Vertical Perspective
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Vertical Perspective Open
Coordinate Operation Method Details [VALID]
Name: Vertical Perspective
Code: 9838
Operation is Reversible: No
Formula: Note: These formulas have been transcribed from EPSG Guidance Note #7-2. Users are encouraged to use that document rather than the text which follows as reference because limitations in the transcription will be avoided.

This general case deals with a viewing point at a finite height hv above the origin. If the viewing point is at infinity, the formulas for the orthographic case (method code 9839) should be used.

The forward equations for the Vertical Perspective to convert geographical 3D coordinates (lat, lon, h) to Easting (E) and Northing (N) begin with the formulas of thje Geographic/topocentric conversions method (code 9836) to convert the geographical coordinates to topocentric coordinates U, V, W. The perspective projection origin is coincident with the topographic origin and has coordinates (latO, lonO, hO).

U = (nu + h) cos P sin (L – Lo)
V = (nu + h) [sin P cos Po – cos P sin Po cos (L – Lo)] + e^2 (nuO sin Po – nu sin P ) cos Po
W = (nu + h) [sin P sin Po + cos P cos Po cos (L – Lo)] + e^2 (nuO sin Po – nu sin P ) sin Po – (nuO – ho)

Then, given the height hv of the perspective viewing point above the origin, the perspective coordinates (E, N) are calculated from topocentric coordinates (U, V, W) as:

E = U * hv / (hv – W)
N = V * hv / (hv – W)

The reverse calculation from E,N to U,V,W and lat,lon,h is indeterminate.
Example: See EPSG Guidance Note 7-2.
Method
Parameters:
Parameter Name Parameter Code Sign reversal Parameter Description
Latitude of topocentric origin 8834 For topocentric CSs, the latitude of the topocentric origin.
Longitude of topocentric origin 8835 For topocentric CSs, the longitude of the topocentric origin.
Ellipsoidal height of topocentric origin 8836 For topocentric CSs, the ellipsoidal height of the topocentric origin.
Viewpoint height 8840 For vertical perspective projections, the height of viewpoint above the topocentric origin.