Queendom Tools

Lambert Conformal Conic Projection Calculator

This calculator applies the Lambert conformal conic projection with two standard parallels in the forward direction: it takes the latitude and longitude of a point and returns the projected coordinates x and y together with the point scale factor k. It works on an ellipsoid or on a sphere and follows J. P. Snyder, Map Projections - A Working Manual, USGS Professional Paper 1395, 1987, equations 15-1 to 15-10.

It is meant for surveyors, GIS analysts and cartographers who already hold a projection definition: the semi-major axis a, the eccentricity squared e², the two standard parallels, and the origin latitude and longitude. Every intermediate quantity (m1, m2, t1, t2, t0, n, F, ρ0, t, ρ and θ) is shown, and the formulas are written out with the values you typed. The fields start with the ellipsoid example from Snyder, pages 296-297.

Forward calculation

Ellipsoid or sphere
Projection definition
Point

Projected point

x (unit of a)
—
y (unit of a)
—
Point scale factor k (dimensionless)
—

Intermediate values

QuantityValueUnit
m1, at φ1—dimensionless
m2, at φ2—dimensionless
t1, at φ1—dimensionless
t2, at φ2—dimensionless
t0, at φ0—dimensionless
n—dimensionless
F—dimensionless
ρ0—unit of a
t, at φ—dimensionless
ρ—unit of a
θ—degrees

Formulas with your values

  1. —

All values are carried in double precision with no rounding inside the calculation; only the displayed results are rounded to 7 decimals.

How to use the calculator

  1. Enter the semi-major axis a in any length unit (above 0) and the eccentricity squared e² (0 or more and below 1). For a sphere, enter e² = 0; a is then its radius.
  2. Enter the two standard parallels φ1 and φ2 in degrees. Each must be from 0 to 89 degrees, and φ1 must not equal φ2.
  3. Enter the origin latitude φ0 (0 to 89 degrees) and the origin longitude λ0 (−180 to 180 degrees, west negative).
  4. Enter the point latitude φ (0 to 89 degrees) and the point longitude λ (−180 to 180 degrees, west negative). The difference λ − λ0 must be from −180 to 180 degrees; it is not wrapped.
  5. Results update as you type; the Calculate button runs the same calculation. Read x, y and k, then check the intermediate values and the formulas written out with your values. A field that is empty or out of range is named in a message below it, and the results show dashes.

Method

Snyder, equations 15-1 to 15-10, forward direction, with degrees converted to radians as π/180:

Frequently asked questions

Why does the calculator ask for e² and not for e?

The eccentricity squared e² is the only ellipsoid input, and e is computed from it as the square root of e². Entering a rounded e instead can shift ρ by 0.07 m.

How do I compute on a sphere instead of an ellipsoid?

Enter 0 for the eccentricity squared e². The semi-major axis a is then the radius of the sphere. With a = 1 and the angles of Snyder's example, the calculator gives n = 0.6304777, x = 0.2966785 and y = 0.2462112.

What units are x, y and k in?

x, y, ρ0 and ρ are in the length unit you used for the semi-major axis a. The point scale factor k is dimensionless and equals 1 on both standard parallels. θ is shown in degrees.

Does the calculator convert GPS or WGS84 coordinates?

No. It is a calculation aid for the projection as defined and performs no datum transformation. A GPS latitude is not converted to the ellipsoid you enter.

Note

This page is a calculation aid for the Lambert conformal conic projection as defined by the values you enter. It performs no datum transformation: a GPS latitude is not converted to the ellipsoid entered. Source: J. P. Snyder, Map Projections - A Working Manual, USGS Professional Paper 1395, 1987.