Horizontal Coordinate Systems
There are two kinds of horizontal coordinate systems; one is called a Geographic Coordinate System and the other is a Projected Coordinate System. The Geographic Coordinate System is based on the globe, coordinates are given in latitude and longitude. Latitude and longitude are usually given in degrees, but can be in other formats as well. Latitude is measured up and down from the equator and longitude is measured from some arbitrary zero point that is chosen called the prime meridian.
On the lower left is an example of a Geographic Coordinate System. This particular view references a GCS which is known as WGS 84. There a two ways to specify a coordinate system in Esri’s ArcMap Software. First, is by a Well Known ID (WKID) and the second is Well Known Text. A WKID is any predefined coordinate system. If the WKID is less than 32767 it is assigned by the European Petroleum Survey Group EPSG. All WKID’s greather than 32767 are assigned by Esri. In the nineteenth century, Nicolas Auguste Tissot developed a method to compare distortion in different types of map projections (depicted in the lower right).
Projected Coordinate System’s are dealing with a flat map with xy values on a Cartesian grid (values would be feet, yards, meters). A Projected Coordinate System is always based on a particular Geographic Coordinate System. PCS contains a projection which is the mathematical algorithm used in converting between the latitude and longitude value and the XY value. There is always various parameters which are specific to the mathematical algorithm and the linear unit referenced. The State of New Hampshire uses a Projected Coordinate System which if referred to as “NAD 1983 State Plane New Hampshire FIPS 2800 Feet“.
Projections
VERTICAL COORDINATE SYSTEMS
Credits: ESA/HPF/DLR: Source; Terms & Conditions
Transformations
What is a transformation and why is it important? If we look at the image above, the dashed blue line is our theoretical ellipsoid which does not necessarily match the surface of the earth. We have some data in the upper left; imagine you have data near Mount Washington New Hampshire which is a mile high. You are a mile high above this theoretical ellipsoid. What happens is we have an ellipsoid that really does not match the surface of the earth at that location, so what we want to do is pick a different ellipsoid which fits the surface of the earth at that location.
This particular ellipsoid works better than the other one. So in this case for instance we are looking at the theoretical WGS84 and now we have a local datum using NAD83. So the data transformation is moving the data from one of these ellipsoids to the other one. This can involve a shift, rotation, or change in direction. Think of the ellipsoid as the size and shape and the datum then fixes that ellipsoid to the earth. For simplification of the model various spheroids or ellipsoids have been created. The terms can be used interchangeably.
If you had ortho imagery that uses a projection of “NAD 1983 State Plane New Hampshire FIPS 2800 Feet” and vector data (Streets) in “NAD 1927 State Plane New Hampshire FIPS 2800” it would not display correctly. If you apply the transformation from “NAD 1927 to NAD 1983 NADCON”, the street data will line up correctly. A Geographic Transformation or Datum transformation typically involves moving your data not more than 100 meters. If you’re looking at a world map; you will not see a 100 meters, but the more you zoom in it will require you to transform the data.
The two kinds of transformations are geographic and vertical. The geographic (horizontal) one is shifting between the two GCS’s. You may have to do a vertical transformation at the same time, which is shifting between some ellipsoidal or geoidal view. A particular transformation goes from one GCS to another GCS. Demo Application Illustrating Geographic Transformation
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