The World Geodetic System 1984 (WGSβ84) is the global reference frame used by GPS and most satellite navigation systems. It defines the shape of the Earth with a semiβmajor axis of 6β―378β―137β―m and a flattening of 1/298.257223563, providing a consistent latitude, longitude, and ellipsoidal height for any location on the planet.
The North American Datum 1983 (NADβ83) is the standard datum for mapping and surveying across the United States, Canada, and Mexico. Although its underlying ellipsoid (GRSβ80) is nearly identical to WGSβ84, subtle tectonic plate motions and regional adjustments create small offsets that must be accounted for when converting coordinates.
A simple Helmertβ7 parameter transformation is often used to shift WGSβ84 coordinates into NADβ83. The core of the conversion can be expressed as a latitude and longitude offset, plus a height correction. The formula is shown below:
ΞΞ» = longitude shift (degrees)
a_i, b_i = transformation coefficients
What is the difference between WGS-84 and NAD-83?
When should I use WGS-84 instead of NAD-83?
How accurate is the conversion from WGS-84 to NAD-83?
Can I convert coordinates back from NAD-83 to WGS-84?
What are some common applications for this conversion?
Is there a free tool available to perform this conversion?
How do I input coordinates for the conversion?
Results are for informational purposes only and do not constitute professional advice.
