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Gnomonic Projection

A center-of-sphere mapping of an open hemisphere to a tangent plane that turns visible great-circle arcs into straight lines.

Version
v1 · 2026-10-03 · History
Domain-specific #
13280
Domain group
Natural Sciences
Origin domain
Geology & Earth Sciences
Subdomains
Mathematical Cartography, Spherical Map Projections → Geology & Earth Sciences
Aliases
Central Azimuthal Projection, Gnomic Projection

Core Idea

Gnomonic projection maps points on a sphere's plane-facing open hemisphere to a tangent plane by drawing rays from the sphere's center. A visible great-circle arc becomes a straight line because its plane, which passes through the sphere center, intersects the tangent plane in a line. This exact property makes a spherical great-circle problem easier to inspect on a flat chart.[ref-9dc47650721e][ref-d6c1a8abf8d4]

The benefit has a sharp boundary. At angular distance \(c\) from the tangent point, planar radius is \(\rho=R\tan c\) for sphere radius \(R\). As \(c\) approaches \(90^\circ\), the image moves to infinity: no finite chart shows a whole hemisphere. Scale, shape and area distortion rise rapidly away from the center. A straight chart line is therefore not a faithful length or area measure.[ref-9dc47650721e][ref-d6c1a8abf8d4]

Scope of Application

On a spherical Earth model, a gnomonic chart can show the shape of a long great-circle route as a straight segment. A NOAA-hosted hydrographic manual describes transferring points from such a chart to a Mercator chart for subsequent course handling. A Mercator chart instead straightens constant-bearing rhumb lines, so the two charts have different jobs.[ref-e099818a3dcc][ref-56686b7785e5]

In astronomy, Starlink's positional-astronomy library maps nearby stellar right ascensions and declinations to gnomonic tangent-plane coordinates around a chosen sky center. Its plate model then treats optical distortion separately. The celestial sphere and terrestrial globe are unlike subject matters but instantiate the same sphere-center/tangent-plane geometry.[ref-15a049b93b65][ref-eaaf8d94688a]

Clarity

“Great circles are straight” means the portions inside the selected front hemisphere. A full great circle crosses the horizon and cannot appear on one finite gnomonic chart. The ordinary chart does not identify antipodal geographic or sky points, and its line property does not claim exact straightness for geodesics on a nonspherical Earth.[ref-9dc47650721e][ref-d6c1a8abf8d4]

Manages Complexity

The mapping compresses spherical great-circle shape into a planar line test. That helps route inspection and celestial tangent-plane coordinate work, but only if the chart center, domain and radial distortion remain visible. Using off-center map lengths as true distances or treating its line as a constant-bearing course would lose the very distinction the projection is meant to clarify.[ref-9dc47650721e][ref-e099818a3dcc]

Abstract Reasoning

Identify a sphere, its center and a tangent plane. Check that the target arc lies in the plane-facing open hemisphere. The great circle's plane passes through the center and meets the tangent plane in a line, so its visible arc maps to a line segment. Then ask whether the decision needs only the great-circle locus or also accurate distance, area, bearing, or ellipsoidal-geodesic results that this projection does not preserve.[ref-9dc47650721e][ref-d6c1a8abf8d4]

Knowledge Transfer

The role mapping transfers literally between geographic great-circle charting and a celestial star field: spherical source, central rays, tangent plane, finite front hemisphere, and rapidly rising distortion. Numerical chart scales and purposes do not transfer. No strict live DAG parent is asserted; the related broad Projection prime currently includes an idempotence condition that needs catalog review before this typed sphere-to-plane map can inherit it. A broader central-projection skeleton is a future-prime question.[ref-e099818a3dcc][ref-15a049b93b65]

[^ref-9dc47650721e]: John P. Snyder, Map Projections—A Working Manual, U.S. Geological Survey Professional Paper 1395 (1987), §22, pp. 164–168. https://pubs.usgs.gov/pp/1395/report.pdf . [^ref-d6c1a8abf8d4]: John P. Snyder and Philip M. Voxland, An Album of Map Projections, U.S. Geological Survey Professional Paper 1453 (1989), “Gnomonic Projection,” p. 116. https://pubs.usgs.gov/pp/1453/report.pdf . [^ref-e099818a3dcc]: Shalowitz, Interpretation and Use of Nautical Charts, chapter 6, p. 349 and note 150. https://nauticalcharts.noaa.gov/publications/docs/shore-and-sea-boundaries/volume-2/cse-library-shalowitz-v2-p2-ch6.pdf . [^ref-56686b7785e5]: U.S. Office of Coast Survey, “Nautical Cartography.” https://nauticalcharts.noaa.gov/learn/nautical-cartography.html . [^ref-15a049b93b65]: Starlink Project, SLALIB—Positional Astronomy Library, “SLA_S2TP.” https://starlink.eao.hawaii.edu/star/OLD_20240118/docs/sun67.htx/sun67ss166.html . [^ref-eaaf8d94688a]: Starlink Project, ASTROM Basic Astrometry Program, User Note 5.18, “Method,” p. 8. https://starlink.eao.hawaii.edu/docs/sun5.pdf .

Neighborhood in Abstraction Space

Gnomonic Projection sits in a moderately populated region (55th percentile for distinctiveness): it has near-neighbors but no dense thicket of look-alikes.

Family — Named Physical Phenomena & Theoretical Constructs (16 abstractions)

Nearest neighbors

Computed from structural-signature embeddings · 2026-10-08