(15)
coordinate
would be
artometric
coordinate
| (15) the
TM, ie.
‘ation (13)
ite side of
condition
oint in the
oelongs to
same line
ee (in the
'e. In this
nt point in
composed
than that
Xy'. The
oint in the
ates are
(16)
(18)
ixel it
in with the
(19)
Lets assume that we are building the image of a
rectangular terrain area. The domain of the function
F(X,Y) is a rectangle. The domain of the function F, (x',y")
is also a rectangle. The set of indices of the pixels P' of
the image F, and of the pixels P" of the terrain grid is the
same and can be written as
IP 4) e (ez? osisi osisig (20)
If we know the indices of the pixels the coordinates of the
centre of the pixel P; can be calculated in the coordinate
system O’X’y’. They will be equal:
x zd yis Did (21)
2 j .;2
According to (10) we have
(ye ei) (22)
Building the orthoimage we fill the grid of the pixels P' of
the side d with corresponding grey levels changing
successively the indices (20) in the lines and columns.
Then using the previous associations we can indicate
possibly precisely from which point in the photo the grey
value should be taken or which points should be chosen
to calculate it .
If we are building the digital othoimage
G: Pj — Ci (23)
means that we are building the image in the ground
coordinate system
Gy: Pi — Ci (24)
because | moving along the pixels P', corresponds to
moving in the terrain along squares of B sides and
centres determined by the formulas (16) and (21).
To determine c; we will compare G, and F images
assuming thatthe distance between the images should
be the smallest i.e.
1 1
HR
[Fo v)-G,0,vy?axv- X Y gxv)-o? -min (25)
D. i=0j=0p"
lj
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International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B3. Vienna 1996
It results that
ff (FO, Y)dxv - B^c =0 (26)
ij
The pixel P', of the orthoimage should then obtain the
grey level
gs INT [[F(X,Y) dXY) (27)
B^p*
j
ij
During the orthoimage generation the values of finite
sums
| k
e ANT ert i02 ROC Y
) (21+1)(2k+1)n=-Im=-k. ^! 242 ! 2k+2
(28)
are calculated more quickly than the integrals (28).
For k=I=0 it is obtained
0j =F(<;,Y;) (29)
and then the orthoimage is the function
(ij) 9 F(F4te (1.1) (30)
The reconstruction (resampling) of the image by the
averaging formula (29) causes that each average
decrease the variance what can be observed as the
smearing of the contours details. On the other hand
using an interpolation by the duplication (30) we obtain
the image more distant from the original (scanned
photograph).
3 Construction of DTM
In the previous paragraph it was assumed that for the
given area the function Z-H(X,Y) is known, i.e. the digital
terrain model (DTM).
This model could be prior determined and written in an
appropriate data base. If DTM doesn’t exist then it can
be obtained by one of the following ways:
e digitalization of the contours of the existing maps,
e the direct terrain measurement,
e the photogrammetric methods from at least two air
photos (stereo pairs).