Coordinate conversion vs transformation: CRS, datum, frame and epoch
A coordinate conversion changes representation within a datum, such as geographic coordinates to a map projection. A transformation relates different datums or reference frames and may require parameters, grids and epochs. An EPSG code identifies a CRS; it does not by itself specify every operation or accuracy needed for a survey.
Name the representation and the reference
| Term | Meaning | What to record |
|---|---|---|
| Geographic coordinates | Angular latitude and longitude, optionally ellipsoidal height | Axis order, angle units and whether height is included |
| Projected coordinates | Planar easting and northing in a projection | Projection, zone, units, false origin and base geodetic CRS |
| Geocentric / ECEF coordinates | Cartesian X, Y and Z about the Earth’s centre | Frame realisation, units and coordinate epoch |
| Coordinate epoch | The time at which coordinates of a moving point apply | A date or decimal year and the model used to change epochs |
출처: PROJ: coordinate reference systems · PROJ: coordinate operations
EPSG:4326, EPSG:4979 and EPSG:4978 are different representations
EPSG:4326 describes a two-dimensional WGS 84 geographic CRS, EPSG:4979 includes ellipsoidal height, and EPSG:4978 is geocentric. A two-dimensional latitude/longitude pair contains no measured height. WGS 84 also has specific realisations: a generic WGS 84 label is insufficient when a task requires precise frame and epoch handling.
- Follow the interface’s declared axis order. Authority definitions and a web API’s longitude/latitude convention may differ.
- Do not put easting/northing into a latitude/longitude field because both accept decimal numbers.
- Preserve input units and decimal precision, but do not interpret additional decimal places as additional accuracy.
Height conversion needs a vertical reference
Ellipsoidal height is measured relative to an ellipsoid. Orthometric height is referred to a gravity-related vertical reference. In the common relation H = h − N, h is ellipsoidal height and N is geoid undulation; using it requires a geoid model and compatible reference conventions. Applying a horizontal projection does not perform this vertical operation.
- Record whether the deliverable uses ellipsoidal, orthometric or another defined height system.
- Check whether a required geoid grid is installed and valid for the location.
- Do not silently replace a missing measured height with zero for a three-dimensional datum transformation.
A seven-parameter transformation needs a convention
A three-dimensional Helmert transformation uses translations, rotations and scale. The position-vector and coordinate-frame conventions differ in the signs of the rotation terms. Parameters also have units, a direction and an area of intended use. A time-dependent operation may additionally use rates and a reference epoch; reversing a transformation is not the same as relabelling its source and target.
Verify the result using independent control
- Record source and target CRS, frame realisations, coordinate epochs, axis order, units and height references.
- Save the chosen operation, parameter convention, grids and their versions.
- Check the operation’s area of use and stated accuracy against the project requirements.
- Transform a known control point that was not used to fit local parameters, then inspect residuals in the deliverable’s units.
- Use a round-trip calculation to detect implementation mistakes, but do not treat round-trip agreement as independent accuracy evidence.
자주 묻는 질문
What is the difference between coordinate conversion and coordinate transformation?
A coordinate conversion changes the mathematical representation of coordinates within the exact same geodetic datum (e.g. from geodetic latitude/longitude to projected UTM easting/northing). A coordinate transformation relates coordinates between two different geodetic datums or reference frames (e.g. ITRF2014 to WGS84 or CGCS2000), typically requiring 3-parameter or 7-parameter Helmert translations, rotations, scale factors, and observation epochs.
Why is epoch important when transforming GNSS coordinates?
Tectonic plates move horizontally across the Earth at 2 to 10 cm per year. In dynamic reference frames like ITRF2020 or ITRF2014, station coordinates change continuously with time. Transforming a point to a static national datum (like CGCS2000 or NAD83) requires knowing the exact measurement epoch to apply plate motion models correctly.
참고 문헌 및 방법론
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