WGS84 Gravity Model
Implement 1984 World Geodetic System (WGS84) representation of Earth's gravity
Libraries:
Aerospace Blockset /
Environment /
Gravity
Description
The WGS84 Gravity Model block implements the mathematical representation of the geocentric equipotential ellipsoid of the World Geodetic System (WGS84). The block output is the Earth gravity at a specific location. To control gravity precision, use the Type of gravity model parameter.
The block icon displays the input and output units selected from the Units list.
Limitations
The WGS84 gravity calculations are based on the assumption of a geocentric equipotential ellipsoid of revolution. Since the gravity potential is assumed to be the same everywhere on the ellipsoid, there must be a specific theoretical gravity potential that can be uniquely determined from the four independent constants defining the ellipsoid.
Use of the WGS84 Taylor Series model should be limited to low geodetic heights. It is sufficient near the surface when submicrogal precision is not necessary. At medium and high geodetic heights, it is less accurate.
The WGS84 Close Approximation model gives results with submicrogal precision.
To predict and determine a satellite orbit with high accuracy, use the EGM96 through degree and order 70.
Ports
Input
Output
Parameters
References
[1] "Department of Defense World Geodetic System 1984, Its Definition and Relationship with Local Geodetic Systems." NIMA TR8350.2.
Extended Capabilities
Version History
Introduced before R2006a