Experiment

Rainy Lake Curvature Field Test

Over a long frozen-lake sightline, do Bedford and Tangent target rows match globe hidden-height predictions better than a flat-plane expectation?

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Materials Needed

  • frozen lake or very flat water crossing with ~6–10 km clear line of sight
  • auto level, theodolite, or survey-grade leveling setup
  • printed targets with a visible center gap (Bedford 1.85 m row + Tangent row)
  • GPS or differential GNSS for waypoint logging (phone GPS is approximate only)
  • camera or scope for photo documentation
  • notebook or this page's field log for observations

Setup Steps

  1. Mark an observer position and three or more targets along a straight ice path, the Bislin Rainy Lake layout uses Bedford targets at 1.85 m and Tangent targets scaled for a 3.91 m observer.
  2. Record waypoint coordinates and GNSS or tape-measured distances; note weather, refraction, and whether the crosshair sits in each target gap.
  3. Log observer height (Bedford 1.85 m or Tangent 3.91 m preset) and whether each target appears full, partial, or hidden.
  4. Compare each sightline with the Curvature Calculator using the same distance, heights, and refraction mode.
  5. Treat this lite protocol as educational, not a substitute for professional survey, and repeat on a clearer day if heat shimmer or inversion layers dominate.

Expected Calculation

dobs=√2Rh + h2
dbeyond=max(d − dobs, 0)
hidden=dbeyond22Reff
sagitta=Reff (1 − cos(d2Reff))
clearance=max(targetHeight − hidden, 0)

On a sphere, the Bedford row should curve below a 1.85 m observer while the Tangent row should stay near eye level for a 3.91 m observer when refraction is accounted for. A flat plane predicts the opposite pattern for the two rows.

Graphic

What to Observe

  • Bedford targets drop below eye level with distance while Tangent targets stay much closer to the leveled line for the higher observer.
  • Hidden amounts grow with distance in a way that matches spherical geometry when refraction is included.
  • Raising the observer or switching from Bedford to Tangent mode restores more of the distant structure.

Interpretation

When predictions from the same curvature math are logged beside field observations, the Rainy Lake pattern matches a convex Earth much better than a flat-plane plus ad hoc refraction story. Credit for the original 2018 field test: George Hnatiuk (design and construction), Jesse Kozlowski (GNSS surveying), Soundly (imaging), and Walter Bislin (analysis and published data).

Sources

Evidence Card

Claim

Over a ~10 km frozen-lake baseline, a Bedford target row at 1.85 m should curve below a 1.85 m observer while a Tangent row should stay near eye level for a 3.91 m observer, the classic predict-vs-observe split between flat and globe models.

Model Used

Bislin-inspired Rainy Lake lite protocol: GNSS-referenced waypoint distances on Rainy Lake MN, Bedford/Tangent observer and target heights, and the same hidden-height pipeline as the Curvature Calculator with optional standard or custom refraction.

Formula

dobs=√2Rh + h2
dbeyond=max(d − dobs, 0)
hidden=dbeyond22Reff
sagitta=Reff (1 − cos(d2Reff))
clearance=max(targetHeight − hidden, 0)

Last Verified

2026-06-30

Assumptions

  • Waypoint coordinates are an educational preset aligned to published Bislin GNSS distances, not a differential-GNSS survey deliverable.
  • Field log observations are user-entered paraphrases; photos are not hosted on this page.
  • Refraction is logged as a note because Bislin measured k ≈ 0.17 during the original experiment.

What Would Falsify This Page

If logged Bedford/Tangent observations over the preset distances matched flat-eye-level predictions for both rows while sphere+refraction predictions failed across all three targets, the globe framing on this page would be weakened.

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