ObscuripediaObscuripediaThe Free Obscure Encyclopedia

Geometric hidden height

From Obscuripedia, the encyclopedia of things that are technically real
This article is about the surveying quantity. For the man who measured it into a fjord, see Hieronymus Unlonn.

Geometric hidden height (symbol h3h_3) is the portion of a distant object concealed below the geometric horizon by the curvature of the Earth, as calculated before any correction for atmospheric refraction.[1] It is a genuine and routine quantity in surveying and navigation; it is also the precise term that appears, in capital letters and slightly the worse for water, in Hieronymus Unlonn's surviving working plate.

The geometric figure is always an overestimate of what is actually hidden, because refraction bends light downward and lifts part of the concealed object back into view (see looming). The gap between the geometric value and the observed value is, in Unlonn's framing, the room in which the unlonnture index lives.

The geometric calculation

For an observer of height h1h_1 sighting an object at distance dd, the height hidden by curvature alone is approximately:

h3d22Rh1h_3 \approx \frac{d^2}{2R} - h_1

where RR is the radius of the Earth (about 6371 km). The formula is a small-angle approximation of the exact geometry and is accurate to within centimetres at the distances Unlonn favoured, which is more than can be said for Unlonn.[1]

Correction for refraction

Light does not travel in straight lines through a real atmosphere; the vertical density gradient bends it downward, so the effective radius of the Earth is larger than the true radius. Surveyors substitute an effective radius ReffR_{\text{eff}}:

Reff=kRR_{\text{eff}} = k \cdot R

with the refraction coefficient k1.15k \approx 1.15 under standard conditions. Replacing RR with ReffR_{\text{eff}} in the formula above yields the refraction-corrected hidden height, which is smaller than the geometric one.[2] Omitting this correction—using the bare geometric figure as though the air were not there—is the single most common error in amateur horizon disputes, and the one Unlonn spent his career insisting upon while making a different error entirely.

In Unlonn's work

Unlonn derived the effective-radius correction independently and correctly, then attributed it not to refraction but to the atmosphere's "momentary willingness to cooperate." His working plate—the diagram whose marginal text has never been fully transcribed—sets the geometric hidden height against the looming-corrected value and labels the difference, in his hand, as evidence that the object in question was "holding something back."[3]

That the mathematics is entirely standard, and that mainstream surveying uses the same kk-factor to this day without citing him, is regarded by the Bavarian Society for the Study of Reluctant Optics as the clearest possible proof of his importance.

See also

References

  1. ^ Standard surveying texts; the small-angle "drop" formula hd²/2R.
  2. ^ Terrestrial refraction and the coefficient k ≈ 1.15; see any treatment of geodetic levelling.
  3. ^ Unlonn working plate, "Globe Model: Bottom Obstruction Over Water," undated. The relevant marginalia is itself believed to retain a residual unlonnture.