WGS84 is standard for GPS
The World Geodetic System (WGS84) is the reference coordinate system used by the Global Positioning System.
It comprises of a reference ellipsoid, a standard coordinate system, altitude data and a geoid.
Similar to the North American Datum of 1983 (NAD83), it uses the Earth’s center mass as the coordinate origin.
The error is believed to be less than 2 centimeters – better than NAD83.
Pinpoint Your Position Using WGS84
When you need to accurately enter coordinates in a GIS, the first step is that you uniquely define all coordinates on Earth.
This means you need a reference frame for your latitude and longitude coordinates because where would you be on Earth without having reference to it?
Because the Earth is curved – and in GIS we deal with flat maps – we need to accommodate both the curved and flat views of the world. Surveyors and geodesists have accurately defined locations on Earth.
We begin modelling the Earth with an ellipse – which is different than a geoid (mean sea level). Over time, the ellipsoid has been estimated to the best of our ability through a massive collection of surface measurements.
When you combine these measurements, we arrive at a geodetic datum. Horizontal datums precisely specify each location on Earth’s surface in latitude and longitude or other coordinate systems. NAD27, NAD83 and WGS84 are examples of geodetic datums.
WGS84: Unifying a Global Ellipsoid Model with GPS
It wasn’t until the mainstream use of Global Positioning Systems (GPS) until a unified global ellipsoid model was developed.
The radio waves transmitted by GPS satellites enable extremely precise Earth measurements across continents and oceans. Global ellipsoid models have been created because of the enhancement of computing capabilities and GPS technology.
This has led to the development of global ellipsoid models such as WGS72, GRS80 and WGS84 (current). The World Geodetic System (WGS84) is the reference coordinate system used by the Global Positioning System.
What is EPSG4326? EPSG4326 is just the way to identify WGS84 using EPSG.
Never before have we’ve been able to estimate the ellipsoid with such precision.
This is primarily because of the global set of measurements provided by GPS.
WGS84 comprises of a reference ellipsoid, a standard coordinate system, altitude data and a geoid.
The error of WGS84 is believed to be less than 2 centimeters to the center mass.