The solar system and the Earth — navigation basics
Understanding the Earth's motion in the solar system matters for navigation because:
- Sun position determines daylight and visibility,
- Seasons affect sunrise and sunset times,
- Earth rotation is the basis of time measurement,
- Magnetic variation changes slowly due to core circulation.
The Earth
Structure:
- Core (solid inner + liquid outer, mostly iron),
- Mantle (silicate rock),
- Crust (continental + oceanic).
Shape:
- Geoid — actual shape, slightly flattened at the poles.
- Ellipsoid — simplified mathematical model (WGS-84 in aviation).
- Equatorial radius: 6 378 km.
- Polar radius: 6 357 km.
- Flattening: about 1/298.
Axis:
- The Earth's axis passes through the geographic poles.
- Tilted about 23.5° from the perpendicular to the orbital plane (ecliptic).
- This tilt is the main cause of the seasons.
Earth rotation — day and night
Properties:
- Earth rotates from west to east (counter-clockwise viewed from above the North Pole).
- One complete rotation takes ~23 h 56 min 4 s (sidereal day).
- Mean solar day (noon to noon) = 24 h (4 minutes longer due to orbital motion).
- Rotational speed at the equator: ~1 670 km/h (465 m/s).
Terminator (day-night line):
- Separates lit and dark hemispheres.
- Moves westward across the globe at 360°/24 h = 15°/h.
Example: New York is 5 hours behind Berlin → 5 × 15° = 75° west.
Earth orbit around the Sun
Properties:
- One orbit (revolution) takes ~365.25 days (leap year correction).
- Orbit is elliptical, not circular.
- Perihelion (closest to Sun): ~3 January — Earth 147 Mkm from Sun.
- Aphelion (farthest): ~4 July — Earth 152 Mkm from Sun.
The Earth's axial tilt causes the seasons — NOT the varying distance from the Sun!
The seasons
Because of the 23.5° tilt, each pole sees different amounts of sunlight during the year:
Northern Hemisphere
Summer solstice — about 21 June:
- North Pole tilted toward the Sun.
- Longest day in the north.
- Sun reaches the Tropic of Cancer (23.5° N).
- Midnight sun north of the Arctic Circle (66.5° N).
Autumn equinox — about 23 September:
- Sun directly over the equator.
- Day = night worldwide.
Winter solstice — about 22 December:
- North Pole tilted away from the Sun.
- Shortest day in the north.
- Sun reaches the Tropic of Capricorn (23.5° S).
- Polar night north of the Arctic Circle.
Spring equinox — about 21 March:
- Sun again over the equator.
Southern Hemisphere
Mirror image of the north — when Berlin has summer, Buenos Aires has winter.
Implications for pilots
Daylight duration
Mid latitudes (e.g. 50° N, central Europe):
- Summer: up to 17 h day (21 June).
- Winter: only 7.5 h day (22 December).
Consequence: cross-country flights in winter require strict timing relative to sunset.
Sun elevation
Sun elevation at noon (observer site, sun in the south):
- Summer solstice: 90° − latitude + 23.5°. Berlin (52.5° N): 90° − 52.5° + 23.5° = 61°.
- Winter solstice: 90° − latitude − 23.5°. Berlin: 90° − 52.5° − 23.5° = 14°.
Consequence: in winter the sun is low in the south → significant glare on approaches to southern runways.
Solar wind and magnetic variation
Solar activity (sunspots, corona, coronal mass ejections) influences:
- Ionosphere → HF radio propagation,
- Earth magnetic field → slight magnetic-variation drift,
- GPS accuracy during severe solar events.
In a solar maximum (every ~11 years) HF communication is disrupted and GPS may show reduced accuracy.
Polar night and polar day
In regions north of the Arctic Circle (66.5° N):
- Polar night in winter — no Sun for weeks.
- Midnight sun in summer — no night.
- Relevant for flights in northern Scandinavia, Iceland, Greenland.
Solar declination
Solar declination δ is the angular position of the Sun north/south of the equator:
| Date | Declination |
|---|---|
| 21 March (spring equinox) | 0° |
| 21 June (summer solstice NH) | +23.5° (north) |
| 23 September (autumn equinox) | 0° |
| 22 December (winter solstice NH) | −23.5° (south) |
Declination is used in astronomical almanacs and sunrise/sunset tables.
Moon orbit and tides (background)
The Moon orbits the Earth in ~27.3 days and together with the Sun causes the tides. Not directly relevant to standard PPL navigation, except:
- Moonlight at night — a full moon can greatly improve VFR visibility.
- Spring/neap tides for seaplane operations.