° True If plotting on map (True → Magnetic): Map bearing: 057° True Compass setting: 057° - 12° = 045° Magnetic
Your compass reads: 045° (magnetic) Declination: 16° West True Bearing = 045° - 16° = 029° True If plotting on map (True → Magnetic): Map bearing: 029° True Compass setting: 029° + 16° = 045° Magnetic
Isogonic and Agonic Lines
Isogonic Lines
Lines connecting points of equal magnetic declination.
20°W 15°W 10°W 5°W 0° 5°E 10°E 15°E 20°E
│ │ │ │ │ │ │ │ │
┌─────────┼───────┼───────┼──────┼──────┼──────┼───────┼──────┼──────┤
│ │ │ │ │ │ │ │ │ │
│ Pacific │ │ │ Agonic │ │ │ │ │
│ Northwest│ │ │ Line │ │ │ │ │
│ │ │ │ │ │ │ │ │ │
│ Seattle │ │ │ Chicago │ │ NYC │ │
│ │ │ │ │ │ │ │ Boston │
│ San Francisco│ │ Denver │ │ │ │ │
│ │ │ │ │ │ │ │ │ │
│ Los Angeles │ │ │ Dallas │ Atlanta │ │
│ (12°E) │ │ │ │ │ (6°W)│ │ │
│ │ │ │ │ │ │ │ │ │
└─────────┴───────┴───────┴──────┴──────┴──────┴───────┴──────┴──────┘
↑
Agonic Line
(0° declination)
The Agonic Line
The agonic line is where declination = 0° (compass points to True North).
-
Runs roughly from Louisiana through the Great Lakes to Hudson Bay
-
Moving westward approximately 0.1°/year in the US
-
In 1900, it ran through the eastern seaboard
Year Agonic Line Position (approximate US crossing) 1900 Through Maine, passing west of NYC 1950 Through Ohio, Great Lakes 2000 Through Michigan, Mississippi 2025 Through Louisiana, Wisconsin 2050 Expected through Texas, Minnesota (projected)
Annual Change
Declination changes over time. Maps include an annual change value.
MAGNETIC NORTH DECLINATION AT CENTER OF SHEET GN MN ╲ ╱ ╲ ╱ ╲╱ │ │ True North Magnetic declination: 12°30' East Annual change: 0°6' West For 2025 (if map dated 2020): Years elapsed: 5 Change: 5 × 6' = 30' = 0.5° West Current declination: 12.5° - 0.5° = 12.0° East
Geomagnetic Field Models
Spherical Harmonic Expansion
The geomagnetic field is mathematically described using spherical harmonic expansion of the scalar magnetic potential:
Where:
-
\(a\) = Earth’s reference radius (6371.2 km)
-
\(r, \theta, \lambda\) = geocentric spherical coordinates
-
\(g_n^m, h_n^m\) = Gauss coefficients (determined from observations)
-
\(P_n^m\) = Schmidt quasi-normalized associated Legendre functions
-
\(n\) = degree, \(m\) = order
The magnetic field components are derived from the potential:
IGRF (International Geomagnetic Reference Field)
The International Geomagnetic Reference Field is the internationally agreed mathematical model of Earth’s main magnetic field, maintained by IAGA (International Association of Geomagnetism and Aeronomy).
| Property | Value |
|---|---|
Current version |
IGRF-14 (released December 2024) |
Degree/Order |
n = m = 13 |
Gauss coefficients |
195 (for main field) |
Secular variation |
Linear prediction (5-year intervals) |
Valid period |
1900-2030 |
Update cycle |
Every 5 years |
Accuracy (declination) |
~0.5° RMS at Earth’s surface |
| n | m | \(g_n^m\) (nT) | \(h_n^m\) (nT) |
|---|---|---|---|
1 |
0 |
-29351.8 |
- |
1 |
1 |
-1410.2 |
4545.4 |
2 |
0 |
-2556.6 |
- |
2 |
1 |
2950.5 |
-2937.1 |
2 |
2 |
1649.1 |
-734.0 |
3 |
0 |
1361.0 |
- |
3 |
1 |
-2329.6 |
-165.8 |
3 |
2 |
1253.7 |
195.6 |
3 |
3 |
714.0 |
-357.6 |
WMM (World Magnetic Model)
The World Magnetic Model is the standard model for US/UK military navigation and aviation, produced jointly by NCEI (NOAA) and BGS (British Geological Survey).
| Property | WMM | IGRF |
|---|---|---|
Primary use |
Navigation (DoD/NATO) |
Scientific reference |
Degree/Order |
n = m = 12 |
n = m = 13 |
Update cycle |
5 years |
5 years |
Out-of-cycle updates |
Yes (when needed) |
No |
Current version |
WMM2025 |
IGRF-14 |
Valid dates |
2025.0 - 2030.0 |
1900.0 - 2030.0 |
Error model |
Included |
Not included |
|
WMM Validity WMM is only valid within its 5-year epoch. Using expired WMM coefficients can introduce errors of several degrees in polar regions where secular variation is rapid. Current WMM2025 expires: December 31, 2029 |
Secular Variation
The magnetic field changes continuously. Secular variation is modeled as the time derivative of Gauss coefficients:
Where \(\dot{g}_n^m\) is the secular variation coefficient (nT/year).
| Region | Typical Change Rate |
|---|---|
North America |
0.0° to -0.15°/year (declination) |
Europe |
0.10° to 0.20°/year (declination) |
South Atlantic Anomaly |
Intensifying, spreading west |
Magnetic poles |
40-55 km/year movement |
Python Implementation: IGRF Calculation
#!/usr/bin/env python3
"""
IGRF-14 Magnetic Field Calculator
Military-grade implementation using spherical harmonics
"""
import numpy as np
from scipy.special import lpmv # Associated Legendre polynomials
def schmidt_quasi_normalize(n, m, P_nm):
"""
Apply Schmidt quasi-normalization to Legendre polynomial.
Schmidt normalization: P_n^m(cos θ) * S_n^m
where S_n^m = sqrt((2 - δ_m0) * (n-m)! / (n+m)!)
"""
from math import factorial
if m == 0:
return P_nm
else:
S = np.sqrt(2 * factorial(n - m) / factorial(n + m))
return S * P_nm
def igrf_field(lat, lon, alt_km, year, coeffs):
"""
Calculate magnetic field components using IGRF model.
Parameters:
lat: Geodetic latitude (degrees)
lon: Longitude (degrees)
alt_km: Altitude above WGS84 ellipsoid (km)
year: Decimal year (e.g., 2025.5)
coeffs: Dictionary of Gauss coefficients
Returns:
X, Y, Z: Magnetic field components (nT)
"""
# Convert to geocentric coordinates
a = 6378.137 # WGS84 semi-major axis (km)
f = 1/298.257223563 # WGS84 flattening
lat_rad = np.radians(lat)
lon_rad = np.radians(lon)
# Geocentric radius and co-latitude
sin_lat = np.sin(lat_rad)
cos_lat = np.cos(lat_rad)
# Earth radius at latitude (simplified)
r = a + alt_km
theta = np.pi/2 - lat_rad # Co-latitude
# Reference radius for IGRF
a_ref = 6371.2 # km
# Initialize field components
X, Y, Z = 0.0, 0.0, 0.0
N_max = 13 # IGRF degree
for n in range(1, N_max + 1):
for m in range(0, n + 1):
# Get coefficients (interpolate for year)
g = coeffs.get((n, m, 'g'), 0)
h = coeffs.get((n, m, 'h'), 0) if m > 0 else 0
# Associated Legendre polynomial
P = lpmv(m, n, np.cos(theta))
P = schmidt_quasi_normalize(n, m, P)
# Derivative of P with respect to theta
if theta != 0 and theta != np.pi:
dP = (n * np.cos(theta) * P -
(n + m) * lpmv(m, n-1, np.cos(theta))) / np.sin(theta)
else:
dP = 0
# Radial scaling
ratio = (a_ref / r) ** (n + 2)
# Accumulate components
cos_m_lon = np.cos(m * lon_rad)
sin_m_lon = np.sin(m * lon_rad)
X += ratio * (g * cos_m_lon + h * sin_m_lon) * dP
Y += ratio * m * (g * sin_m_lon - h * cos_m_lon) * P / np.sin(theta) if theta != 0 else 0
Z -= ratio * (n + 1) * (g * cos_m_lon + h * sin_m_lon) * P
return X, Y, Z
def calculate_elements(X, Y, Z):
"""Calculate all seven magnetic elements from X, Y, Z."""
H = np.sqrt(X**2 + Y**2)
F = np.sqrt(X**2 + Y**2 + Z**2)
D = np.degrees(np.arctan2(Y, X)) # Declination
I = np.degrees(np.arctan2(Z, H)) # Inclination
return {
'X': X, # nT
'Y': Y, # nT
'Z': Z, # nT
'H': H, # nT
'F': F, # nT
'D': D, # degrees
'I': I # degrees
}
Magnetic Inclination (Dip)
Definition and Significance
Magnetic inclination (dip angle, \(I\)) is the angle between the horizontal plane and the total magnetic field vector. It varies from:
-
0° at the magnetic equator (horizontal field)
-
+90° at the north magnetic pole (pointing straight down)
-
-90° at the south magnetic pole (pointing straight up)
The Magnetic Equator (Aclinic Line)
The aclinic line (magnetic equator) is where inclination = 0°. It does NOT coincide with the geographic equator:
160°W 120°W 80°W 40°W 0° 40°E 80°E 120°E 160°E
│ │ │ │ │ │ │ │ │
12°N┼───────┼───────┼───────┼──────┼───────┼───────┼───────┼───────┼
│ │ │ │ │ │ │ │ │
│ │ │ ╱──┼──────┼───────┼──╲ │ │ │
│ ╱────┼───────┼───╱ │ │ │ ╲───┼───────┼────╲ │
│ ╱ │ │ ╱ │ │ │ ╲ │ │ ╲ │
0°N┼───────┼───────┼───────┼──────┼───────┼───────┼───────┼───────┼
│ ╲ │ │ ╲ │ │ │ ╱ │ │ ╱ │
│ ╲────┼───────┼───╲ │ │ │ ╱───┼───────┼────╱ │
12°S┼───────┼───────┼───────┼──────┼───────┼───────┼───────┼───────┼
│ │ │ │ │ │ │ │ │
↑
Magnetic Equator (I = 0°)
Maximum deviation: ~12° from geographic equator
Dip Angle Formula (Dipole Approximation)
For a centered dipole model:
Where \(\phi_m\) is the magnetic latitude (angle from magnetic equator).
At the magnetic poles (\(\phi_m = \pm 90°\)):
Effect on Compass Operation
|
Dip Circle Error Near magnetic poles, high inclination causes severe compass errors:
|
At 80°N magnetic latitude (I ≈ 83°):
Isoclinic Lines
Lines connecting points of equal magnetic inclination:
| Region | Inclination | Compass Reliability |
|---|---|---|
Equatorial (±10° mag lat) |
-10° to +10° |
Excellent |
Temperate (30-50° mag lat) |
±45° to ±70° |
Good |
Sub-polar (60-75° mag lat) |
±75° to ±85° |
Marginal |
Polar (>75° mag lat) |
±85° to ±90° |
Unreliable |
Compass Types
Baseplate Compass (Silva/Suunto type)
Direction of travel arrow
↑
┌─────────┴─────────┐
│ │
│ ╭─────────╮ │
│ │ N │ │ ← Rotating bezel (declination adjustment)
│ │ ╱ ╲ │ │
│ │ W E │ │ ← Magnetic needle (red end = North)
│ │ ╲ ╱ │ │
│ │ S │ │
│ ╰─────────╯ │
│ │ ← Baseplate (transparent for map work)
│ ──────────────── │ ← Orienting lines
│ │
└───────────────────┘
Lensatic Compass (Military)
Sighting wire
│
┌────────┼────────┐
│ Cover │ │
│ ╲ │ ╱ │
│ ╲ │ ╱ │
│ ╲ │ ╱ │
│ ╲ │ ╱ │ ← Lens for reading dial
│ ╲ │ ╱ │
│ ╲│╱ │
│ N │
│ W E │ ← Floating dial (mils or degrees)
│ S │
└─────────────────┘
Degrees vs Mils
| System | Full Circle | 1 Unit Equals |
|---|---|---|
Degrees |
360° |
1° = 17.78 mils |
Mils (NATO) |
6400 mils |
1 mil ≈ 0.0563° |
Mils (Warsaw) |
6000 mils |
1 mil = 0.06° |
At 1000m range, 1 mil = 1 meter of lateral displacement.
Grid-Magnetic Angle (G-M Angle)
The G-M Angle is the combined effect of grid convergence and magnetic declination.
To convert GRID azimuth to MAGNETIC azimuth:
1. Read the G-M Angle from map margin diagram
2. Apply as shown in the diagram
Example:
Map shows: GN is 2° East of TN
MN is 12° East of TN
G-M Angle = 14° (MN is 14° East of GN)
Grid azimuth from map: 090°
Magnetic azimuth for compass: 090° - 14° = 076°
Practical Declination Application
Setting Declination on Baseplate Compass
1. Locate declination adjustment screw (small screw on bezel)
2. Using screwdriver or key:
- For EAST declination: Rotate orienting arrow EAST (clockwise)
- For WEST declination: Rotate orienting arrow WEST (counter-clockwise)
3. Set to your local declination value
4. Now compass reads TRUE bearings directly
Field Expedient Method (No Adjustment)
1. Read magnetic bearing from compass
2. Apply declination mentally:
- East declination: ADD to get True
- West declination: SUBTRACT to get True
Example (12°E declination):
Compass reads: 045° Magnetic
True bearing: 045° + 12° = 057° True
Declination Lookup
CLI Calculation
# Using geomag library
pip install geomag
python3 << 'EOF'
import geomag
from datetime import date
# McAllen, TX coordinates
lat, lon = 26.2034, -98.2300
today = date.today()
declination = geomag.declination(lat, lon, today)
print(f"Declination at McAllen, TX: {declination:.2f}°")
print(f"Direction: {'East' if declination > 0 else 'West'}")
EOF
From Your Nav Library
source examples/navigation/nav-calc.sh
# Convert magnetic to true
apply_declination 45 12 E # 57.00 (12°E declination)
apply_declination 45 16 W # 29.00 (16°W declination)
Compass Deviation
Deviation vs Declination
Critical distinction:
| Error Source | Declination (\(\delta\)) | Deviation (\(\Delta\)) |
|---|---|---|
Cause |
Earth’s magnetic field |
Local magnetic interference (ship/aircraft) |
Varies with |
Geographic location |
Vessel heading |
Predictable |
Yes (IGRF/WMM models) |
Must be measured empirically |
Changes over time |
Slowly (secular variation) |
With equipment changes |
Correction |
Applied from charts/models |
Applied from deviation table |
The Compass Correction Formula
The complete relationship between True (T), Magnetic (M), and Compass © headings:
Or using the mnemonic "TVMDC ADD WEST" (True-Variation-Magnetic-Deviation-Compass):
T V M D C
↓ ↓ ↓ ↓ ↓
TRUE → MAGNETIC → COMPASS
↑ add West ↑ add West
↓ subtract ↓ subtract
Going DOWN (T to C): Add West, Subtract East
Going UP (C to T): Subtract West, Add East
Swinging the Compass
"Swinging" is the procedure to determine deviation on multiple headings. Required after:
-
Installation of new equipment
-
Major structural changes
-
Suspected magnetic contamination
-
Annual certification (ships/aircraft)
1. Position vessel at a known location with reference marks
2. Use pelorus or gyro compass as reference for TRUE headings
3. Steady on each cardinal and intercardinal heading (8 points minimum)
4. Record compass reading vs true heading at each point
5. Calculate deviation: δ = True - Compass - Declination
6. Construct deviation table/curve
Standard headings: 000°, 045°, 090°, 135°, 180°, 225°, 270°, 315°
Deviation Table Format
| Heading | 000° | 045° | 090° | 135° | 180° | 225° | 270° | 315° |
|---|---|---|---|---|---|---|---|---|
Deviation |
+2°W |
+1°W |
0° |
-1°E |
-2°E |
-1°E |
0° |
+1°W |
|
Deviation follows a predictable pattern based on hard and soft iron effects:
The combined effect typically produces a sinusoidal deviation curve with two peaks per revolution. |
Mathematical Model of Deviation
The deviation can be modeled using Fourier coefficients:
Where:
-
\(A\) = Constant coefficient (lubber line error, soft iron asymmetry)
-
\(B\) = Semicircular deviation (athwartship hard iron)
-
\(C\) = Semicircular deviation (fore-aft hard iron)
-
\(D\) = Quadrantal deviation (induced magnetism)
-
\(E\) = Quadrantal deviation (induced magnetism)
-
\(\psi\) = Magnetic heading
| Coefficient | Physical Cause | Correction |
|---|---|---|
A |
Lubber line misalignment, asymmetric soft iron |
Adjust lubber line, degauss |
B, C |
Permanent magnets (hard iron) |
Corrector magnets |
D, E |
Induced magnetism in soft iron |
Flinders bar, quadrantal spheres |
Heeling Error
When a vessel heels (rolls), vertical components of magnetism affect the compass. Particularly important in:
-
Sailing vessels
-
Small craft in heavy seas
-
Aircraft banking
Where:
-
\(k\) = Heeling error coefficient
-
\(Z\) = Vertical component of Earth’s field
-
\(\theta_{heel}\) = Angle of heel
|
High Latitude Heeling Error Near magnetic poles, the vertical component (Z) is large, so heeling errors become severe:
Solution: Heeling error corrector magnet (vertical) |
Magnetic Anomalies
Local Magnetic Disturbances
The WMM and IGRF models represent the main field only. Local anomalies arise from:
-
Geological formations: Iron ore deposits, volcanic rock
-
Man-made structures: Steel bridges, pipelines, power lines
-
Vehicle-borne interference: Vehicle engines, electronics
| Location | Cause | Effect |
|---|---|---|
Kursk Magnetic Anomaly (Russia) |
Iron ore (30-40% magnetite) |
Declination varies ±10° over km |
Swedish Lapland (Kiruna) |
Iron ore mining |
Compass unreliable in mining areas |
South Atlantic Anomaly |
Weak field region |
GPS affected, compass sluggish |
Bermuda Triangle (myth) |
Normal field (no anomaly) |
Declination changes rapidly with longitude |
Field Survey for Anomalies
Before establishing navigation aids or conducting precision surveys:
1. Grid the area with 100m spacing
2. Record magnetic elements at each point
3. Compare with WMM/IGRF predictions
4. Map residuals (observed - predicted)
5. Contour anomaly regions
6. Mark anomaly zones on charts/maps
Geomagnetic Storms
Space Weather Effects
Geomagnetic storms occur when solar wind disturbs Earth’s magnetosphere. Effects on navigation:
| Level | Kp Index | Navigation Effect |
|---|---|---|
G1 (Minor) |
Kp = 5 |
Minimal (<1° declination shift) |
G2 (Moderate) |
Kp = 6 |
Compass fluctuations (1-2°) |
G3 (Strong) |
Kp = 7 |
High-latitude compass errors (3-5°) |
G4 (Severe) |
Kp = 8 |
GPS degraded, compass unreliable above 60° |
G5 (Extreme) |
Kp = 9 |
Widespread navigation system failures |
Mathematical Description
During a geomagnetic storm, the external (magnetospheric) field adds to the main field:
The disturbance storm-time index (Dst) measures ring current intensity:
Where:
-
\(E_{ring}\) = Ring current energy
-
\(R_E\) = Earth radius
-
\(k\) = Geometrical factor
| Dst (nT) | Storm Phase | Compass Effect |
|---|---|---|
> 0 |
Sudden commencement |
Initial compass deflection |
-30 to 0 |
Quiet or recovery |
Normal operation |
-50 to -30 |
Minor storm |
Slight variations |
-100 to -50 |
Moderate storm |
Noticeable variations (1-3°) |
< -100 |
Intense storm |
Significant errors (>3°) |
< -250 |
Superstorm |
Compass unreliable |
Navigation During Geomagnetic Storms
|
Operational Guidance
|
Historical Notable Storms
| Event | Peak Dst | Effects |
|---|---|---|
Carrington Event (1859) |
Est. -1760 nT |
Telegraph systems failed globally |
March 1989 Storm |
-589 nT |
Quebec blackout, GPS errors |
Halloween Storms (2003) |
-353 nT |
Aviation rerouting, GPS degraded |
St. Patrick’s Day (2015) |
-223 nT |
Compass irregularities reported |
Backup Navigation Methods
When Magnetic Compass Fails
In situations where magnetic compass is unreliable (polar regions, magnetic storms, local anomalies):
| Method | Requirements | Accuracy |
|---|---|---|
Directional Gyro (DG) |
Working gyroscope, initial heading |
<1° (requires periodic reset) |
Astro Compass |
Clear sky, known time, almanac |
±0.5° (daytime with sun) |
Sun Compass |
Clear sky, watch, latitude |
±2° (shadow method) |
Inertial Navigation System (INS) |
Functional INS |
<0.1°/hour drift |
GPS Heading |
2+ GPS antennas (vector) |
±0.5° (baseline dependent) |
Terrain Association |
Visible landmarks, map |
Position-based (no heading) |
Sun Compass Procedure
For emergency navigation when magnetic compass fails:
1. Plant a straight stick vertically
2. Mark shadow tip position at time T1
3. Wait 15-30 minutes
4. Mark shadow tip position at time T2
5. Draw line from T1 to T2
6. This line runs approximately East-West
7. Perpendicular to this line = North-South axis
Accuracy: ±5° (improves with longer wait time)
Note: More accurate near noon when shadow moves fastest
1. Point hour hand at the sun
2. Bisect angle between hour hand and 12 o'clock
3. This line points approximately South (before noon) or North (after noon)
Correction for Daylight Saving Time:
- Use 1 o'clock instead of 12 o'clock
Accuracy: ±15° (depends on latitude and time of year)
Exercises
Drill 1: Declination Conversion
-
Magnetic: 090°, Declination: 8°E
-
Magnetic: 270°, Declination: 15°W
-
Magnetic: 045°, Declination: 3°E
-
Magnetic: 315°, Declination: 20°W
-
True: 180°, Declination: 12°E
-
True: 000°, Declination: 10°W
-
True: 225°, Declination: 5°E
-
True: 135°, Declination: 18°W
Drill 2: Map Reading
Your map shows: - Date: 2015 - Declination: 14°30' East - Annual change: 0°8' West
Calculate current declination for 2025.
Drill 3: Field Problem
You need to travel from Point A to Point B.
-
Map bearing (grid): 067°
-
Grid convergence: 2° West
-
Declination: 11° East
What compass bearing should you follow?
Drill 4: Deviation Table Application
A ship’s deviation table shows:
| Heading | Deviation |
|---|---|
000° |
3°W |
045° |
1°E |
090° |
4°E |
135° |
2°E |
180° |
2°W |
225° |
4°W |
270° |
3°W |
315° |
1°W |
Local declination: 8°E
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You want to steer True course 090°. What compass heading should you use?
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Your compass reads 225°. What is your True heading?
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Interpolate deviation for magnetic heading 067°.
Drill 5: IGRF Calculation
Given IGRF coefficients \(g_1^0 = -29351.8\) nT, \(g_1^1 = -1410.2\) nT, \(h_1^1 = 4545.4\) nT:
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Calculate the dipole component of the field at 45°N, 0°E
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Estimate declination using only degree-1 terms
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What is the expected horizontal intensity?
Drill 6: Geomagnetic Storm Assessment
A CME (Coronal Mass Ejection) is predicted to arrive. Space weather forecast shows:
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Kp = 7 (G3 storm)
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Dst = -120 nT
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Duration: 12 hours
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What navigation precautions should be taken?
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Above what latitude will magnetic compass be unreliable?
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What backup systems should be activated?
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Drill 7: Heeling Error (Maritime)
A sailing vessel at magnetic latitude 55°N heels 20° in a gust.
Given: * Vertical field component Z = 45,000 nT * Horizontal field component H = 20,000 nT * Heeling coefficient k = 0.02
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Calculate the heeling error
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What corrective action is available?
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Would this error be worse at 70°N magnetic latitude?
Quick Reference Card
| Conversion | Formula |
|---|---|
Magnetic → True (East dec) |
True = Magnetic + Declination |
Magnetic → True (West dec) |
True = Magnetic - Declination |
True → Magnetic (East dec) |
Magnetic = True - Declination |
True → Magnetic (West dec) |
Magnetic = True + Declination |
"East is least, West is best" (True → Magnetic) "Declination East, Compass least" (True → Magnetic) "CADET" - Compass Add Declination Equals True (for West) "MTC" - Magnetic To Compass (add West, subtract East)
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Continue to Time & Longitude for the relationship between time, position, and celestial navigation.