Nautical Distance Calculator (Rhumb & Great-Circle)

Calculate sea distance between two ports by rhumb-line and great-circle methods

Compute rhumb-line and great-circle distance in nautical miles between two latitude/longitude positions, with the initial great-circle course and the mileage saved versus the constant-heading rhumb line. Navigators and voyage planners use it for passage planning. It runs free in your browser on Gera Tools, with nothing uploaded.

Last updated Source: Gera Tools

What is the difference between rhumb line and great circle?

A great circle is the shortest path across the curved earth but requires a constantly changing heading. A rhumb line holds a single constant compass course, which is simpler to steer but longer. The gap grows on long, high-latitude, east-west passages.

For passage planning you need two numbers: the great-circle distance, which is the shortest path across the curved earth, and the rhumb-line distance, which holds a single constant compass heading. This calculator returns both in nautical miles from two lat/long positions, plus the initial course and the miles you save by sailing the great circle.

When each method matters

The choice between great-circle and rhumb-line routing is not purely academic — it affects fuel costs, voyage time, and crew scheduling on long ocean passages.

On short coastal passages (under a few hundred miles) the difference is negligible. A voyage down the U.S. East Coast or across the English Channel gains almost nothing from a great-circle track; a simple rhumb-line course is easier to plot and steer.

On long, high-latitude, east-west passages the gap becomes significant. Crossing the North Pacific or the North Atlantic, a great-circle track arcs deep into higher latitudes and can save hundreds of nautical miles compared with the constant-heading rhumb line. A transatlantic crossing from Southampton to New York (roughly 3,000 nm) can see a meaningful saving. The downside is that the heading changes continuously; modern autopilots handle this, but paper-chart navigation requires waypoints at regular intervals to approximate the arc.

How it works

The great-circle distance uses the haversine formula to find the central angle between the two points, then scales by the earth’s radius:

a = sin²(Δφ/2) + cos φ1 · cos φ2 · sin²(Δλ/2)
central angle = 2 · atan2(√a, √(1−a))
distance (nm) = central angle · 3440.065

The rhumb line uses the Mercator inverse, where the constant course holds against a straightened-out longitude scale:

Δψ = ln( tan(π/4 + φ2/2) / tan(π/4 + φ1/2) )
q   = Δφ / Δψ   (or cos φ1 near east-west tracks)
rhumb distance (nm) = √(Δφ² + q²·Δλ²) · 3440.065

Here φ is latitude in radians, λ is longitude, and 3440.065 is the earth’s radius expressed in nautical miles.

Entering positions

Coordinates are entered as decimal degrees, with south latitudes and west longitudes as negative values. For example, the position 51° 30’ N, 000° 07’ W (roughly London) becomes latitude 51.5, longitude -0.117. The tool accepts decimal fractions directly, so convert degrees-minutes-seconds before entering (degrees + minutes/60 + seconds/3600).

Example and tips

From the English Channel to New York the great circle bows north toward Newfoundland and can save dozens of miles over the flat rhumb line, but it demands continual course changes. On a short hop down a coastline the two distances differ by a fraction of a mile, so steering a single rhumb-line heading is simpler with no real penalty.

The initial great-circle course output is the compass heading at departure; it changes continuously along the route. On a west-to-east North Atlantic crossing the initial course typically points well north of the destination, which surprises navigators who expect to head straight for the port. This is the nature of geodesic geometry on a sphere.

Remember both figures are open-water geodesics — real routing must clear land, traffic separation schemes, and weather. This tool gives the geometric distance; voyage planning software with chart overlays handles the navigational constraints.