j'on-
ohoto-
.ng
medium
ty
ars)
8
| mini-
| and
elblad
t 38000
vas
plec-
suit-
ted
his,
|rec-
;he
Experimental Results‘
In this paper a brief discussion will be given concerning
the attained experimentel results, Full.datails will be given
in the final rapport of the work.
Figure 6a shows the obtained Fourier transfornate using the
classical processor confiquration as shown in figure 2. Figure
6b shows the resulting Fourier transformate using the modified
optical configuration as proposed in this text. The benefits
Of the modification ars clearly shown in this confrontatione
Figures 6c to 6h show a series of equidensities anelyzed using
Agfacontour Professional film. The original is nubered as Fig.
6 and corresponds tc the Canary Islands archipelago. The bi-
nomy time of exposure - amplitude of the equidensity band was
calculated for each one of the equidensities, being the uncer-
tainity given by the dot shoun in figure 6g. This uncertainity
is due to the amplitude of the laser beam.
Figures 7a, 7b, and 7c confront the original trensperency
(7a) with the Fourier transformate (7b) and the contouring com-
position (7c). The original corresponds to the aroa of St. Jor-
ge's Bay. The analyzed part corresponds to the lower left cor-
ner since the amplitude of the laser beam was restricted to this
areas
Figures Sa, 3b, and 8c confront the original transparency
(Ca) with the Fourier transformate and the contouring composi-
tion (6b and Sc respectively. The original corresponds to
the Canary Islands archinelago and the analyzed area was res-
tricted to tha upper left part of the original since it revealed
a more interesting pattern of uaves.
The scale appearing in the contours has been calculated
taking account of the altitude of flight, the angle of vision
of the camera ( or what is the same, ths scale of the trans-
parencies) and the enhancement when doing the photographical
work.