The Earth-Moon system

Scale

Goal: get the Earth-Moon distance right in your head. Almost every diagram you have ever seen has lied to you about it.


Predict

Take a ball about 10 cm across; that is Earth, roughly to scale.

  1. How big is the Moon at that scale? Pick an object.
  2. How far away do you put it? Guess in centimetres, before measuring.

Write both down. Most people are wrong about the second by a factor of five or more.


Run

from moonfield import moon
import datetime as dt
from moonfield import time as mtime

p = moon.position(mtime.utc_now())
print(f"distance right now: {p.distance_km:,.0f} km")

The numbers:

QuantityValueAt 10 cm Earth
Earth diameter12,742 km10 cm
Moon diameter3,475 km2.7 cm
Mean distance384,400 km302 cm

Three metres. A tennis ball, three metres from a football.

Textbook diagrams almost always show the Moon a few Earth-diameters away, because the true spacing does not fit on a page. That distortion quietly sabotages your intuition about eclipses, tides and orbits.

Go and lay it out on the floor. It is worth the two minutes.


The consequence you can check

At that distance the Moon subtends about 0.52°, half a degree. So does the Sun, which is 400 times larger and 400 times further away. That coincidence is why total solar eclipses exist at all, and why they are so nearly-not-quite.

from moonfield import moon, sun
print(f"Moon: {moon.angular_diameter(mtime.utc_now()):.4f} deg")
print(f"Sun:  {sun.angular_diameter(mtime.utc_now()):.4f} deg")

Half a degree is about the width of your little fingernail at arm's length. Check it against the real Moon tonight. Almost everyone thinks the Moon is bigger than that, see the Moon Illusion in Go and look.


Checkpoint

Questions to think about

change your sense of the achievement?

600 million years?

Next: Tidal locking.