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General / Re: Dense Cloud and TLS positional mismatch by 0.5m in PhotoScan
« on: March 31, 2017, 09:27:06 AM »
I got this answer from agisoft support. I'm posting it here in case someone else has a problem with this.
I haven't tried the solution yet though but I'll post back when I know more
Dear Hans,
Thank you for contacting.
We assume that the issue is related to the following:
When you are exporting tiled model to zip format, it is actually saved in Euclidean (orthogonal) coordinate system that is tangential to the ellipsoid. In addition the coordinates of this system origin in WGS84 are stored in doc.kml (KML format only supports WGS84).
But exported point cloud is not in Euclidean coordinate system, as Transverse Mercator projection is not orthogonal, also the projected coordinate system takes into account the meridian convergence. So in your case only one point is transformed correctly - the origin of the tiled model, while in other areas the discrepancy can be observed due to the mentioned reasons.
So there are two ways, as we see it:
either to recalculate the coordinates of every vertex in the tiled model to the TM projection, or to export the dense cloud in local coordinates and adjust it's origin in accordance to the tiled model origin, as in this case the scale and orientation of the coordinate system axis should be the same.
I haven't tried the solution yet though but I'll post back when I know more

Dear Hans,
Thank you for contacting.
We assume that the issue is related to the following:
When you are exporting tiled model to zip format, it is actually saved in Euclidean (orthogonal) coordinate system that is tangential to the ellipsoid. In addition the coordinates of this system origin in WGS84 are stored in doc.kml (KML format only supports WGS84).
But exported point cloud is not in Euclidean coordinate system, as Transverse Mercator projection is not orthogonal, also the projected coordinate system takes into account the meridian convergence. So in your case only one point is transformed correctly - the origin of the tiled model, while in other areas the discrepancy can be observed due to the mentioned reasons.
So there are two ways, as we see it:
either to recalculate the coordinates of every vertex in the tiled model to the TM projection, or to export the dense cloud in local coordinates and adjust it's origin in accordance to the tiled model origin, as in this case the scale and orientation of the coordinate system axis should be the same.
