Notes on Mercator’s Projection

The following work is my math essay assignment (an essay on any topic related to the Math 30 curriculum). I found it interesting enough that I’ll post it here on my math blog. Yay.


How do you make a world map? We find world maps everywhere — but the making of world maps is more complicated than most people realize. The earth is round, and a map is flat. How should one represent the surface of the earth, a sphere, on a flat sheet of paper?

The problem of displaying the surface of a sphere on a map has concerned cartographers, or map makers, for centuries. Over the years, cartographers have come up with a multitude of map projections, or systematic methods of transferring the surface of the earth onto flat paper.

There are many types of map projections, but one of the most common types is the cylindrical projection. Imagine a semi-transparent, hollow globe with a light inside of it. Now wrap a piece of blank map paper around it, like a cylinder:

Let the earth be represented as a unit sphere. The longitude (east-west location) shall be denoted as \lambda, and the latitude (north-south location) as \theta. A is the center of the earth, and B a point on the equator.

Now a light source is placed at point A; a point D on the surface of the globe will be projected in a straight line to point C on the cylinder such that points A, D, and C are collinear. Using some trigonometry, we have \tan \theta = \frac{BC}{AB}; since AB=1, the length of BC is \tan \theta.

After repeating this procedure for every point on the sphere, the cylinder is unrolled into a flat sheet. The result is the following map:

Here, if a point on the earth is known (we know its latitude and longitude), we know its position on the map. The position coordinates of the map, (x,y) can be described in terms of \lambda and \theta in the following equations:

x = \lambda

y = \tan \theta

This projection has several major drawbacks: most notably, as the latitude \theta increases toward 90^\circ, the slope of \tan(\theta) becomes increasingly steep, and the y-coordinates of the point of the map increases towards infinity. At high latitudes, the map is very distorted.

The map is not equal-area — in an equal-area map, shapes of equal area on the sphere have equal area on the projection. Looking at the map we created, this is clearly not the case. Neither is the map conformal, or shape preserving. In a conformal map, the angle between any two lines must be the same as their counterparts on the map.

Mercator’s Projection

One of the most well known cylindrical map projections is Mercator’s projection. Invented by Belgian cartographer Gerardus Mercator in 1569, Mercator addresses some of the problems in older cylindrical projections. Unlike our projection, Mercator’s projection is conformal, and it has been used for navigation for centuries:

However, the equations for Mercator’s projection are rather complicated. The position on Mercator’s projection, when given the latitude and longitude, is:

x = \lambda

y = \ln ( \sec \theta + \tan \theta )

This is a strange and seemingly random formula. But when we use this formula, we get a conformal map. How does this work?

Deriving Mercator’s Projection

Before deriving the formula for Mercator’s Projection, we take a step back and ask ourselves — what was the projection for in the first place?

Unlike most maps today which are used to decorate walls, Mercator’s map was more than that — it was used for nautical navigation. Suppose you were to travel by ship from Vancouver to Honolulu, equipped with nothing more than a compass. Which direction should you travel?

Now if you have a copy of Mercator’s map, this becomes simple. You draw a straight line from Vancouver to Honolulu, and with a protractor you find that the direction is 40^\circ south to the parallel. With a compass, it would be easy for you to maintain this constant heading for the entire duration of the trip.

(Footnote — The straight line on Mercator’s map is not straight on the Earth — it is actually a curved line, called a rhumb line. That is, after taking an initial bearing, one proceeds along the same bearing (relative to the north pole) for the duration of the trip. In the example, you would have to adjust your heading intermittently so that you are always heading at the direction 40^\circ south to the parallel.)

This technique is possible because it relies on one crucial property of Mercator’s map: that it is conformal. It would fail if we tried the same technique on the cylindrical projection given in the introduction.

However, notice that on Mercator’s map, all parallels have the same length: a parallel is simply a line across the width of the entire map. But on Earth, a sphere, parallels are longer when they are closer to the equator and shorter when near the poles:

Let the Earth be a unit sphere with center A. D is a point on the surface of the Earth and B is its corresponding point on the equator. Let C be a point such that CD is parallel to AB and AC is perpendicular to AB. As AB = 1, the circumference of the Earth at the equator is 2 \pi. But the circumference at latitude \theta is only 2\pi \cos \theta.

It is easy to see why: as AB || CD in the diagram, it follows that angles \angle DAB and \angle ADC are equal. Next, \cos \angle ADC = \frac{CD}{AD} = \frac{CD}{1} = CD, therefore CD = \cos \theta. The result follows.

On the map, the length of the equator and the parallel at latitude \theta are equal. But on Earth, the parallel at latitude \theta is smaller than the equator by a factor of \cos \theta; in the projection any line at latitude \theta ends up being stretched horizontally by a factor of \frac{1}{\cos \theta} or \sec \theta.

Finally, in order to satisfy the property of conformality, any part of the map stretched horizontally by some factor, say k, must be stretched vertically by the same factor k. Doing so preserves the angles of that part of the map:

Imagine a very small piece of land at latitude \theta. When it is represented on the map, it is stretched horizontally by \sec \theta. Hence to preserve conformity, it must also be stretched vertically by \sec \theta.

But this can only work if the piece of land has no area. But as all pieces of land, no matter how small, has some area, the latitude of the piece of land is not \theta, but goes from \theta to \theta + \Delta \theta for some small number \Delta \theta. Similarly, the space this piece of land occupies on the map is not just y, but goes from y + \Delta y for some small number \Delta y. Now as \Delta \theta approaches 0, the ratio of \Delta y to \Delta \theta approaches \sec \theta:

\lim_{\Delta \theta \to 0} \frac{\Delta y}{\Delta \theta} = \sec \theta

Or equivalently,

\frac{dy}{d \theta} = \sec \theta

Solving for dy and integrating both sides gives:

\begin{array}{rl}y & = \int \sec \theta \, d \theta \\ & = \int \left( \sec \theta \cdot \frac{\sec \theta + \tan \theta}{\sec \theta + \tan \theta} \right) d \theta \\ & = \int \frac{\sec^2 \theta + \sec \theta \tan \theta}{\sec \theta + \tan \theta} \, d \theta\end{array}

If we let u be the denominator, u = \sec \theta + \tan \theta, it turns out that the numerator is the derivative of u, or du = \sec^2 \theta + \sec \theta \tan \theta. Thus we can substitute u into the integral:

\begin{array}{rl} y & = \int \frac{du}{u} \\ & = \ln |u| + C \\ & = \ln | \sec \theta + \tan \theta | + C \end{array}

We defined the map so that the equator lies on the x-axis, therefore when \theta = 0, y=0. Substituting and solving for C, we find that C=0. Also, since \sec \theta + \tan \theta > 0 for -\frac{\pi}{2} < \theta < \frac{\pi}{2}, we can remove the absolute value brackets. Therefore,

y = \ln ( \sec \theta + \tan \theta )

This is what is desired.

An Alternative Map Projection

Mercator’s Projection is merely a conformal map, not a perfect map. It has several drawbacks — the scale varies greatly from place to place: as the latitude increases, the map gets stretched more and more. This severely distorts larger figures, especially areas near the poles. At a latitude greater than about 70^\circ, the map is practically unusable.

The Gall-Peters Projection is an alternative cylindrical projection:

When a map is used in navigation, it is important that angles are preserved in the map. But when a map is used to present statistical data, it’s often more important to preserve areas in the map: otherwise one may be deceived into thinking one country is bigger than another when they are actually the same size.

The Gall-Peters projection does this, trading conformity for equal-area — two countries of the same area will have the same area on the map, no matter where they are on the map. This map projection is produced by the following equations:

x = \lambda \cos 45^\circ = \frac{\lambda}{\sqrt{2}}

y = \frac{\sin \theta}{\cos 45^\circ} = \sqrt{2} \sin \theta

A discussion on why this set of equations produces an equal-area map is beyond the scope of this essay.


It is a tricky matter to accurately depict the surface of the earth on a flat sheet of paper. The method of cylindrical projection produces several considerably different maps.

The first map we considered uses only simple trigonometry, but the map produced is not very useful. The second map we investigate, Mercator’s Projection, preserves angles on the map. The last map we consider, the Gall-Peters projection, preserves areas on the map.

Each of these map projections are both similar and very different. They are similar in that they are all produced in some way by wrapping a cylinder around a spherical Earth. But the mathematics needed to produce them differ.

5 thoughts on “Notes on Mercator’s Projection

  1. Great article! Thanks for your work. Regarding the first simple projection discussed where y = tan(latitude), I assume that the map shown here is not truly to scale, right? because, for example, the tan(40), New York, for example is just .8 and the map here show NY to be quite a way more north on y axis. So are you multiplying the final y value by some constant to make the map look decent here?
    Just wondering. Thanks!

    1. I don’t quite remember where I got this image from, but I believe that it’s (a portion of) the tan projection described. I say a portion because the entire map is technically infinite (when you approach the poles, the map just stretches out more and more).

  2. But this can only work if the piece of land has no area. But as all pieces of land, no matter how small, has some area, the latitude of the piece of land is not \theta, but goes from \theta to \theta + \Delta \theta for some small number \Delta \theta. Similarly, the space this piece of land occupies on the map is not just y, but goes from y + \Delta y for some small number \Delta y. Now as \Delta \theta approaches 0, the ratio of \Delta y to \Delta \theta approaches \sec \theta:

    This part isn’t clear. I have no problem with the Calculus, it is the question of what is y. You never define it. It is described in the diagram as the height of the square of land in the diagram. But in the text it is defined as the area. Further, there is no description for why the limit approaches sec(theta). Very confusing.

    1. I don’t quite remember either, since I wrote this 7 years ago. Here, y is definitely not the area, I probably meant “vertical space on the map”, but I agree that this is confusing. If you do figure it out, tell me and I’ll edit it.

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