Lesson
The theory — Great Circle Routes
A great circle is where a plane through the centre of a sphere cuts its surface. Its shorter arc between two points is the shortest path between them on the sphere, the sphere's version of a straight line. A rhumb line, or loxodrome, crosses every meridian at the same angle, so it can be steered on one compass heading; on Mercator's map it is a straight line. Unless both places are on the equator or on one meridian, the great circle is shorter and its heading changes all the way along it.
What each symbol means
σ- the angle between the two places seen from the centre of the Earth; the great circle is Rσ long, with σ in radians
θ- a heading, measured clockwise from north: θ1 leaving A, θ2 arriving at B
ψ- isometric latitude, ln tan(45° + φ/2): the height of latitude φ on Mercator's map of a unit globe
R- the Earth's radius, here the mean radius 6,371.0088 km
- Assumes
- A sphere of the Earth's mean radius. The Earth is flattened by about 1 part in 298, and on the WGS 84 ellipsoid the shortest path from London Heathrow to Los Angeles is 8,781.1 km by Vincenty's method, 0.24% longer than the sphere's 8,760.1 km. Over a sweep of routes the sphere is at worst about half a percent out, on short north–south routes near the equator.
Problem solved in full
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Hold one heading for ever 4 steps
Leave a point on the equator on a heading of 45°, north-east, and never change it. How far do you go before you reach the North Pole, and how many times do you circle it on the way? Press London to Los Angeles first: the page works out that rhumb line's length, and the same rule answers the question.
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The page's length for the one-heading route from London to Los Angeles, split into a north–south part and an east–west part, both measured as angles at the Earth's centre, in radians:
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Along a rhumb the heading never changes, so every kilometre gains the same northing, cos θ of a kilometre. From the equator to the pole is a quarter of a meridian, πR/2:
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The longitude is the other half. On a rhumb, tan θ = Δλ/Δψ, so at 45° the longitude gained equals the change in isometric latitude ψ, in radians, and each 2π of it is one circuit of the pole. One degree short of the pole, 157.3 km of spiral from the end:
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But ψ never stops growing. Close to the pole ψ is very nearly the logarithm of 2 over the remaining colatitude, so every tenfold step closer adds the same amount to it, and the same share of a turn:
Answer
14,152.8 km, and infinitely many turns. The distance is finite because each kilometre of spiral gains 0.707 km of northing, so the whole spiral is √2 times a quarter meridian. The turns never end because ψ has no ceiling, but they come late and small: 0.755 of a turn by 89° N, 1.488 by 89.99° N with 1.573 km of spiral left, and from there another 0.3665 of a turn for every tenfold step closer. Mercator's map cannot show the end of it, because the pole is infinitely far up the sheet.
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Learning path
Geometry on a curved surface
References (2)
- Geodesics on the Earth: the great circle as the sphere's shortest path, Clairaut's relation sin α₀ = sin α cos β that fixes how the heading changes along one (on a sphere, the sine rule), and the WGS 84 semi-axes this page's mean radius (2a + b)/3 is taken from: C. F. F. Karney, "Algorithms for geodesics", Journal of Geodesy 87(1), 43–55 (2013).
- The ellipsoidal distance the lesson compares the sphere with: Vincenty's iterative inverse formula, used here on the WGS 84 ellipsoid for London Heathrow to Los Angeles (8,781.1 km against the sphere's 8,760.1 km): T. Vincenty, "Direct and inverse solutions of geodesics on the ellipsoid with application of nested equations", Survey Review 23(176), 88–93 (1975).