Coordinate System Basics
The challenge of representing a spherical Earth on a flat surface has posed many problems to academics of all types over the past two thousand years. The attempt to solve these problems has resulted in the systematic representation of all or part of the surface of a spherical body, otherwise known as a map projection. All geographic data has a coordinate system assigned to it so that it can be located to its actual location on Earth. There are two primary types of coordinate systems: geographic and projected coordinate systems (GCS & PCS). The details of these coordinate systems are explained later in this post. However, the figure below paints an informative picture of the primary differences between the two.
Datums
Datums are a single parameter of a geographic coordinate system that are vital in determining alignment and accuracy. The two most common datums used in North America are NAD83 (North American Datum 1983) and WGS84 (World Geodetic System 1984). NAD83 is North America-centric while WGS84 is meant to comprise a standard coordinate system for the Earth. The figure below illustrates the difference in accuracy and precision between the two. The bold line represents the actual surface of the Earth.
When making decisions based on maps it is crucial to ensure that the correct datum is being used. It is important to keep in mind that despite their individual shortcomings there is no best coordinate system or datum. That varies depending on the location of the map being created and the message that the cartographer wishes to convey.
Selecting the Ideal Coordinate System
Any time that one projects a curved surface onto a flat surface there will be a distortion in shape, area, distance, or direction. The trick is to determine which projection best fits the specific needs of the map that you are creating. Below are a few quick tips for accomplishing this.
- Databases created under contract or to be used by a government are often in a projection determined by that governing body (e.g. state plane in the United States or Great Britain Nation Grid in the United Kingdom.)
- Use equal-area projections (e.g. Lambert, Mollweide) for thematic maps. Equal-area maps preserve area measure, but do so at the cost of distorting shapes.
- Presentation maps are typically conformal projections (e.g. Mercator, Stereographic), although others may be used as well. Conformal projections maintain angles locally,
- Navigational maps are typically Mercator, despite its deficiencies.
Utilize local datums if making a map of a particular area. The coordinate system of a local datum is not at the center of the earth like the coordinate system of a geocentric datum, but rather has its origin at a location on the earth’s surface. If a map area contains multiple datums, for instance a map of the border area between Eastland, Texas and Comanche, Texas, it would use the datum that covers the majority of the mapped area. Let’s say the map in questions is primarily in Eastland County, Texas. You would then use SPC S83 4202, which is the Texas North Central Zone
Coordinate Systems in ArcMap
Defining a projection lets ArcMap know which projection your data is in for use in projecting on the fly, while projecting physically alters the source projection of the data. It is best practice to use the ‘Project’ geoprocessing tool to bring all data within the same coordinate system, if possible. Projecting on the fly uses additional resources and can harm the efficiency of your map.
What does one do if the coordinate system of the data is unknown? There are a few steps that one can take in order to be able to make an educated guess.
- Check the ‘Extent’ box of your data in ArcCatalog.
- If there are 6-8 units to the left of the decimal place, then it is most likely a projected coordinate system using linear measures of distance.
- If the units are in decimal degrees, one can be certain that the data is in a GCS.
- Once you have an idea of the projection type and units, the rest is trial and error. If you know that the data is based in North America then you will most likely use a UTM or state plane coordinate system.
- You may test your hypothesis by defining the projection in the feature class properties and seeing what happens. As stated before, this process may take some trial and error to achieve the desired results.
Conclusion
The first map projections held sparse information, but the cartographic community has since made tremendous strides. Still, it is key for any GIS Analyst to understand the pitfalls and advantages of various coordinate systems. Map projections not only affect the aesthetic of a map, but can also present an inaccurate depiction of its underlying data. At InterDev, we possess a keen understanding of these cartographic concepts and employ them in all of the maps that we create. For us, there is no way to create a great map without it first being an accurate map. This level of attention to detail permeates everything that we do.
Chris Rice
GIS Analyst I
crice@Interdev.com