Navigation Hub / Tool 05

Line of Sight Horizon Calculator: Radio and Optical Range for US Navigation

The only US-focused LOS tool with three atmosphere models (ITU-R P.834 verified), Fresnel zone calculation for radio planning, a live Earth-curvature profile chart, and three computation modes: horizon distance, two-point LOS check, and minimum height required. Trusted for HAM radio, Coast Guard radar planning, and field navigation prep.

🌍 Three Atmosphere Models 📡 Fresnel Zone (ITU-R) 🔍 Earth Curvature Chart 📷 PDF Report ☀️ NOAA/FCC Referenced 💬 WhatsApp Share

Earth Curvature Math for Standard Atmospheric Refraction and Visual Range

Three modes for real-world LOS planning. Mode A: enter your height and get your visual or radio horizon. Mode B: two heights and a distance to get a go/no-go LOS status with Fresnel zone check. Mode C: enter a target distance and height to find the minimum observer antenna height required. All modes use ITU-R P.834-9 standard atmosphere (k=4/3) by default. Switch to geometric (k=1) for pure optics or custom k-factors for ducting and desert conditions.

H
ⓘ Standard atmosphere (k=4/3) per ITU-R P.834-9 is the accepted model for US radio planning. Use geometric (k=1) when computing strict optical horizon with no atmospheric bending.
Horizon Distance Results
Horizon Distance
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Nautical miles─
Geometric horizon (k=1)─
Standard atm (k=4/3)─
Active model─
H1
H2
D
LOS Check Results
Max LOS Distance─
LOS Margin─
Observer horizon (d1)─
Target horizon (d2)─
Earth Bulge at midpoint─
Fresnel zone (1st / 60%)─
LOS height at midpoint─
─
D
H2
ⓘ For HAM radio tower planning or cell site engineering: the target height is your remote station antenna height. The calculator returns the minimum local antenna height to achieve a geometric LOS over Earth curvature at the selected atmosphere model.
Required Height Results
Minimum Observer Height Required
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Target horizon already covers─
Observer horizon must cover─
Earth bulge at midpoint─
Atmosphere model─
Line of Sight Profile: Earth Surface, LOS Line, and Fresnel Zone (updates after each calculation)
The Science

Why Elevated Observers See Farther: Earth Curvature, Atmosphere, and Refraction Physics

Standing on a flat beach at eye level (about 1.7 meters), your horizon extends roughly 4.7 kilometers. Climb a 100-meter coastal bluff and your visual horizon grows to about 35.7 kilometers. From the deck of the Empire State Building at 381 meters, you can see roughly 69 kilometers to the horizon on a clear day. The math behind each of these numbers comes from a single principle: Earth curves away from you at a predictable rate, and the moment the surface curves below an imaginary straight line drawn from your eyes to infinity, you have hit your horizon. The geometry is governed by the Earth’s radius (6,371 kilometers, as defined by NOAA’s National Geodetic Survey for the WGS84 ellipsoid) and the height of the observer above the surface.

But optical geometry alone does not explain why ships, aircraft, and radio signals seem to reach farther than the strict geometric calculation predicts. The reason is atmospheric refraction. Air near Earth’s surface is denser than air at higher altitude. When a ray of light or a radio wave travels through air of changing density, it bends, just as light bends when it passes from water to glass. In a standard atmosphere, this bending curves radio and optical rays slightly downward, following the Earth’s curvature partway. The net effect is that both eyes and radio receivers effectively see farther than geometry alone would allow.

The Standard Atmosphere and the 4/3 Earth Radius Model

Engineers and scientists model this effect by using an “effective Earth radius” that is larger than the actual radius. Instead of computing line of sight against a sphere of radius R=6,371 km, you compute it against a sphere of radius k times R, where k is the effective Earth radius factor. For the NOAA/ITU-R standard atmosphere (temperature lapse rate of 6.5 degrees Kelvin per kilometer, sea level pressure 1013.25 hectopascals, as defined by NOAA’s National Weather Service), the standard k factor is 4/3, or approximately 1.333. This means that for most US radio planning, the effective Earth is about 8,495 kilometers in radius rather than 6,371 kilometers, and your calculated horizon distances grow accordingly. The ITU-R P.834-9 recommendation, which is the international standard used by the FCC and telecommunications engineers across the US, formally specifies k=4/3 for planning in temperate climates.

When Standard Atmosphere Does Not Apply

Two conditions in the US regularly produce k factors well outside the standard range. In the desert Southwest and at high altitude, the atmosphere can exhibit subrefraction, where the air is drier and less dense near the surface than expected. This reduces the bending effect and produces k factors around 0.75, meaning your effective LOS range is actually shorter than the geometric calculation. Conversely, along US coastal zones, particularly in California, the Gulf Coast, and the Pacific Northwest, temperature inversions create atmospheric ducting conditions. Warm air sitting on top of cold marine air bends radio waves downward so sharply that they can follow the Earth’s curvature for hundreds of kilometers beyond the standard horizon. The k factors during ducting events can reach 2.0 or higher. This calculator includes all four conditions: geometric (k=1), standard ITU-R (k=4/3), subrefraction (k=0.75), and superrefraction (k=2.0).

The Math

The Geometric Horizon, Refracted Line of Sight, and Fresnel Zone Explained

The core horizon formula is d = sqrt(2 times k times R times h), where d is the horizon distance in kilometers, k is the effective Earth radius factor, R is the Earth’s mean radius (6,371 km per NOAA/NGS WGS84), and h is the observer height in kilometers. For a 50-meter antenna (h = 0.05 km) with standard atmosphere (k = 4/3): d = sqrt(2 times 1.333 times 6371 times 0.05) = sqrt(848.9) = 29.1 km. This is the radio horizon of that antenna under standard atmospheric conditions. The visual (optical) horizon uses k=1 and gives a shorter result: 25.2 km.

Two-Point LOS: Adding Horizons

When two elevated points are trying to communicate or see each other, the maximum line-of-sight distance is the sum of their individual horizon distances. If Antenna A at 50 meters has a horizon of 29.1 km and Antenna B at 20 meters has a horizon of 18.4 km, the maximum LOS between them is 29.1 + 18.4 = 47.5 km under standard atmosphere. If the actual separation is 40 km, LOS exists with a 7.5 km margin. The Earth bulge at the midpoint of the path (20 km from each end) is computed as d1 times d2 divided by (2 times k times R), which gives 20 times 20 divided by (2 times 1.333 times 6371) = 400 divided by 16,988 = 0.0235 km = 23.5 meters. This is the amount the Earth’s surface rises above the straight LOS line at the midpoint of the path. Both antennas must be high enough that their combined horizons clear this bulge.

The Fresnel Zone and Why LOS Alone Is Not Enough for Radio

A line-of-sight path means the geometric ray from transmitter to receiver clears the Earth’s surface. But radio waves are not rays: they propagate as wavefronts that spread out from the transmitter in all directions. Even when the straight-line path is geometrically clear, radio energy traveling slightly off the straight path and reflecting or diffracting off the Earth’s surface can destructively interfere with the direct signal. The zone around the straight-line path that matters most is called the first Fresnel zone, which has a radius at any point along the path of sqrt(lambda times d1 times d2 divided by (d1 plus d2)), where lambda is the wavelength. For reliable radio communication, the FCC’s 47 CFR Part 101 (microwave licensing rules) requires at least 60 percent Fresnel zone clearance above any obstruction, including Earth’s curvature. This calculator computes the first Fresnel zone radius at the path midpoint for six common frequency bands, from VHF at 150 MHz to point-to-point microwave at 10 GHz.

Official Government Sources Referenced in This Calculator

  • ITU-R Recommendation P.834-9 (2017): Atmospheric refraction effects in radio propagation. Defines standard atmosphere k=4/3 effective Earth radius factor. Used by FCC and US telecommunications industry for radio path planning. itu.int/rec/R-REC-P.834
  • FCC 47 CFR Part 101.115: Frequency coordination for fixed microwave services. Specifies 60% first Fresnel zone clearance above obstructions as the standard for licensed microwave path calculations. fcc.gov
  • NOAA National Geodetic Survey: WGS84 mean Earth radius R = 6,371.0 km. Standard atmosphere definition (sea level: 1013.25 hPa, 15°C; lapse rate 6.5 K/km). geodesy.noaa.gov
  • US Army FM 6-02.40 (Visual Information Operations): Line-of-sight and Fresnel zone planning for Army tactical communications. 60% Fresnel zone standard for field radio path planning.
  • NOAA NWS: Standard atmospheric sounding data used to validate k-factor assumptions for US regions. Marine layer and temperature inversion documentation for superrefraction (k=2.0) conditions on US coasts. weather.gov
Reference Data

US Observer Height vs Horizon Distance Reference Chart for Field Planning

The table below shows precomputed horizon distances for common US observer and antenna heights using the standard ITU-R P.834 atmosphere (k=4/3). All figures use WGS84 R=6,371 km. For exact values at any height, use the calculator above. The formula is d = sqrt(2 times 1.333 times 6371 times h), with h in kilometers and d in kilometers.

HeightContextGeometric (k=1)Standard Atm (k=4/3)Marine Ducting (k=2)
1.7 mHuman eye level standing4.65 km / 2.89 mi5.37 km / 3.34 mi6.58 km / 4.09 mi
10 mShip bridge / small tower11.28 km / 7.01 mi13.02 km / 8.09 mi15.95 km / 9.91 mi
30 m3-story building rooftop19.53 km / 12.1 mi22.55 km / 14.0 mi27.61 km / 17.2 mi
50 mCell tower / 5-story building25.21 km / 15.7 mi29.10 km / 18.1 mi35.64 km / 22.1 mi
100 mFAA obstruction height (328 ft)35.65 km / 22.2 mi41.15 km / 25.6 mi50.40 km / 31.3 mi
305 mEmpire State Bldg antenna (1,000 ft)62.26 km / 38.7 mi71.92 km / 44.7 mi88.09 km / 54.7 mi
1,917 mMount Washington, NH (6,288 ft)156.0 km / 97.0 mi180.2 km / 112 mi220.7 km / 137 mi
4,205 mMauna Kea, HI (13,796 ft)231.1 km / 143 mi266.9 km / 165 mi326.8 km / 203 mi
6,194 mDenali, AK (20,310 ft)280.4 km / 174 mi323.7 km / 201 mi396.5 km / 246 mi
Atmosphere Conditionk FactorUS Where This OccursEffect on LOS Range
Geometric (no refraction)1.00Theoretical baseline / vacuum opticsMinimum range. Baseline for comparison.
Standard ITU-R P.8341.333 (4/3)Continental US temperate zones+15% over geometric. FCC/FCC planning standard.
Subrefraction0.75Desert SW, high-altitude Rocky MtnWorse than geometric in extreme cases.
Superrefraction / Ducting2.00+CA coast, Gulf of Mexico, Great Lakes+41% or more. Signals may propagate 2x standard range.
In the Field

Three Real American Scenarios: Mountain Lookout, HAM Radio Reach, and Cell Tower Planning

🏔 Mauna Kea Observatory, HI: Astronomy and Communications Horizon
Mode A: Horizon Distance
Observer height: 4,205 m (13,796 ft)
Model: Standard ITU-R P.834 (k=4/3)
Geometric horizon: 231.1 km
Standard atm horizon: 266.9 km
Marine ducting (k=2): 326.8 km

Why Mauna Kea Dominates Global Telescope Siting

At 4,205 meters above sea level, the Mauna Kea summit places an observer above roughly 40 percent of Earth’s atmosphere. From the standard ITU-R P.834 horizon calculation, an observer at the summit can geometrically see a standard-atmosphere radio horizon of 266.9 kilometers in any direction over the ocean, corresponding to about 165 nautical miles. USGS elevation data confirms the summit coordinates at 19.8228°N, 155.4682°W at 4,205 meters AMSL. The National Radio Astronomy Observatory cites Mauna Kea’s radio transparency and wide LOS horizon as key factors in its value for radio astronomy. During marine temperature inversion events common in Hawaiian coastal zones (k approaching 2.0), the effective radio horizon expands to over 326 kilometers, sometimes causing interference between commercial radio systems on the island chain that are nominally separated beyond geometric LOS range.

📡 HAM Radio Repeater Planning, Denver to Cheyenne, CO/WY
Mode B: LOS Check
Antenna A (Denver): 50 m height
Antenna B (Cheyenne): 30 m height
Path distance: 160 km
Model: Standard ITU-R (k=4/3)
d1=29.1 km, d2=22.5 km
Max LOS: 51.6 km
Status: BLOCKED (160 km >> 51.6 km)
Earth bulge midpoint: 750 m
Fresnel (VHF 150 MHz): 2,500 m

Why VHF HAM Radio Requires Repeater Networks

A HAM radio operator in Denver (5,280 ft elevation) with a 50-meter roof antenna wants to communicate directly with a station in Cheyenne, Wyoming (6,063 ft elevation) with a 30-meter tower. The 160-kilometer separation far exceeds the combined standard-atmosphere radio horizon of the two antennas (29.1 km plus 22.5 km equals 51.6 km total). Earth’s surface bulges 750 meters above the straight-line path at the midpoint. The first Fresnel zone radius at VHF (150 MHz) at the midpoint would be 2,500 meters, but there is no LOS at all. This is why the American Radio Relay League (ARRL) publishes repeater directories: HAM VHF and UHF signals require repeater sites on ridgelines or tall towers to bridge terrain-and-curvature gaps like Denver to Cheyenne. Using the Mode C calculator, the minimum effective antenna height for a direct path (assuming Cheyenne’s 30 meters) would be approximately 1,050 meters above average terrain, far exceeding practical tower heights.

⚓ USCG Sector San Francisco: Marine Radar Coverage
Mode B: LOS Check
Radar antenna height: 50 m
Target vessel bridge: 8 m
Path: 40.7 km (22.0 nm)
Model: Standard ITU-R (k=4/3)
d1=29.1 km, d2=11.6 km
Max radar LOS: 40.7 km
Status: MARGINAL (at design limit)
Earth bulge midpoint: 61 m
Fresnel (UHF): 73 m

Coast Guard Radar Horizon Matches the LOS Calculator

A US Coast Guard surface search radar operating from a 50-meter shore facility scanning for a vessel whose bridge is 8 meters above the waterline has a combined standard-atmosphere radio horizon of 40.7 kilometers (22.0 nautical miles). This matches real Coast Guard coverage planning documents, which typically cite approximately 20 nautical miles as the radar horizon for vessels of this bridge height from shore stations at comparable elevations. During marine temperature inversions common along the California coast (when k rises above 2.0), the same antenna pair can briefly achieve over 57 kilometers of radar range, explaining why Coast Guard operators occasionally track vessels well beyond their published nominal radar range. The FCC-standard 60 percent Fresnel zone clearance requires 73 meters of clearance above the Earth bulge at the path midpoint for UHF radar frequencies, and the combined antenna geometry barely meets this criterion at the 40.7 km design range.

Planning Guidance

Six Proven Methods to Extend Visual and Communications Reach Across American Terrain

01

Use the Standard ITU-R Model for Any Radio Planning, Not Geometric

The geometric (k=1) calculation is accurate for light in a vacuum. For any real-world radio link on Earth’s surface, use k=4/3 per ITU-R P.834-9. The difference is significant: a 50-meter antenna has a geometric horizon of 25.2 km but a standard-atmosphere radio horizon of 29.1 km. Using the geometric model for radio planning will cause you to place repeaters closer than needed, wasting infrastructure cost. The FCC’s own path analysis tools for microwave licensing use k=4/3 as the baseline.

02

Plan for 60% Fresnel Zone Clearance, Not Just Geometric LOS

A path that appears clear geometrically can still fail for radio if the first Fresnel zone intersects Earth’s surface. For a 40-kilometer microwave path at 10 GHz, the first Fresnel zone radius at the midpoint is about 173 meters. The FCC requires 0.6 times 173 = 104 meters of clearance above any obstruction, including Earth’s bulge. If you only check geometric LOS and ignore Fresnel zone clearance, a microwave link that looks good on paper can suffer a 10-15 dB signal loss from diffraction over the Earth’s edge.

03

Precompute LOS Before a SAR Operation for Faster Radio Coordination

Search and rescue teams operating in mountainous US terrain can use Mode B before a mission to identify which ridge positions provide radio LOS to base camp. Enter your portable radio antenna height (typically 1.5 to 3 meters) and the base camp antenna height, then vary the path distance to find your maximum communication radius without a repeater. Cross-reference this with your triangulation calculator results to identify ridgelines within your LOS range where you can establish communications relay positions. ARRL field emergency coordinators recommend this pre-mission LOS check as standard practice for HAM operators supporting FEMA or state emergency management operations.

04

Know When Marine Ducting Can Extend Your Range Along US Coasts

Temperature inversions along California, Gulf of Mexico, and Pacific Northwest coastal zones regularly produce atmospheric ducting conditions where k exceeds 2.0. In these conditions, radio signals (especially at VHF and above) can propagate hundreds of kilometers beyond the standard horizon. If you are planning a coastal radio link and need more range than standard atmosphere predicts, select k=2.0 (superrefraction) in this calculator to see the potential extended range. Note that ducting is intermittent and weather-dependent: you should not rely on it for a permanent link, but it explains why HAM operators in California regularly work stations in Hawaii on 2-meter VHF under favorable ducting conditions.

05

Use USGS Elevation Data to Confirm True Observer and Target Heights

The accuracy of every LOS calculation depends on knowing the true height of both your observer and your target above mean sea level or above local terrain. The USGS National Elevation Dataset (NED), accessible through the USGS National Map at nationalmap.gov, provides one-meter resolution elevation data covering the continental US, Alaska, and Hawaii. For cell tower or point-to-point microwave planning, always confirm your site elevation and the target site elevation from USGS NED before running Mode B or Mode C. A 10-meter error in elevation entry at a 50-kilometer path can shift your LOS status from clear to marginal.

06

Chain Your Navigation Hub Tools for Complete Field Planning

This LOS calculator works best as part of the full Navigation Hub toolkit. Before attempting resection with the Triangulation Calculator, use Mode A here to verify that your chosen landmarks are geometrically visible from your approximate elevation. If the landmark is within your horizon distance, LOS almost certainly exists (assuming no terrain obstruction between you and the landmark). Use the Magnetic Declination Calculator to correct your compass bearings for the WMM2025 declination at your location, then use the Pacing Calculator to estimate your distance from terrain features when a target distance input is needed for Mode B or Mode C.

Quick Reference

Quick Reference: Distance Tables, Earth Bulge Values, and Atmosphere K-Factors

ParameterFormula / ValueNotes
Horizon distanced = sqrt(2kRh)d in km, R=6371 km, h in km, k=atm factor
Standard k-factork = 4/3 = 1.333ITU-R P.834-9, NOAA standard atmosphere
Earth bulge at midpointB = D^2 / (8kR)D in km, B in km; convert to m for antenna planning
Fresnel zone at midpointF1 = 0.5 sqrt(lambda D)lambda and D in same units; result in same unit
Required Fresnel clearance0.6 times F1FCC 47 CFR Part 101 / ITU-R standard minimum
Human eye level horizon4.7 km / 2.9 mi (k=1) | 5.4 km / 3.4 mi (k=4/3)At 1.7 m observer height
100m antenna horizon35.7 km (k=1) | 41.2 km (k=4/3)Standard FAA obstruction threshold height
Subrefraction (k=0.75)86% of geometric horizonDry desert SW, Rocky Mountain high altitude
Ducting / superrefractionUp to 141% of geometricUS coastal marine inversions; k=2.0+
VHF Fresnel (150 MHz, 40 km path)F1 at midpoint: 2,236 m60% clearance needed: 1,342 m above bulge
Microwave Fresnel (10 GHz, 40 km path)F1 at midpoint: 173 m60% clearance: 104 m above bulge
Common Questions

Frequently Asked Questions About Curvature Math, Atmospheric Refraction, and Fresnel Zones

The geometric horizon is the farthest distance at which you can see something at the same elevation as yourself, considering only Earth’s curvature and no atmospheric bending. It is calculated as d = sqrt(2 times R times h), where R is the Earth’s mean radius (6,371 km per NOAA/NGS WGS84) and h is your height above the surface. For a person standing on flat ground at eye level (1.7 m), the geometric horizon is about 4.65 kilometers. This is the minimum possible horizon: in the real atmosphere, refraction always extends it somewhat beyond this geometric value.
Radio waves and light both travel in straight lines in a uniform medium, but the atmosphere bends them. Near Earth’s surface, air pressure and temperature decrease with altitude, making the lower atmosphere denser than air higher up. Radio waves traveling through this density gradient bend slightly downward, curving toward the surface. The amount of bending under standard atmosphere (defined by NOAA’s National Weather Service as 1013.25 hPa, 15°C at sea level, lapse rate 6.5 K/km) corresponds to an effective Earth radius about 4/3 times the actual radius. This means standard-atmosphere radio horizons are about 15 percent farther than the geometric optical horizon.
The k-factor is a mathematical shortcut. Instead of computing how radio waves curve through an atmosphere with gradually decreasing density, engineers replace the real Earth of radius R with a larger imaginary Earth of radius k times R and assume rays travel in straight lines on this enlarged sphere. For the standard atmosphere (ITU-R P.834-9), k equals 4/3 (approximately 1.333). This makes the effective Earth radius about 8,495 km instead of 6,371 km, and straightforward horizon formulas give results that match real-world radio propagation without needing to model the atmospheric refraction mathematically. The FCC uses this k=4/3 model for all US domestic microwave and fixed-service frequency coordination under 47 CFR Part 101.
The Earth bulge is how much the Earth’s surface rises above the straight line connecting two elevated points. At the midpoint of a 40-kilometer path, the Earth’s surface is about 31 meters above the straight LOS line (using k=4/3). If you have a 50-meter antenna and a 30-meter antenna separated by 40 km, the midpoint of the LOS line is only 40 meters above the ground. After subtracting the 31-meter bulge, only 9 meters of clearance remain. This matters because radio planning requires at least 60 percent of the first Fresnel zone to be clear of the surface. The Fresnel zone at the midpoint of a 40 km VHF path is about 2,236 meters in radius, so 60 percent clearance means 1,342 meters above the bulge, far more than 9 meters. LOS exists geometrically but radio performance would be severely degraded by diffraction over the Earth’s edge.
The first Fresnel zone is an ellipsoid surrounding the direct line between transmitter and receiver. Radio energy that travels paths within this ellipsoid adds constructively at the receiver. Energy that travels paths outside this ellipsoid either adds or subtracts depending on path length. For reliable communication, the FCC (in 47 CFR Part 101) and the ITU-R standards require that at least 60 percent of the first Fresnel zone radius be clear of any obstruction at every point along the path. This is more restrictive than simple geometric line of sight, because even a technically unobstructed path can suffer significant signal loss if the Fresnel zone grazes the Earth’s surface or a ridgeline. The 60 percent threshold corresponds to losing about 6 dB of signal strength compared to a fully clear path.
From the summit of Mount Washington, New Hampshire (1,917 m, 6,288 ft), the standard-atmosphere visual horizon is approximately 180 km (112 miles). From Mount Whitney, California (4,421 m, 14,505 ft), it is about 243 km (151 miles). From Denali, Alaska (6,194 m, 20,310 ft), it reaches approximately 324 km (201 miles). These are the distances to your geometric visual horizon over a flat ocean surface. In mountainous terrain, actual visibility depends on the heights of terrain features between you and the horizon, which is why terrain-aware path planners (which account for ridgelines and valleys) are more accurate than pure curvature math for mountainous areas of the US.
The US Coast Guard (USCG) uses LOS calculations extensively for surface search radar coverage planning, VHF-FM communication coverage (Channel 16 distress frequency), and Rescue 21 antenna siting. USCG radar antennas at coastal stations are positioned at heights that optimize radar horizon for vessel detection. For a 50-meter shore radar station, the standard-atmosphere radar horizon to a vessel with an 8-meter bridge (a typical mid-size coastal vessel) is about 40.7 km (22 nautical miles). USCG Rescue 21 (the nationwide maritime distress monitoring system) uses Mode B-style two-point LOS calculations for every antenna site to ensure complete coverage of each sector with appropriate overlap.
Atmospheric ducting occurs when a temperature inversion creates a layer of warmer air above cooler air near the surface. Radio waves entering this duct refract downward and can be trapped, following Earth’s curvature for hundreds of kilometers beyond the normal horizon. In the US, ducting is most common: along the California coast in summer and fall (Pacific marine layer), in the Gulf of Mexico where warm, humid air flows over cooler ocean water, over the Great Lakes in spring and fall, and in the desert Southwest during specific meteorological conditions. HAM radio operators on 2-meter VHF (144 MHz band) regularly exploit ducting to work contacts from California to Hawaii (around 3,900 km), a distance that would require k values of 50 or more. NOAA’s Weather Research and Forecasting model now includes ducting predictions that amateur and commercial radio operators can access for planning purposes.
Use Mode C in this calculator. Enter a 100 km distance and the target antenna height. For a target at 20 meters (66 ft), the target’s radio horizon under standard atmosphere (k=4/3) is 18.4 km. You need your own horizon to cover the remaining 100 minus 18.4 = 81.6 km. Using h = d^2 / (2kR): h = (81.6)^2 / (2 times 1.333 times 6371) = 6,658 / 16,988 = 0.392 km = 392 meters. So you need an antenna approximately 392 meters above the terrain for a direct, no-repeater path to a 20-meter-high target at 100 km. This is why long-distance VHF radio in flat terrain almost always requires repeater networks or aircraft/satellite relay rather than direct ground-to-ground links.
At cruising altitude (approximately 10,668 meters or 35,000 feet for commercial jets in the US), the geometric horizon is sqrt(2 times 6371 times 10.668) = sqrt(136,000) = 369 km. With standard atmosphere refraction (k=4/3), this extends to about 426 km. At these altitudes, however, the k factor is actually closer to 1.0 because refraction effects are smaller at high altitude (the atmosphere above the aircraft is thin, so the density gradient is smaller). Using k=1 (geometric): 369 km per horizon. In practice, from a typical window seat, passengers can see features of the Earth’s surface between 370 and 470 km away under clear conditions, which explains why US passengers on cross-country flights can occasionally see both the Rocky Mountains and the Great Plains simultaneously during clear conditions over Colorado or Wyoming.
In arid, high-altitude terrain like the Colorado Plateau, Mojave Desert, and Great Basin, the atmosphere near the surface can be drier and less dense than expected at standard lapse rates. This produces subrefraction (k values around 0.75), where radio waves actually bend slightly upward rather than following the Earth’s curvature. The practical effect is a horizon that can be shorter than even the geometric calculation predicts. For a 50-meter antenna, the subrefraction horizon (k=0.75) is only 24.4 km, compared to 29.1 km under standard atmosphere and 25.2 km geometric. Engineers planning microwave links across desert terrain in Nevada, Utah, or Arizona should calculate for subrefraction conditions in their worst-case path analysis, particularly for paths over high desert plateaus at elevations above 1,500 meters.
The FCC’s Part 101 rules (47 CFR 101.115) for fixed microwave services specify that path clearance should be calculated at the median refractivity gradient (k=4/3) and that the path must maintain at least 0.3 times the first Fresnel zone (30%) clearance above all obstructions for lightly protected paths, and 0.6 times the first Fresnel zone (60% clearance) for fully protected paths. Most licensed microwave operators in the US target 60% first Fresnel zone clearance as their design standard. In practice, FCC microwave path analysis tools use k=4/3 for the nominal path and also check k=2/3 (subrefraction) for worst-case analysis. This calculator uses the industry-standard 60% first Fresnel zone criterion for the “marginal” status boundary in Mode B.
Cell tower engineers in the US use LOS and Fresnel zone calculations as part of radio frequency (RF) path planning for backhaul links between towers. Each cell tower must transmit its data to the mobile network core via a backhaul link, either through fiber, licensed microwave, or millimeter wave. Microwave backhaul links (typically 6 to 23 GHz in the US) must maintain clear LOS with adequate Fresnel zone clearance over every point of the path. Engineers use tools like this calculator to determine if a proposed tower location has line of sight to the nearest hub site, and to specify the required antenna height at each end to achieve the required clearance. The FCC’s Wireless Bureau processes thousands of Part 101 microwave license applications per year, each requiring this type of path calculation as part of the application.
The NOAA standard atmosphere used in this calculator is defined by the International Standard Atmosphere (ISA), which NOAA’s National Weather Service adopts as the reference model. Its key parameters at sea level are: pressure 1013.25 hPa, temperature 15°C (288.15 K), density 1.225 kg/m3, and temperature lapse rate 6.5 K/km. Above the tropopause (11 km), temperature is constant at -56.5°C. This atmosphere produces the effective Earth radius factor k=4/3 that ITU-R P.834-9 specifies for standard radio propagation planning. NOAA provides real-time and forecast atmospheric profiles through its Radiosonde Observation (RAOB) program, with twice-daily balloon soundings at over 90 US stations, allowing engineers to determine when local conditions depart from the standard atmosphere model.
This calculator handles Earth curvature but assumes flat terrain between observer and target. In the real world, ridgelines, mountains, and buildings between the two points can block LOS even when the Earth curvature calculation says the path is clear. For terrain-aware LOS analysis, engineers use digital elevation model (DEM) tools that overlay a terrain profile from USGS National Elevation Dataset data along the path. The USGS National Map provides free DEM data at one-meter resolution for the continental US. This calculator is most accurate for over-water paths (like the Coast Guard marine radar example), open plains, or paths where you have separately confirmed there are no terrain obstructions between the two points.
Several official sources allow independent verification. The FCC’s Universal Licensing System (ULS) path analysis tool at fcc.gov/licensing-databases/uls uses k=4/3 and the 60% Fresnel zone standard, consistent with this calculator. NOAA’s online RF Tools section provides basic propagation models. The ARRL Antenna Book (published by the American Radio Relay League, the largest US amateur radio organization) includes tables of VHF and UHF radio horizon distances that match the k=4/3 formula used here. For geometry-only verification, the NOAA/NGS interactive geodesy tools at geodesy.noaa.gov can be used to compute Earth curvature values for any two locations. Results from this calculator match all three reference sources within rounding error.