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ET Surface and Projections
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This topic will discuss some issues concerning the
projections of the surface datasets and the analysis performed on these
datasets.
Coordinate System Types ( from ArcGIS
desktop help)
- A Geographic
Coordinate System
(GCS) uses a three-dimensional spherical surface to define locations
on the earth. A GCS is often incorrectly called a datum, but a datum is only
one part of a GCS. A GCS includes an angular unit of measure, a prime
meridian, and a datum (based on a spheroid).
A point is referenced by its longitude and latitude values. Longitude and
latitude are angles measured from the earth's center to a point on the
earth's surface. The angles often are measured in degrees (or in
grads).
- A projected coordinate system is defined on a
flat, two-dimensional surface. Unlike a geographic
coordinate system, a projected coordinate system has constant
lengths, angles, and areas across the two dimensions. A projected coordinate
system is always based on a geographic coordinate system that is based on a sphere
or spheroid.
In a projected coordinate system, locations are identified by x, y
coordinates on a grid, with the origin at the center of the grid.
Coordinate systems and 3D analysis.
The Geographic
Coordinate System
provides a way to store common coordinates for locations anywhere in the
world.. Due to this fact it is used in many areas (Location based services,
navigation, etc.).
If however we want to measure distances and areas
on data in a GCS we are facing an obvious problem - the units of measure of a
GCS are actually angles - a distance of 2.5 Decimal Degrees does not mean much,
an area of 1.5 "Square Decimal Degrees" (if such term existed) means
even less.
One can argue that using GCS we can calculate
distances and areas on the Spheroid and the results will be in meaningful
distance/area units (meters, feet, etc..) and more accurate than the results
derived from projected data. This might be true, but only on large scale
(continental) data where the projected data will be more distorted by the single
projection used to represent it in Cartesian coordinates.
If we take into consideration the geographic
extent of the surface data that is normally used for 3D analysis, we can
conclude that an appropriately selected projection for the location of the data
will give us better results.
Based on the discussion above, the functions of
ET Surface work
- On surface data in any Projected Coordinate
System.
- Surfaces (Raster, ESRI TIN, PolygonZ TIN) that
are in a Geographic Coordinate System, need to be projected to a suitable
projection first.
- In order to get correct results for
Slope, Volume and 3D Area the Z units should be the same as the units
of the spatial reference of the data.
| Copyright © Ianko Tchoukanski |