WGS84

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Introduction

When you need to accurately enter coordinates in a GIS, the first step is to uniquely define all coordinates on Earth. This means you need a reference frame for your latitude and longitude coordinates. Because the Earth is curved and in GIS we deal with flat map projections we need to accommodate both the curved and flat views of the world. Surveyors have accurately defined locations on Earth. We begin modelling the Earth with an ellipsoid. To be clear, this is different than a geoid which is a measure of 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 …show more content…

It was in the year 1980 when the need for world geodetic system was recognised by the so called the geodetic community, also within the US Department of Defense.
The earliest used geodetic system no longer provide sufficient data, information, geographic coverage, or product accuracy for all the-current and anticipated applications. The means for producing a new WGS84 were available in the form of improved data, increased data coverage, new data types and improved techniques.
The new world geodetic system called WGS84 is an acronym for World Geodetic System 1984. It is a standard for various activities related to mapping for an example: Navigation, Cartography and Geodesy. The World Geodetic System 1984 (WGS84) is the datum used by the Global Positioning System (GPS).
Within the World Geodetic System (WGS), there are several datums that have been in use throughout the years. These are WGS 60, 70, 72, and 84. The WGS84 is currently one in use for this system. In addition, it is one of the most widely used datums around the …show more content…

WGS84 coordinates system are geographically positioned with respect to center of the earth. Such a system is called ECEF (Earth-centered, Earth fixed). The WGS84 coordinate is a three-dimensional, right-handed, Cartesian coordinate point at the center of mass of an ellipsoid, which approximate the total mass of the earth. Figure 2.1 and 2.2 below shows the geographically positioned coordinate with respect to the center (ECEF). And figure 2.3 shows what it is meant by right-handed Cartesian

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