What Is the Radar Horizon?
The radar horizon is the maximum distance at which a radar system can detect a target, limited by Earth’s curvature and atmospheric refraction. Unlike the visual horizon, radar waves bend slightly downward due to atmospheric density gradients, effectively extending the detection range by about 15% under standard conditions.
Formulas
Simplified (h « R):
Where k = 4/3, R_e = 6371 km, heights in metres.
The k-Factor
| k-Factor | Condition | Effect |
|---|---|---|
| 1.0 | No atmosphere (geometric) | Baseline horizon |
| 4/3 (1.333) | Standard atmosphere | ~15% extension |
| 2.0 | Super-refraction | ~22% extension |
| < 1.0 | Sub-refraction | Reduced range |
Applications
- Marine radar — ship-to-ship and ship-to-shore detection range.
- Air traffic control — radar coverage for aircraft detection.
- Military radar — low-flying target detection limits.
- Radio communications — VHF/UHF link planning.
How to Use
- Enter radar antenna height and target height.
- Set k-factor (default 4/3 for standard atmosphere).
- Click Calculate to see detection range with geometric comparison.
Examples
Ship radar (25m antenna, surface target)
d ≈ 4.12 × √25 = 4.12 × 5 = 20.6 km
ATC radar (30m, aircraft at 10,000m)
d ≈ 4.12 × (√30 + √10000) = 4.12 × (5.48 + 100) = 434 km
FAQ
What is the k-factor in radar horizon calculations?›
The k-factor (or effective Earth radius factor) models how atmospheric refraction bends radio waves. k = 4/3 (1.333) is standard for temperate climates. The effective Earth radius is R_eff = k × R_Earth, making calculations equivalent to straight-line propagation on a larger Earth.
How does the radar horizon differ from the visual horizon?›
The radar horizon is typically farther because radio waves bend more than visible light in the atmosphere. Standard visual horizon uses k ≈ 1.07-1.17, while radar uses k ≈ 4/3 (1.333). This means radar can 'see' about 15% farther than the eye.
What is ducting and how does it affect radar?›
Atmospheric ducting occurs when extreme temperature inversions trap radio waves in a layer near the surface, effectively making k → ∞. This can extend radar range hundreds of kilometers beyond normal, but is unpredictable and can also create blind spots.
Why is the simplified formula d ≈ 4.12√h used?›
This approximation drops the h² term (valid when h << R_Earth) and uses R_Earth = 6371 km with k = 4/3: d = √(2 × 4/3 × 6371000 × h) ≈ 4120√h metres = 4.12√h km. It's accurate to within 1% for heights below 1000 m.
Sources

Author & technical reviewer
Manish Kumar
PhysicsCalcs tools are reviewed with an educational focus: clear formulas, transparent assumptions, and practical context for students and science learners.
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