Objectives of lecture:
If you didn't figure it out by now, GIS runs on coordinates. If you are weak on coordinate reference systems, check out Peter Dana's lecture notes (Geographer's Craft Project).
Registration connects known points on the map image to their intended location. This requires knowing the location of some set of points (tics in some parlance) in both coordinate systems. The selection of tic points is not as simple as it sounds. The distribution of tic points should be fairly uniform across your study area. If tic marks are always along roads, some areas might not be as carefully transformed. Errors in the sources might correlate with the landscape, creating bias and undiscovered troubles in analysis. Also, hidden in most software: a 'fit' computed between measurements.
{Geometric components: rotate, translate, scale} [Notation: x,y IN; XY out]
Equation 10-1: Similarity transformation
X = A + Cx + Dy
Y = B - Dx + Cywhere C = [scale factor] times cosine ( [angle of rotation] )
D = [scale factor] times sine ( [rotation angle] )
A & B are offsets for the center of rotation in output coordinates {Translation}Equation 10-2: Affine transformation
{ because maps may not have the same scale in X & Y}
X = A + Cx + Dy
Y = B - Ex + Fy
Many more: Helmert transformation (can deal with radial distortion
as from a camera lens)
the real source for registration points. Measured by geodetic
surveying, often used to 'control' surveys to construct maps.
(most features on map are indirectly measured on the earth, connected
by geodetic control)
About National
Geodetic Reference System; Peter Dana's lecture
notes on Geodetic Datums;
watch out for roundoff. Computers may only have 6 digits unless you use the much slower 'double precision'.
Map may not match projection of coordinate system [See: Spatial Reference Systems].
Do not expect the above equations to make the projection change
along with the transformation. The geometry of the ellipsoid
and projection matter.
In USA: Feds use UTM (Universal
Transverse Mercator), local 'State Plane' is either Lambert
Conformal Conic (as in Wa) or some other Transverse Mercator;
Washington
State Plane is a particular Lambert Conformal
The 'grid north' on these projections is NOT 'true north' except
along the central meridian. [An example
from Texas - capitol]
The scale is not true except along particular lines and at sea
level. GIS often assumes that these corrections are not important...
There really should be corrections built into calculation of area
and perimeter for "grid to ground" (distance from projection
surface to ground elevation) as well as known distortions (such
as using conformal projections that are not equal area...).
USGS response [not online today...]
Projections matter; grid north is NOT true North; see 465 course
all models simplify.
Geographic models choose which component to control and which
to measure.
Representations also impose further modifications.
Beard presents a system of generalization:
either a lot of visual inspection, or use software to verify relationships (integrity constraints) expected to occur - the topological model for geometry; attributes verified by other relationships (completeness from list of all objects) or brute force inspection.
stitch map sheets together into sheetless coverage.
'Rubber sheet' forces certain points to match, interpolates between;
'Conflation' matches attributes.
Zipper interpolates across sheet edges. [slides]