Navigation — AeroplanesLektion 4 von 34
04/34The Earth and coordinates

Solar System, Earth Rotation and Seasons

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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:

DateDeclination
21 March (spring equinox)
21 June (summer solstice NH)+23.5° (north)
23 September (autumn equinox)
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.
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