When you are trying to choose a coordinate system for your map, are you sometimes confused by the options?

What is the difference between a geographic coordinate system (GCS) and a projected coordinate system (PCS) anyways?

Here’s the short answer:

- A GCS defines
the data is located on the earth’s surface.*where* - A PCS tells the data
to draw on a flat surface, like on a paper map or a computer screen.*how*

- A GCS is round, and so records locations in angular units (usually degrees). A PCS is flat, so it records locations in linear units (usually meters).

## Where: Geographic Coordinate Systems

You are part of a search and rescue team looking for an injured person in the Australian outback. The point location you have from her satellite phone is 134.577°E, 24.006°S. Where is she located?

Both location A and B in the above image are correct. A is 134.577°E, 24.006°S in one GCS (*Australian Geodetic Datum 1984*) and B is the same coordinate location in another (*WGS 1984*). Without knowing which GCS the data is in, you don’t know if the hiker is on top of the plateau or if she has fallen off the cliff.

A geographic coordinate system (GCS) is used to define locations on a model of the surface of the earth. The GCS uses a network of imaginary lines (longitude and latitude) to define locations. This network is called a graticule.

So why isn’t knowing the latitude and longitude of a location good enough to know where it is? How can location A and location B in the Australia example both be correct?

Well it turns out the earth isn’t a perfect sphere. It’s a lumpy, bumpy, and uneven rounded surface. There are high mountains and deep ocean trenches. Because the planet spins, the poles are a bit closer to the center of the earth than the equator is. But in order to draw a graticule, you need a model of the earth that is at least a regular spheroid, if not a perfect sphere.

There are many different models of the earth’s surface, and therefore many different GCS! *World Geodetic System 1984 (WGS 1984)* is designed as a one-size-fits-all GCS, good for mapping global data. *Australian Geodetic Datum 1984* is designed to fit the earth snugly around Australia, giving you good precision for this continent but poor accuracy anywhere else.

The GCS is what ties your coordinate values to real locations on the earth. The coordinates 134.577°E, 24.006°S only tell you where a location is within a geographic coordinate system*. *You still need to know which GCS it is in before you know where it is on Earth.

## How: Projected Coordinate Systems

Once your data knows *where* to draw, it needs to know *how*. The earth’s surface—and your GCS—are round, but your map—and your computer screen—are flat. That’s a problem. You can’t draw the round earth on a flat surface without deforming it. Imagine peeling an orange and trying to lay the peel flat on a table. You can get close, but only if you start tearing the peel apart. This is where **map projections** come in. They tell you how to distort the earth—how to tear and stretch that orange peel—so the parts that are most important to your map get the least distorted and are displayed best on the flat surface of the map.

You’re perhaps already aware that there are many different map projections and that each displays the earth in a different way. Some are good for preserving areas on your map, others at preserving angles or distances.

**A projected coordinate system (PCS) is a GCS that has been flattened using a map projection. **

Your data must have a GCS before it knows where it is on earth. Projecting your data is optional, but projecting your map is not. Maps are flat, so your map *must* have a PCS in order to know how to draw.

Next, let’s take a look at how these coordinate systems (geographic and projected alike) are put together.

## Coordinate System Construction

In ArcGIS Pro, you can view the details of any coordinate system in the **Map Properties **window, on the **Coordinate Systems** tab. Click the green **Details** link.

The image below shows the **Details** page for the *Fuller (world)* coordinate system:

- The first line tells you that it’s a
**Projected Coordinate System**, as opposed to a GCS. - A PCS, by definition, uses a
**Projection**. The second line tells you that this PCS uses the*Fuller*projection, which was invented by Buckminster Fuller in 1954. **WKID**is a unique identifier number for the PCS, defined by its**Authority**.- Coordinates in a PCS are recorded in a
**Linear Unit**, often meters. **False Easting**,**False Northing**, and**Option**are parameters specific to the Fuller projection. Other projections have parameters like Central Meridian, Standard Parallel, and Latitude of Origin. You can often modify these parameters to center the PCS on a specific location. Below are two different PCS:*Hawaii Albers Equal Area Conic*and*Canada Albers Equal Area Conic.*They both use the same projection but different projection parameters.

- A PCS also contains a
**Geographic Coordinate System**! In this case, it’s WGS 1984.

Remember that a PCS is just a GCS that has been projected. Let’s look at the properties of the WGS 1984 geographic coordinate system:

- It has a
**WKID**(and**Authority**) as well. - Coordinates in a GCS are recorded in an
**Angular Unit**, usually degrees. - The
**Prime Meridian**is an arbitrary line of longitude that is defined as 0°. It typically runs through Greenwich, England, but it doesn’t have to. - The
**Datum**defines which model is used to represent the earth’s surface and where that model is positioned relative to the surface. - The
**Spheroid**is the regular model of the irregular earth. It’s part of the datum.**Semimajor Axis**,**Semiminor Axis**, and**Inverse Flattening**define the size of the spheroid.

## But wait!

Can’t we choose a GCS for our map instead of a PCS? I’ve made maps before that were in *WGS 1984* and they drew just fine, didn’t they?

Let’s try it out.

In **Map Properties**, expand the **Geographic Coordinate System **list and choose any one. Click **OK**.

Your map will look like this, regardless of which GCS you chose:

Remember that it is *impossible* to draw the round earth on a flat surface without a projection. So when you tell ArcGIS to make a flat map with a GCS, it is forced to choose a projection! So it draws using a pseudo Plate Carrée projection. This is just latitude and longitude represented as a simple grid of squares. It is called pseudo because it is measured in angular units (degrees) rather than linear units (meters). This projection is easy to understand and easy to compute, but it also distorts all areas, angles, and distances, so it is senseless to use it for analysis and measurement. You should choose a different PCS.

## Summary:

- You can store your data in a GCS. But you can’t draw it on a flat map without a PCS.
- The GCS tells your data where to draw. The PCS tells the map how to stretch the GCS out flat.
- Which GCS you choose depends on where you are mapping.
- Which PCS you use depends on where you are mapping, but also the nature of your map—for example, should you distort area to preserve angles, or vice versa?

Most of the time, you don’t need to choose a GCS. Your data was already stored in one and you should just stick with that. But often you do need to choose a PCS. Read the lesson Choose the Right Projection to learn how to pick the right one.

There are plenty of other resources that help to explain coordinate systems in greater depth and in different ways. If you want to learn more, try some of these:

- Coordinate systems, projections, and transformations
- Basics of Map Projections
- Map Projections in ArcGIS

*Cloth globe image by Charles Preppernau.*

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