The Global Positioning System (GPS) does not directly account for the Earth's irregular surface but provides latitude, longitude, and altitude based on a smooth model, specifically mean sea level (MSL). It calculates height above the Earth's barycenter and converts this to a height using the WGS84 spheroid model. When a specific map grid is selected, GPS translates the height into MSL for that coordinate system. This process is essential due to variations in elevation, as seen with coastal areas in Britain being several meters below MSL according to WGS84. For improved accuracy, Differential GPS (DGPS) can be utilized.