One way to measure Earth's curvature is by comparing true vertical from plumb lines at two points with the straight line of sight between them. Any angular deviation reveals the Earth's curvature.
Between two stations A and B separated by distance D
, the sightline forms angles θA
and θB
with true vertical. Sum of these angles equals the central angle of Earth's curvature.
On a flat lake surface, points A and B are at equal elevation. The vertical drop h
between the plumb line at B and the tangent gives:
h ≈ D² / (2R)
(small-angle approximation)
Thus R ≈ D² / (2h)
.
For D = 1000 m
and observed drop h = 0.0785 m
:
R ≈ (1000²) / (2 × 0.0785) ≈ 6.37 × 106 m
(close to the true radius)
With elevation difference ΔH
, the observed angle:
φ = (θA − θB) + arctan(ΔH / D)
For small φ (in radians): R ≈ D / φ
.
Let D=500 m
, θA=0.02°
, θB=−0.015°
, ΔH=5 m
.
Convert to radians: θA=0.000349, θB=−0.000262;
arctan(5/500)=0.009999;
φ≈0.000349−(−0.000262)+0.009999=0.010610 rad;
R≈500/0.010610≈4.71×104 m.