PlotMapProjection
Selects the underlying projection of PlotMap.
Robinson
The Robinson projection, presented by Arthur H. Robinson in 1963, is a modified cylindrical projection that is neither conformal nor equal-area. Central meridian and all parallels are straight lines; other meridians are curved. It uses lookup tables rather than analytic expressions to make the world map look right.
Name | Type | Annotation |
---|---|---|
centralMeridian | angle | central meridian [degree] |
Orthographic
The orthographic azimuthal projection is a perspective projection from infinite distance. It is therefore often used to give the appearance of a globe viewed from space.
Name | Type | Annotation |
---|---|---|
lambdaCenter | angle | central point [degree] |
phiCenter | angle | central point [degree] |
Perspective sphere
The orthographic azimuthal projection is a perspective projection from infinite distance. It is therefore often used to give the appearance of a globe viewed from space.
Name | Type | Annotation |
---|---|---|
lambdaCenter | angle | longitude of central point in degrees |
phiCenter | angle | latitude of central point in degrees |
altitude | double | [km] |
azimuth | angle | to the east of north of view [degrees] |
tilt | angle | upward tilt of the plane of projection, if negative, then the view is centered on the horizon [degrees] |
viewpointTwist | angle | clockwise twist of the viewpoint [degrees] |
viewpointWidth | angle | width of the viewpoint [degrees] |
viewpointHeight | angle | height of the viewpoint [degrees] |
Polar
Stereographic projection around given central point.
Name | Type | Annotation |
---|---|---|
lambdaCenter | angle | longitude of central point in degrees |
phiCenter | angle | latitude of central point in degrees |
Skyplot
Skyplot used to plot azimuth/elevation data as generated by GnssAntennaDefinition2Skyplot or GnssResiduals2Skyplot.
UTM
A particular subset of the transverse Mercator is the Universal Transverse Mercator (UTM) which was adopted by the US Army for large-scale military maps. Here, the globe is divided into 60 zones between 84$^{o}$S and 84$^{o}$N, most of which are 6$^{o}$ wide. Each of these UTM zones have their unique central meridian.
Name | Type | Annotation |
---|---|---|
zone | string | UTM zone code (e.g. 33N) |
Lambert
This conic projection was designed by Lambert (1772) and has been used extensively for mapping of regions with predominantly east-west orientation.
Name | Type | Annotation |
---|---|---|
lambda0 | angle | longitude of projection center [deg] |
phi0 | angle | latitude of projection centert [deg] |
phi1 | angle | latitude of first standard parallel [deg] |
phi2 | angle | latitude of first standard parallel [deg] |
Linear
Linear mapping of longitude/latitude to x/y (Plate Caree).
Mollweide
This pseudo-cylindrical, equal-area projection was developed by Mollweide in 1805. Parallels are unequally spaced straight lines with the meridians being equally spaced elliptical arcs. The scale is only true along latitudes 40$^{o}$44' north and south. The projection is used mainly for global maps showing data distributions.
Name | Type | Annotation |
---|---|---|
centralMeridian | angle | central meridian [degree] |