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For: the best aerial view of the zone, the flights were
made along the axis of the canal, in a SSW-NNE direction at an
altitude of 6600 feet, permitting a swath about 3500 meters
(fie. 2).
A Daedalus 1230, 2-channel thermal scanner (1-2 and 8-114)
with the black bodies regulated between 16? and 20? C as a re-
ference, was used for the survey.
Harmonic analysis
As the prime aim of the aerial survey was preferably to
follow the movement of water, the recorded data was elaborated
on using the 8-11y channel, as it i's more suitable to our pur-
pose.
Over a body of water the use of near infrared reflected
energy and the thermal infrared emitted one, can fairly de -
scribe two quite different properties of the liquid surface.
The former, due to the strong absorption can give just a small
signal, related to the sea roughness; the latter, the emission
depending on the water temperature, can offer a panoramic view
of the gradienvs generated both by the current pattern and by
the waves. Then we can consider two distinct roughnesses, one
being of geometrical origin, the second referred to as energy
seepages at the surface produced by the preferential movement
of the water.
The applicable technique for data elaboration is the so
alled "harmonic analysis" consisting in the selection of com-
ponents forming the original signal of a scan line in the case
of thermography, and in particular in the choice of the most
meaningful among them to describe the texture. In the domain
of thermal infrared, the extraction of a component can posi-
tiveiy describe the currents field as seen at the surface of
the body of water, being the lines which the eye correlates on
the final result, given by the alignment of points showing an
appreciable thermal gradient. The presence of currents them-
selves should always produce a thermal gradient. But, unfortu-
nately, the value itself pends strongly on the direction tne
phenomenon is observed and, in the case of a scanner, surveyed.
To remove the influence »f the direction, the component extracted