Mollweide’s Projection

The Mollweide projection is an equal-area projection that represents the world in an elliptical shape. This means that areas on the map are proportional to their corresponding areas on the globe. This makes it particularly useful for displaying global data, such as population density, climate zones, or land use, where the preservation of area is essential.

The Mollweide projection with Tissot's indicatrix of deformation
The Mollweide projection with Tissot’s indicatrix of deformation. Source

Mollweide’s projection is often used in world maps to balance the distortion of shapes and sizes, providing an accurate visual comparison of different regions.

Key Features

  • Parallels of Latitude: The parallels are unequally spaced straight lines, but they are parallel to each other and the equator.
  • Meridians of Longitude: The central meridian is a straight line, while all other meridians are equally spaced elliptical arcs that converge at the poles.
  • Equal-Area Property: The projection is pseudocylindrical and equal-area, meaning it preserves the relative size of landmasses.
  • Scale and Distortion: The scale is true only along the 40°44′ N and S parallels. Distortion is most severe near the outer edges and at high latitudes.
  • Usage: It’s primarily used for global maps that display data distributions.
Mollweide Projection – Step-by-Step Construction

Mollweide Projection

Step-by-Step Construction of the World Graticule
Scale 1 : 250,000,000  |  Interval 30°

Mollweide’s projection is an equal-area world map projection in which the entire Earth is represented inside an ellipse.

The equator forms the long horizontal axis, the central meridian forms the vertical axis, the parallels are straight horizontal lines, and the remaining meridians are smooth curves joining the two poles.

Step 1 – Calculate the Reduced Radius of the Earth

Take the mean radius of the Earth as approximately:

R = 6371 km

The given representative fraction is:

1 : 250,000,000

First convert the Earth’s radius into centimetres:

6371 km = 637,100,000 cm

Now divide by the scale denominator:

Rm = 637,100,000 ÷ 250,000,000
Rm ≈ 2.5484 cm

Therefore, the reduced radius used for the construction is approximately 2.5484 cm.

Step 2 – Calculate the Dimensions of the Ellipse

In Mollweide’s projection, the world is enclosed by an ellipse whose major axis is twice the minor axis.

Major Axis

Major Axis = 4√2 Rm
= 4 × 1.4142 × 2.5484
≈ 14.42 cm

Minor Axis

Minor Axis = 2√2 Rm
= 2 × 1.4142 × 2.5484
≈ 7.21 cm
Required dimensions of the projection:
Major axis = 14.42 cm
Minor axis = 7.21 cm

Step 3 – Draw the Main Axes

Draw a horizontal line AB = 14.42 cm. This line represents the equator.

Mark the midpoint of AB as O.

Through O, draw a perpendicular vertical line PN = 7.21 cm.

Since O is the midpoint:

OP = ON = 7.21 ÷ 2
OP = ON ≈ 3.604 cm

Point P represents the North Pole and point N represents the South Pole.

A B P N O Equator Central Meridian 14.42 cm

Step 4 – Draw the Outer Ellipse

Draw a smooth ellipse passing through the four points A, P, B and N.

The ellipse forms the outer boundary of the complete world map.

A B P N 180°W 180°E 90°N 90°S

Step 5 – Calculate the Positions of the Parallels

The parallels in Mollweide’s projection are straight horizontal lines, but they are not equally spaced.

For each latitude φ, first calculate the auxiliary angle θ from:

2θ + sin(2θ) = π sin φ

After obtaining θ, calculate the vertical distance from the equator:

y = √2 Rm sin θ

Example: Position of 30° N

For:

φ = 30°

Solving the auxiliary equation gives approximately:

θ ≈ 0.4159 radians

Therefore:

y = √2 × 2.5484 × sin(0.4159)
y ≈ 1.456 cm

Measure 1.456 cm upward from O along the central meridian to locate 30° N.

Measure the same distance downward from O to locate 30° S.

Parallel Distances from the Equator

Latitude Distance from Equator
90° N +3.604 cm
60° N +2.748 cm
30° N +1.456 cm
0 cm
30° S −1.456 cm
60° S −2.748 cm
90° S −3.604 cm

Mark these distances on the central meridian.

Through the marked points, draw horizontal lines across the ellipse, stopping each line where it meets the boundary.

60°N 30°N 30°S 60°S 90°N 90°S

Step 6 – Calculate the Positions of the Meridians

Draw meridians at intervals of 30°:

0°, 30°, 60°, 90°, 120°, 150° and 180°

The central meridian, 0°, is represented by the straight vertical line PN.

All the remaining meridians are curved.

Their horizontal position on each parallel is calculated from:

x = (2√2 / π) Rm (λ − λ0) cos θ

where:

λ = longitude being plotted
λ0 = central longitude
θ = auxiliary angle corresponding to the latitude

When using the formula, longitude is expressed in radians.

Example: 60° E at 30° N

At 30° N:

θ ≈ 0.4159

Convert 60° to radians:

60° = π / 3 radians

Therefore:

x = (2√2 / π) × 2.5484 × (π / 3) × cos(0.4159)
x ≈ 2.198 cm

On the 30° N parallel, measure approximately 2.198 cm to the right of the central meridian to locate 60° E.

Measure the same distance to the left to locate 60° W.

Step 7 – Plot the Longitude Points on Each Parallel

The distance between meridians decreases progressively from the equator towards the poles.

Longitude Positions on the Equator

Longitude Distance from Central Meridian
30° 1.201 cm
60° 2.403 cm
90° 3.604 cm
120° 4.805 cm
150° 6.007 cm
180° 7.208 cm

Longitude Positions on 30° N and 30° S

Longitude Distance from Central Meridian
30° 1.099 cm
60° 2.198 cm
90° 3.297 cm
120° 4.396 cm
150° 5.495 cm
180° 6.594 cm

Longitude Positions on 60° N and 60° S

Longitude Distance from Central Meridian
30° 0.777 cm
60° 1.555 cm
90° 2.332 cm
120° 3.109 cm
150° 3.887 cm
180° 4.664 cm

Plot all longitude positions symmetrically on both sides of the central meridian.

Step 8 – Join the Meridian Points with Smooth Curves

After all longitude points have been marked, join the points belonging to the same longitude.

For example, join all the points representing 60° E from the North Pole to the South Pole.

Repeat the same procedure for:

30°, 60°, 90°, 120° and 150°

Construct corresponding curves on the western side of the central meridian.

All meridians converge at the North and South Poles. The 180° meridian coincides with the outer elliptical boundary.

60°N 30°N 30°S 60°S 90°N 90°S 180°W 150°W 120°W 90°W 60°W 30°W 30°E 60°E 90°E 120°E 150°E 180°E

Step 9 – Label and Finish the Projection

After the complete graticule has been drawn, finish the construction neatly.

  1. Darken the outer elliptical boundary.
  2. Keep the equator slightly more prominent than the other parallels.
  3. Keep the central meridian slightly more prominent than the other meridians.
  4. Label the parallels as 90° N, 60° N, 30° N, 0°, 30° S, 60° S and 90° S.
  5. Label the eastern and western meridians at 30° intervals.
  6. Write the title: Mollweide’s Equal-Area Projection.
  7. Mention the scale: 1 : 250,000,000.

Construction Sequence at a Glance

  1. Calculate the reduced radius of the Earth.
  2. Calculate the major and minor axes of the ellipse.
  3. Draw the equator and central meridian.
  4. Construct the outer ellipse.
  5. Calculate the positions of 30° N, 60° N, 30° S and 60° S.
  6. Draw the parallels as straight horizontal lines.
  7. Calculate longitude positions on each parallel.
  8. Plot longitude points symmetrically east and west of the central meridian.
  9. Join corresponding longitude points with smooth meridian curves.
  10. Label the projection and complete the final graticule.
mollweide's projection

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