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Astronomy

Earth's wandering pole

Scrub through 25,772 years. Follow the axis around the ecliptic pole and see why the pole star changes.

Earth's wandering pole — Actual application image
Actual application image

The model and its limits

Constant-rate axial precession with fixed obliquity. Nutation and planetary perturbations are omitted; celestial distances are illustrative.

Equations used in the module
Equations
ω = 2π/P; n = (sin ε cos ωt, cos ε, sin ε sin ωt).

Related experiments

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Earth's orbital climate rhythms — Actual application image

Astronomy / Earth

Earth's orbital climate rhythms

Compare eccentricity, tilt and precession with summer sunlight at a selected latitude. Move through 400,000 years.

Sunlight nudges an asteroid — Actual application image

Astronomy

Sunlight nudges an asteroid

Reverse the spin-axis tilt to reverse the diurnal Yarkovsky drift. Change thermal inertia to move the afternoon hot spot.

When planets migrate together — Actual application image

Astronomy

When planets migrate together

Compare slow and fast convergent migration. Watch an imposed 2:1 resonance retain the period ratio as the pair moves through the disk.