Fig 1. Vector Co-ordinate Diagram
A vector (Fig 1; V) is a quantity with both magnitude and direction that can be defined using three related dimensions, either linear or angular.
Cartesian co-ordinates (Fig 1), are the linear dimensions (x,y,z) that define the end of a vector with respect to two or three-dimensional axes.
Polar co-ordinates (Fig 1) define a vector with respect to a two or three-dimensional plot using angular rotations (α,β) along with its length (V).
Fig 2. Map Co-ordinate Diagram
Grid co-ordinates (Fig 2) are normally used to specify a point on a map that may be a flat (2-D) plane or the surface of a 3-D volume, such as the spherical surface of a planet.
Location of a point on a spherical surface, e.g. that of a planet, can be defined either from two related angles at right-angles to each other, that are generally referred to as latitude and longitude, or from circumferential distances at right-angles to each other; e.g. the UTM system.
Co-ordinates Calculator - Technical Help
It is unnecessary to define distance and length units as you will get out whatever you enter.
Cartesian to Polar & Polar to Cartesian calculation options:
x, y, z: 3-D linear dimension from the co-ordinate origin to the end of the vector
V: the length of the vector
β: the vertical angle from the x,y plane at z=0 [°]
α: the horizontal angle from the x,z plane at y=0 [°]
Angle to Distance & Distance to Angle calculation options:
R: the radius of the sphere (or planet)
Lat: Latitudinal angle up (+ve) or down (-ve) from the equator [°]
Long: Longitudinal angle east (+ve) or west (-ve) from a datum vertical co-ordinate (e.g. GMT) [°]
N/S: vertical circumferential distance up (+ve) or down (-ve) from the equator
E/W: horizontal circumferential distance east (+ve) or west (-ve) from a datum vertical co-ordinate (e.g. GMT)
... input data above and:
a: horizontal 3-D linear dimension from the co-ordinate origin to the end of the vector (Fig 1)
E/W defines the horizontal circumferential length from the datum/origin at the latitudinal height above the equator or horizontal circumferential datum. In other words, this length will reduce as the latitude (Lat) rises until at the top or bottom poles at which point Lat = 90° and E/W = 0
The co-ordinates calculator applies to any vector length and spherical diameter within the numerical limits of the operational computer
The co-ordinate calculator produces no known errors.
You will find further reading on this subject in reference publications(15)